ELEMENTS OF PHYSICAL BIOLOGY BT ALFRED J. LOTKA, M.A., D.Sc. "Voil& un homme qui a fait son miens pour _enniwer deux ou trois cents de ses concitoyens; mais son intention 6tait bonne: il n'y a pas de quoi dftniire PersepolM. Yoltovre BALTIMORE WILLIAMS & WLKINS COMPANY 1925 Composed and Printed at the WAVERLf PRESS BT THE VYlLLIAMS & WlLKINS Baltimore, Md., U. S. A. T COPTEIQHT 1925 WILLIAMS & WILKINS COMPANY Made in United States of America Published February, 1925 ALL BIGHTS KESERVIpD v^ DEDICATED TO THE MEMORY OF JOHN HENBY POYNTING PREFACE The preface is that part of a book which is written last, placed first, and read least. As I approach my concluding task I am moved to reflect why a preface should be written at all. This question, if followed into all the intricacies of which it holds potentiality, should apparently result in a composition new in literature, a Preface to the Preface. Such precedent should not be lightly established, for it suggests a vista of future degenerations after the pattern of Josiah Royce's infinite succession of maps, each containing within Itself its own replica on a reduced scale. But without going to such lengths as this, the philosophy of the preface may perhaps briefly be summarized to this effect, that It is the author's subjective introduction , to the more objective matter that should follow. Here he may, if this is deemed of any interest, say something regarding the circumstances that gave origin to the w-ork, and the conditions under which it came into being. He may express his feelings as to its alleged purpose, and may follow custom by giving voice to pious wishes as to the function which the product of his presumptive mind may fulfill in an Universe in which no event, however trivial be it no more than the addition of one more book to the groaning library shelves is without distant reverberations. As to origin, the first plan of the work was laid about 1902, in the author's student days In Leipzig. The development of the topic is recorded, in outline, in various publications, of which the first appeared in 1907 in the American Journal of Science. Eeference to this and to its various sequels will be found in pertinent places in the text that follows. The last stage of the work, arrangement of the matter in collected form, and filling in the flesh about the skeleton framework elaborated in the journal literature, was carried out at the Johns Hopkins University upon the invitation of the Department of Biometry and Vital Statistics. For the courtesies so extended to him the author wishes here to express his thanks, as well as for the interest shown in the progress of the work by Dr. Raymond Pearl and the members of the Department, notably Drs. W. T. Howard, L. J. Reed and J. R. Miner. Outside the walls of VU1 PREFACE this University I think with very particular appreciation of the never-failing succor in times of mathematical trouble, which I found at the hands of Prof. F. R. Sharpe of Cornell University; also of the patient assistance, upon more than one occasion, from Prof. W. B. Fite of Columbia University. And I gratefully recall encouragement received from Dr. G. K. Burgess, Director of the Bureau of Standards, especially in the earlier stages of the work, when encouragement was most needed. Acknowledgment has been made in the text for numerous quotations. The somewhat extended excerpts from certain articles published in the Scientific Monthly call for special notice here, and I wish to express my thanks both to the author, Prof. G. W. Martin, and to the Editor of the Monthly, for permission to quote thus at length from its pages. I am similarly indebted to the Editor of Harpers Magazine for permission to reproduce here certain portions of an article from my pen, entitled "Biassed Evolution", which originally appeared in the May issue (1924) of that publication. Toward the publishers, Messrs. Williams and Wilkins and in particular Mr. C. C. Thomas, I have every occasion to entertain feelings of the most cordial appreciation. Through their courteous attentions the business of bookmaking was made a pleasure. My greatest debt is acknowledged in the dedication. Whatever merits this book possesses may well be credited to the influence and teaching of Poynting. There is little danger that its faults shall be charged to his account. As to the topic of the work it seems unnecessary to say many words here, inasmuch as a delineation of this has been made the subject of a special chapter on The Program of Physical Biology. Only this explanation it may be well to offer here, that, as proposed in Chapter V} the term Physical Biology has been employed to denote the broad application of physical principles and methods in the contemplation of biological systems, whereas Biophysics, in common parlance, relates rather to the special field of certain physical aspects of the life processes of the individual. With this terminology, Physical Biology would comprehend Biophysics within its scope. The writer cannot in reason expect to have produced a work without blemish. Even an approach to such absolute perfection is the rare privilege of a few. He would, however, be unjustified in addressing the reading public at all if he did not entertain the hope PEEFACE IX that, despite shortcomings, these pages may bring to the reader new assets, here and there a new piece for his mental furniture, now and again a new perspective, a new comprehensive outlook over a body of facts and relations in themselves perhaps familiar. The work has been largely one of systematization, and of development of method. Factual material has been introduced essentially for the purpose of illustrating the point of view to be set forth. There seems therefore hardly any occasion for apologetic explanations that anything of the nature of completeness in the presentation of pertinent facts was in nowise armed at. Indeed, it must be obvious upon most casual reflection that such completeness, in a subject of the amplitude of that here taken in view, could be achieved only in a cyclopedic work of several tiers of volumes. Considerable care has been taken to cite in detail the sources consulted. It was felt that, on account of the wide dispersal of these citations over a broad field of scientific literature, few readers could be expected to be familiar with all the branches of pertinent library lore, and for this reason a collation of such references should have a value of its own, even apart from the text. At the same time the compilation of anything like a complete bibliography could not be undertaken on the present occasion. It is hoped that the mathematical mien of certain pages will not deter biologists and others, who may be disposed to look askance at symbols of the art, from acquiring an interest in other portions of the book. Biometricians will, presumably, not shrink on this score; to them, and to physicists, (whomI should greatly wish to numberamong my readers) I may perhaps confess that I have striven to infuse the mathematical spirit also into those pages on which symbols do not present themselves to the eye. For this I offer no apology. For the sake of space economy recapitulary paragraphs have, as a rule, not been given a place in the text. An exception has however been made in Chapters XX, XXXIII and XXIV, the last of which, in particular resumes and amplifies somewhat certain phases of the topics discussed in earlier chapters. The reader who may wish briefly to review the substance of his reading as he proceeds, should find suitable assistance in the rather detailed Analytical Synopsis of Chapters that has been placed immediately after the Table of Contents. And finally, a bird's eye survey of the general X PREFACE field covered in this work can be obtained by consulting the Tabular Synopsis at the end. Here, then, I make my exit from the prefatory stage and commend my work to the tender mercies of the reader; not without some trepidation, for I recall how Voltaire said of one: "II fit une philosophic comrne on fait un bon roman; tout parut vraiseniblable, et rien ne fut vrai;" and there comes to mind the language still plainer of du Maupassant "Depuis qu'ils ont appris a lire et a ecrire, la betise latente se degage." I trust that the reader's response to these pages may not be too fervent an Amen to the prayer of The Sceptical Chymisi "It is to be hoped that these men, finding that they can not longer write impertinently and absurdly .... will be reduced either to write nothing, or books that may teach us something . , . . ; and so, ceasing to trouble the world with riddles or impertineneies, we shall either by their books receive an advantage, or by their silence escape an inconvenience." ALFEED J. LOTSA. Johns Hopkins University, May, 1924- CONTENTS PART I. GENERAL PRINCIPLES CHAPTER I Regarding definitions 3 CHAPTER II Evolution Defined : The History of a System in the Course of Irreversible Transformation 20 CHAPTER III The Statistical Meaning of Irreversibility 30 CHAPTER IV Evolution Conceived as a Redistribution 41 CHAPTER V The Program of Physical Biology 49 PART n. KINETICS CHAPTER VI The Fundamental Equations of the Kinetics of Evolving Systems. General Case 57 CHAPTER VII Special Case : Single Dependent Variable 64 CHAPTER VIII Special Cases : Two and Three Dependent Variables 77 CHAPTER IX Analysis of the Growth Function 100 CHAPTER X Further Analysis of the Growth Function 128 PART III. STATICS CHAPTER XI General Principles of Equilibrium 143 CHAPTER XII Chemical Equilibrium, as an Example of Evolution under a Known Law. . 152 xi Xll CONTENTS CHAPTER XIII Inter-species Equilibrium. . , 161 CHAPTER XIV Inter-species Equilibrium : Aquatic Life. 171 CHAPTER XV The Stage of the Life Drama 185 CHAPTER XVI The Circulation of the Elements. The Water Cycle 209' CHAPTER XVII The Carbon Dioxide Cycle 218 CHAPTER XVIII The Nitrogen Cycle 229 CHAPTER XIX The Phosphorus Cycle 246 CHAPTER XX Cycles : Conclusion and Summary 252 CHAPTER XXI Moving Equilibria. . . 259 CHAPTER XXII Displacement of Equilibrium 280 CHAPTER XXIII The Parameters of State 300 PART IV. DYNAMICS CHAPTER XXIV The Energy Transformers of Nature 325 CHAPTER XXV The Helation of the Transformer to Available Sources 336 CHAPTER XXVI The Correlating Apparatus 362 CHAPTER XXVII Extension of the Sensuous World Picture 371 CHAPTER XXVIII The Adjusters. 381 CONTENTS Xlll CHAPTER XXIX Consciousness 388 CHAPTER XXX The Function of Consciousness 394 CHAPTER XXXI The Origin of Consciousness in the Living Organism 402 CHAPTER XXXII Energy Relations of Consciousness 406 CHAPTER XXXIII Review of the Correlating Apparatus 410 CHAPTER XXXIV Conclusions ] Retrospect and Prospect 417 Synoptic chart of physical biology 435 LIST OF ILLUSTRATIONS FIG. 1. Graph of model process illustrating the statistical meaning of irreversibility. Reproduced from A. J. Lotka, Two Models in Statistical Mechanics, Am. Math. Monthly, vol. 31, 1924, p. 122 31 FIG. 2. Graph of second model process illustrating the statistical meaning of irreversibility. Reproduced from A. J. Lotka, Two Models in Statistical Mechanics, Am. Math. Monthly, vol. 31, 1924, p. 124 33 FIG. 3. Frequency diagram for the deviations from the mean appearing in figure 2. Reproduced from A. J. Lotka, Two Models in Statistical Mechanics, Am. Math. Monthly, vol. 31, 1924, p. 125 34 FIG 4. The law of population growth for the United States according to Pearl and Reed 68 FIG. 5. Growth of a population of Drosophila (fruit flies) undsr controlled experimental conditions, according to Pearl and Parker. 69 FIG. 6. Growth of a bacterial colony (B. dendroides). according to H. G. Thornton 71 FIG. 7. Growth of rat according to H. H. Donaldson and T. B. Robertson. 73 FIG. 8. Growth of sunflower seedlings according to H. S. Reed and R. H. Holland; computed curve by L. J. Reed 74 FIG. 9. Growth of sunflower seedlings. The same data as in figure 8, but plotted in logarithmic diagram 75 FIG. 10. Presumptive curve of growth of endemic malaria according to the Ross Equation. Reproduced from A. J. Lotka, Am. Jour. Hygiene, January Supplement, 1923 84 FIG. 11. Course of parasitic invasion of insect species according to W. R. Thompson 85 FIG. 12. Increasing diffusion-in-time of successive generations in the progeny of a population element 86 FIG. 13. Course of parasitic invasion of insect species, according to Lotka; elementary treatment 90 FIG. 14. Course of parasitic invasion of insect species, according to Lotka; more exact treatment 91 FIG. 15. Some historical human survival curves, exhibiting an evolutionary trend toward longer average duration of life 103 FiGi 16. Survival curves for the State of Massachusetts, for the three decades 1890-1900-1910. After Glover 104 FIG. 17. Survival curves for different countries. After Glover 105 FIG. 18. Survival curve plotted on logarithmic scale. II. S. 1910 107 FIG. 19. Logarithmic survival curves for man, Drosophila, and Proales decipiens. Plotted according to centiles of life-span. After R. Pearl. . 109 FIG. 20. Diagrams to illustrate proof of stability of normal age distribution. Reproduced from A. J. Lotka, Proc. Natl. Acad. Sci., vol. 8, 1922, p. 339 , 113 xv ^ LIST OP ILLUSTRATIONS FIG. 21. "Stable" age distribution, as exemplified by the population of England and Wales in the decade 1871-1880........................... 114 FIG, 22. Diagram of relation between birth rate per head 6 and death rate per head d in population with stable age distribution ................ 117 FIG. 23. Diagrammatic illustration of influence of random and of selective slaughtering upon survival curve of biological species .............. 120 FIG. 24. Growth of favored type in mixed population of two phenotypes After J. B. S. Haldane............................................. 124 FIG. 25. Effect of selection on population comprising two phenotypes with Mendelian inheritance. After J. B. S. Haldane ..................... 126 FIG. 26. Feed consumed, and increase in live weight of steers at several ages. After Moulton, Trowbridge and Haigh....................... 133 io. 27. Some fundamental types of equilibrium, in a system with two dependent variables............................ j4g FIG 28. Map of integral curves for the Ross malaria equations.' Repro- 1923 A' J" L tka' Am' JoUr- Hygiene> January Supplement, FIG 29 Model of surface corresponding to figure 28 '."Reproduced from ff^ A ?' JoUr' Hygiene> January Supplement, 1923 ......... 150G. dO. Age distribution in population of molecules of two substances in monomolecular chemical equilibrium. Reproduced from A. J. Lotka,Am. Jour. Science, 1907, p. 208....... 155 n contents " of '' * of srasshoppe FIG 34. Seasonal food habits of the Meadow" Lark.' After H.c'.B^ant* ' ' ^ of FIG. 39. Key to figure 38 .............................................. 177 205 LIST OF ILLUSTRATIONS FIG. 45. Periodic classification of the elements, showing division into petrogenic elements and metallogenic elements. After H. S. Washington ^ 7 FIG. 46. Circulation of the elements in nature. The water cycle 215 FIG. 47. Circulation of the elements in nature. The carbon cycle 226 FIG. 48. Circulation of the elements in nature. The nitrogen cycle 230 OQTJ FIG. 49. Organic nitrogen circulation *0i FIG. 50. The rise of the saltpeter industry 235 FIG. 51. The rise of the fixed nitrogen industry 24 FIG. 52. Circulation of the elements in nature. The phosphorus cycle. . . 247 FIG. 53. The Soxhlet extraction apparatus 253 FIG. 54. Circulation of the elements in nature. The sodium chloride cycle ; m FIG. 55. Uranium and its products of radioactive disintegration 263 FIG. 56. Equilibrium polygon for Radon (radium emanation) in contact with its disintegration products 266 FIG. 57. Relative abundance of the elements. Diagram according to W. D. Harkins, based on analysis of meteorites. (Jour. Am. Chem. Soc., 1916, p. 863) 271 FIG. 58. Equilibrium polygon for the human species and some of the species on which it depends for its food supply 277 FIG. 59. The Yellow Shark and some of his relatives, as an example of possibly orthogenetic development 296 FIG. 60. Law of urban concentration 308 FIG. 61. Relation between rate of reproduction in Drosophila (fruit fly) and density of mated population. After Pearl and Parker 309 FIG. 82. Relation between mean length of life and population density in Drosophila. After Pearl and Parker 310 FIG. 63. Hyperbolic curves obtained by plotting as ordinates the number of genera 1, 2, 3, . . . n species, and as abscissae the number n of such species. After J. G. Willis 314 FIG. 64. Relation between number and size of genera of all flowering plants, plotted logarithmically. After J. C. Willis 315 FIG. 65. Relation between number and size of Rubiaceae, plotted logarithmically. After J. C. Willis 315 FIG. 66. Relation between number and size of genera of chrysomelid beetles, plotted logarithmically. After J. C. Willis 316 FIG. 67. Solubility of carbon dioxide in water, expressed in volumes of COj measured at normal temperature and pressure, per volume of water. After G. W. Martin 318 FIG. 68. The mill-wheel of life 334 FIG. 69. Mechanical walking beetle, exhibiting the several characteristic elements of the correlating apparatus 341 FIG. 70. The evolution of man's means of transportation 367 FIG. 71. Growth of American Railways 369 FIG. 72. How the future enters into the determination of the motion of the walking mechanical beetle, thus imitating purposive action (teleology) 382 LIST OF TABLES Table 1. The program of physical biology 53 Table 2. Growth of the population of the United States 67 Table 3. Growth of bacterial colony. After H. G. Thornton 70 Table 4. Growth of sunflower seedlings. After H. S. Reed and R. H. Holland 74 Table 5. Course of parasitic invasion of insect species, according to W. R. Thompson 86 Table 6. Tabular survey of different modes of interdependence of biological species 98 Table 7. Example of normal age distribution 113 Table 8. Relation between birth rate per head b and death rate per head d in a population with normal age distribution 117 Table 9. Growth of steers, and feed consumed 134 Table 10. Survey of methods of marine biological census 178 Table 11. Principal components of the earth's surface crust 185 Table 12. Distribution of gases in the atmosphere at different levels 188 Table 13. Constituents of the atmosphere, at earth's surface and in toto . . 190 Table 14. Composition of the Ocean 191 Table 15. Comparison of air and aquatic atmosphere 192 Table 16. Composition of lithosphere 194 Table 17. Composition of human body 197 Table 18. Composition of living organisms. After H. F. Osborne 198 Table 19. Comparison of composition of blood serum and sea water 201 Table 20. Moisture contents of foods 211 Table 21. Discharge of the World's rivers 214 Table 22. Progress of by-product coke ovens in the United States 233 Table 23. Growth of the saltpeter industry 237 Table 24. Uses of saltpeter 237 Table 25. Meteoric rise of the nitrogen fixation industry 242 Table 26. Supply of plant foods in the soil 257 Table 27. Rate of participation of the elements in the cycle of nature. . . 258 Table 28. Radioactive equilibrium of radium in contact with its disintegration products 265 Table 29. Radioactive equilibrium of radon (radium emanation) in contact with its disintegration products 268 Table 30. Geological time table. After C. Schuchert 269 Table 31. World's production of population and its accessories. After R. Pearl 278 Table 32. Association of high blood pressure with over-weight 295 Table 33. Distance travelled in one hour by different modes of conveyance 368 Table 34. Man's correlating apparatus, native and artificial contrasted. . 411 Table 35. Man's correlating apparatus (continued). The Adjusters 413 Table 36. Classification of the sciences 423 ANALYTICAL SYNOPSIS OF CHAPTERS PART I. GENERAL PRINCIPLE Chapter I. Regarding Definitions. Definitions are arbitrary, 3 But are governed by considerations of expediency, 3 The problem of expediency in framing definitions is not always a simple one, 3 Pseudo-problems arising from failure to recognize the arbitrary character of definitions: Hunting the Jabberwock, 4 Subjective discontinuities introduced by the senses, 5 Examples: Colors, e.g. blue, green; light and heat waves; distinction between animals and plants; between biological species; between living and non-living matter, 5 To such abrupt subjective divisions there may correspond no objective discontinuity in nature, 5 Definitions in Biology, 5 Vitalism versus Mechanism; merely a question of terms, 7 Herbert Spencer's "proximate definition" of life, 7 Inadequacy of Spencer's definition, 7 Sir Edward Schaefer's standpoint, 8 Line of division recedes with increasing knowledge 8 Alleged characteristics of living matter: Growth from within 8 Chemical growth as distinguished from physical growth of crystals, 10 Growth from unsaturated solution, as distinguished from growth of crystals from supersaturated solution, 10 "Selective" growth, 10 Reproduction, 11 Vital Force, 13 Physical chemistry of structured systems, 13 Geometrical element lacking in physical chemistry of today, 13 Systems ordinarily considered are either structureless or of simple structure, 14 This absence of structural features in physico-chemical systems is due to subjective, not objective reasons, 14 Due in part to convenient arbitrary restrictions, 15 Relation between growth, environment and structure, 15 The laws of chemical dynamics in structured systems will be the laws that govern the evolution of a system comprising living organisms, 16 Application to Biology: The organism as a structured physico-chemical system, 16 The travelling environment, milieu inte"rieur, 17 Increasing independence of organism of its remote environment, 18 The policy of resignation: Abandoning the attempt to define life, 18 Parallels in the history of science : Abandonment of the attempt to prove Euclid's twelfth postulate led to new systems of geometry, 18 Abandonment of attempts to build perpetual motion machines was equivalent to recognizing the law of conservation of energy, 18 Abandonment of the attempt to detect the earth's motion through the ether is the foundation of the modern theory of relativity, 18 The ideal definition is quantitative, 19 Desirability of establishing a quantitative definition and conception of evolution, 19. Chapter II. Evolution Defined. Definition should conform as far as possible to common usage of the term, 20 Analysis of common conception of evolution, 20 Evolution is history, but not all history is evolution, 20 Systems in purely periodic motion would not be said to evolve. They repeat in endless xxi XXil ANALYTICAL SYNOPSIS OF CHAPTERS succession the same series of events. In an evolving system each day is unlike any other day, 21 Evolution not a mere changeful sequence, 21 Abortive attempts to formulate the direction of evolution, 21 These attempt definition in terms of a single component, 22 Such definitions are foredoomed to failure, a successful definition must be framed in terms of the evolving system as a whole, 22 Evolution is the history of a system in the course of irreversible transformation, 24 Scope of this definition: What it excludes; what it includes 24 The line of division depends on the nature and extent of our knowledge regarding the system, 25 This is in harmony with the fact that problems of evolution are largely problems of probability, 25 All real transformations are irreversible, hence all real history is evolution, 26 What then is gained by the definition? 26 It indicates the direction of evolution as the direction of irreversible transformations, the direction of increasing entropy, 26 Example of pendulum. Irreversible feature introduced by frictional force, 27 Inertia-free or completely damped systems, 28 Accelerations vanish with velocities, 29 Velocities are single-valued functions of configuration, 29. Chapter III. The Statistical Meaning of Irreversibility., Apparent irreversibility (progressiveness in time) of certain theoretically periodic processes, 30 Their periodicity, with eventual return to initial state, never observed in practice, 30 Explanation of this discrepancy: Macroscopic model illustrative of irreversibility of gaseous diffusion, 30 Return to initial state possible, but exceedingly rare (highly improbable), 31 The model is competent to illustrate also the highly improbable event of return to initial state, 32 Dynamical theory indicates not only occasional but periodic return to initial state, 32 A second model illustrates this also, 32 Evolution aspassage from less probable to more probable states, 35 Inadequacy of this "principle" : it is indefinite in failing to specify the characteristic with respect to which probability is reckoned; and it is incomplete in failing to draw attention to certain energy relations, 35 Irreversibility is relative, depending upon the means naturally available or arbitrarily permitted to operate upon the system, 35 Significance of this m organic world: Macroscopic irreversibility of diffusion processes in nature, 36 Need of a method of mathematical analysis to deal with cases intermediate, in specified degree, between the following two extremes: (a) Wholly indiscriminate (pure chance) operation upon material in bulk, (b) Wholly determinate operation, with nothing left to chance, upon materials discriminated and acted upon in detail, piece by piece, and circumstance by circum- stance, _36--This method must take account of degree of perfection of the mechanical and psychic equipment by which each organism reacts upon its environment, 37-Senses as a means of overcoming chance, 37-PhysicaI significance of our subjective sense of forward direction in time, which finds no expression in the differential equations of pure dynamics, 37-This subjectivetune sense may be related to the influence of initial conditions in dynamics,38-But the direction of evolution seems related rather to that directedness in Zdltl 18 f+rCt TtiC f aperi dic r S6emingly aPeriodic ?**, 38Inadequacy of thermodynamic method, 39-The linking of evolution with the ANALYTICAL SYNOPSIS OF CHAPTERS XX111 concepts of thermodynamics and statistical mechanics is instructive as suggesting a conception of the direction of evolution, the direction of increasing entropy, increasing probability, 39 This point of view, however, is inadequate for application to concrete cases of organic evolution, because data are furnished in terms unsuited to the methods of thermodynamics, 39 Neither are existing methods of statistical mechanics, as applied to molecules and the like, helpful; the instrument is ill adapted to the scale of the object, 39 New method needed, that shall accept its problems in terms of biological data, as thermodynamics accepts its problems in terms of physical data; a General Theory of State, an "Allgemeine Zustandslehre " 39. Chapter IV. Evolution Conceived as a Redistribution. Evolution viewed as a redistribution of matter among the components of a system, 41 System described by statement of mass of each component, and indication of value of certain parameters, 41 Analytical expression of history of system given by relations or equations established between the variables and parameters denning the state of the system, 41 Fundamental equations usually simplest in form of differential equations, 42 Particular form of equations of evolving systems, 42 General form of equations of evolving system, 43 Equations as applied to life-bearing system, 43 Definition of the components arbitrary but conclusions relate to the components as defined, 44 Relation of evolution, as here conceived, to the problem of the origin of species, 44 Inter-group and intra-group evolution, 44 Analytical indication of intra-group evolution, 45 Fundamental equations resemble in form the equations for an inertia-free or completely damped system, 47 Fundamental equations, as here given, may not cover all cases, but are at any rate of very wide scope, 47 Equations interpreted to include possible lag or lead effects, 47 Singular implications of lag and lead effects; possible relation to phenomena of memory and will, 48 Appearance of lag and lead effects in equations may, however, be spurious, 48. Chapter V. The Program of Physical Biology. Systematization and division of subject, 49 General mechanics of evolution, 49 Macro-mechanics and micro-mechanics, 50 Statistical mechanics as the connecting link, 50 Stoichiometry, the study of mass relations (material transformations), 50 Energetics or Dynamics, the study of the energy transformations, 50 Kinetics and Statics, 51 Equilibrium and steady states, 51 Moving equilibria, 51 Displacement of equilibrium; Le Chatelier's principle, 52 Sociological analogues of forces and "quasi-dynamics" (economics), 52 The term Physical Biology to be used to cover the territory indicated in this chapter, 52 Methods of obtaining data, 52 Chart of Program of Physical Biology, 53 Methods of elaborating data, 54. PART II. KINETICS Chapter VI. The Fundamental Equations of Kinetics of Evolving Systems. General case, 57 Some implications of the fundamental equations in their general form, 57 Equations of constraint, 58 Elimination of variables. Introduction of constants A, 58 Evolution with parameters P, Q and A constant, 58 Equilibria or steady states, 59 Number and character of XXIV ANALYTICAL SYNOPSIS OF CHAPTEES equilibria. Example: Fly population, 59 Fundamental equations transformed by introduction of excess of actual masses over equilibrium masses in place of the former, 60 Expansion in Taylor's series, and solution in exponential series, 60 Characteristic equation for exponential coefficients, 60 Significance of sign and character of roots X of characteristic equation, 61 Stability of equilibrium, 61 Mode of approach to equilibrium: Aperiodic and periodic (oscillatory) type, 61 Analytical confirmation and extension of a passage in Herbert Spencer's First Principles, 61 Zero or negative roots of the equilibrium equation: Unfit species, 62. Chapter VII. Fundamental Equations of Kinetics (Continued). Special Case: Single Dependent Variable. Law of population growth, 64 Population of United States, 66 Stability of equilibrium, 67 Experimental populations, 69 Diminishing population, 70 Growth of individual organism, 71 Autocatakinesis, 76. Chapter VTII. Fundamental Equations of Kinetics (Continued). Special Cases: Two and Three Dependent Variables. Interdependence of species, 77 Several types of interdependence, 77 Analytical characteristics of those types, 78 Effect of these characteristics upon the nature of the solution of the equation of Kinetics for two variables, 79 Concrete examples, 5 Martini's equation for immunizing diseases, 79 A special case noted by Watson, 81 The Ross malaria equations, 81 Example in parasitology, 83 Thompson's treatment of the case, 83-Objections to this, 87-Treatment of case by general equation of kinetics, 88-Nature of the solution: it represents a periodic or oscillatory process, 90-Comparison with observed facts according to L O Howard^ 90 Annihilation of one species by another, 92-Case of three depen-dent variables, 94-Relation of this to a practical problem in sea fisheries, 95Replaceable and irreplaceable components, 95-Limiting factors, 97-Liebig s law, 97 Chart of types of interdependence of biological species 98 * 2!r K' A*dysis of the Growth Unction. The form of thi function A+ ? T l aggregates 100-Demographic functions, 101-Survival M?^'^ i T r , mal Ege diataibu*^ HO-DemograPhic relations in normal population, 115-Rate of increase per generation, 118-Effect of selects slaughtering 119-Intelligence as a discriminating agency 20 (With MendeH J B. S Chapter X. Further Analysis of the Growth Function. Adjustment of the e teful produce, 132-nrnHnna 1QO T?~i j.- j ' -^ vvu^o uiv, muuiaiS ICept tor p^ss^s^it^s^SrPS-^;-- -:s-i; ANALYTICAL SYNOPSIS OF CHAPTEBS XXV from standpoint of domestic species is high efficiency from human standpoint, 135 Network of chains of interrelated species, 136 Transformation factors and their economic significance, 137. PART ill STATICS Chapter XI. General Principles of Equilibrium. Equilibria and stationary states, 143 Scope of Statics, 143 Kinetic, dynamic, and energetic definition of equilibrium, 143 Our chief interest here in stationary states not true equilibria, 145 General equilibrium condition, 145 Different types of equilibria, 146 Illustration: Malaria equilibrium according to Ross, 147 Metastable equilibrium, 151 Exceptional cases, 151. Chapter XII. Chemical Equilibrium, as an Example of Evolution under a Known Law. Case of simple balanced reaction, 152 Relation between "birth" rate and "death" rate of molecules, 153 The survival factor p (a) and life curve of molecules, 153 Reaction constant as a a force of mortality, 154 Chemical reaction as a case of survival of the fittest, 154 Analogy of chemical reaction to course of events in population of mixed biological species, 155 Presumptive mechanism of chemical reaction (Baly), 155 The fugaceous transitional state intermediate between chemical compounds (Schonbein), 156 Laws of thermodynamics, as determinants of the end state in an equilibrium reaction, are, in this case, the Law of Evolution of the system, 157Natural laws conveniently expressed as maximum or minimum principles, 157Law of organic evolution may be expected to take this form, 158 Law of chemical evolution is framed in terms of the system as a whole ; law of organic evolution must undoubtedly also be thus framed, 158 Law of equilibrium expressed in form of a minimum principle, 158. Chapter XIII. Inter-Species Equilibrium. Equilibrium condition in more particular form, 161 Numerical illustration, 162 Economic relationship of coefficients appearing in equilibrium condition, 163 Sources of information regarding biological equilibrium : Biological surveys, 164 Analysis of stomach, contents, 166 Intra-species equilibrium (with Mendelian inheritance), 170. Chapter XIV. Inter-species Equilibrium: Aquatic Life. Special occasion for demological studies of aquatic population, 171 Fishes as natural dragnets, 171 Aquatic food chains in relation to human food, 2 Importance of aquiculture for the future, 172 Loss of fertilizer through modern methods of sewage disposal, 172 Partial restoration of such material to human food supply through fisheries, 173 Different methods of census of marine population : dragnet; bottom samplers; recatching of marked catches; centrifuge; dilution culture, 173 The nannoplankton, 173 Work of Petersen in Kattegatt, 174 Quantitative estimates of principal groups of the marine population of Kattegatt, and their interrelation, 175 Summary of methods of marine biological census (Table), 176 Food chains, 176 Necessity of occupying ourselves with the more remote links of our food chain, 177 "Feeding our foods, " a species of symbiosis, 180 Agriculture and aquiculture, as mining and as manufacturing industries, 180 Resources but recently tapped, and others still untouched, 180 Food chains in aquatic species, 180 Wastefulness of long food chains, XXVI ANALYTICAL SYNOPSIS OF CHAPTEES 181 Economic value of shell fisheries owing to simple food chain coverting vegetation directly into human food (oysters, etc.); 181 Primary, secondary and tertiarv foods, 171 Cycles and the circulation of the elements in Nature. 183. ' Chapter XV. The Stage of the Life Drama. The tripartite world, 185 Atmosphere, 185 How the earth holds her atmosphere, 185 Cosmic losses from the atmosphere negligible, 188 Cosmic accessions to the atmosphere, 192Hydrosphere, 192 Aquatic atmosphere, 193 Lithosphere, 193 Cosmic accessions to lithosphere, 195 Composition of earth's crust, 195 Relation to composition of organism, 197 Similarity in composition of sea water and blood serum, 201 Significance of this as regards aquatic origin of terrestrial fauna, 202 Chemical correlation in soil and in organism, 204 Accessibility of valuable earth constituents, 206 Accessibility not in any direct relation to abundance, 206 H. S. Washington's classification of petrogenic (rock-forming) and metallogenic (ore-forming) elements of the periodic table, 207 Dissipating and concentrating processes in Nature, 208. Chapter XVI. The Circulation of the Elements : The Water Cycle. Circulation of elements vaguely realized by ancients, 209 Water requirements of human body, 210Water requirements of plants; rainfall as limiting factor, 211 Sources of supply, 213 Quantitative estimates of several items in water cycle, 213 Water cycle diagram, 215 Fraction of total water circulation taking part in life cycle, 216. Chapter XVII. The Carbon Dioxide Cycle. Combustion as an essential feature of the life process, 218 Analogy of flame arising from spark and life arising from germ, 218 Rarity of ignition except from pre-existing flame analogous to apparent impossibility of life originating except from preexisting life, 218 Oxygen as an inorganic food, 219 Plant nature of man in his attitude toward this inorganic food, 219-The carbon cycle, 220-Carbon as the organic element, 220 Source and gate of entry into the organic carbon cycle, 220 Some estimates of quantities involved in the carbon cycle, 220 Interrelation of green plants and animals, 221 Carbonization of dead vegetable matter and its significance for the industrial civilization of the present era, 221The present an atypical epoch: man living on his capital, 222-Attempts to establish the balance sheet of the earth's carbon economy, 222 Absorption of C02 in weathering of rocks, 223-Formation of CO2 by burning of coal, 224-The ocean as an equalizer regulating the C02 content of the air, 224-Unccrtainty as to net loss or gam of total C02 in atmosphere, 225 The oxygen cycle, 225-Oriinof atmospheric carbon dioxide and oxygen, 225-Carbon cycle diagram 226Loss of oxygen from the atmosphere, 228. Chapter XVIII. The Nitrogen Cycle. Natural demand and supply 229Seemmg abundance of nitrogen illusory, 229-Nitrogen cycle diagram,' 230-Cate of entry into nitrogen cycle, 232-Leak of nitrogen out of circulation 2ipLoss of nitrogen in combustion, distillation and coking of coal 233-Sk-mficance and rapid increase of by-product recovery type of coke ovens, 233-Other losses of combined nitrogen, 234-Accessory sources of combined nitronSJ f ^' 234 rHuman ^erference in nitrogen cycle, 236-Exploitation of guano deposits, 236-CMlean nitre beds, 236-Consumption of ANALYTICAL SYNOPSIS OF CHAPTERS XXV11 saltpeter as fertilizer and otherwise, 237 Origin of nitre beds, 238 Industrial nitrogen fixation processes, 239 Birkeland and Eyde nitric acid process. Cyanamide process. Haber ammonia process. Biicher cyanide process, 239 Combination of Haber process with Solvay soda process, 239 Ostwald oxidation process, 241 Meteoric rise of nitrogen fixation industry, 241 Its ethnological significance, 241 Economic and energetic significance of concentration, e.g. of supply of combined nitrogen, 243 Localized sources of concentrated supplies as centers of attraction in man's economic activities, 244 Total circulation tends to increase, 245. Chapter XIX. The Phosphorus Cycle, Immobile elements, 246 Natural phosphorus supply of soils, 246 Phosphorus cycle diagram, 247 Leakage of phosphorus from circulation, 248 Phosphate rock and the migration of phosphorus, 248 The role of fish and birds in the phosphorus cycle, 249 Soil losses of phosphorus, 250 Phosphate slag as fertilizer, 251. Chapter XX. Cycles: Conclusion and Summary. Circulation of chlorine and the alkalis, 252 The sea and the sun as a Soxhlet extractor, 252 Sodium chloride cycle diagram, 254 Differential behavior of sodium and potassium in the process of extraction, 255 Comparative rarity of potash in soils, 255 Effect of World War on potash market, 256 Circulation of sulphur, 256 Circulation of iron, 256 Summary of cycles, 257 Supply of plant food in soil, 257 Rate of participation of elements in cycles of nature, 258. Chapter XXI. Moving Equilibria. Principle of continuity, 259 Equation of slowly moving equilibrium; first approximation, 259 Higher approximations, 260 Special case : pace set by slowest member in a chain, 261 Radioactive equilibrium, 261 Equilibrium polygon, 266 Extinction of unadapted species, 266 Example of inaccuracy of first approximation, 268 Radioactive chains as cosmic clocks, 268 Geological time table, 269 Origin of elements and ultimate genesis of organisms, 269 Relative abundance of the elements, 271 Terminal stages of the earth's evolution: Geophysics and geochemistry, 273 Joly's theory of periodic melting of the earth's crust, 275 Organic moving equilibria, 276 Equilibrium polygon, 277. Chapter XXII. Displacement of Equilibrium. Perfectly general case of influence of change in parameters will not here be considered, 280 Principle of Le Chatelier, 281 Some common misstatements of the principle, 282 Early essayed application to biology, 283 Conditions of validity of the principle, 284 Extension of scope of rigorous applicability, 286 Area and rent, 288 Discussion of displacement of equilibrium independently of Le Chatelier's principle, 289 Case I: Displacement of equilibrium between food and feeding species, 289 Case II: Change of circulation through moving cycles, 292 Some significant cases of instability, 294 Vicious circles, 294 Cumulative cycles simulating orthogenesis, 296 Benign cycles, 297. Chapter XXIII. The Parameters of State. Topographic parameters, 300 Intensity factor of energy, 303 Simpliest examples of topographic parameters : volume, area, 301 Complexity of topography in organic evolution, 301 Simplification of problem by "substituting ideal upon which it is possible to operate, for intractable reality", 302 Empirical study of biogeography and ecology, 302 Conjugate parameters, 303 The intensity law in organic and xxviii ANALYTICAL SYNOPSIS OF CHAPTERS economic systems, 303-Rent as a measure or index of population pressure 304 But population pressure exists independently of rent, e.g., in species other than man, 304-Distant analogy of law of population pressure to gas law, 305-Law of urban concentration, 306-Biological background of population pressure, 307 Influence of population density on rate of reproduction (Pearl and Parker), 308 Influence of population density on duration of life (Pearl and Parker), 309 Topographic parameters during period of diffusion, 311 Willis' theory of Age and Area, 311 Climatic parameters, 317 Their laboratory investigation (Pearl and Parker), 319 Parameters of state and the analytical condition for equilibrium, 319 Thermodynamic analogy, 320 Inversion of typical problem of thermodynamics, 321 Systems of QuasiDynamics, 321. PART IV. DYNAMICS Chapter XXIV. The Energy Transformers of Nature. The fundamental equations of Kinetics do not exhibit any explicit reference to dynamical or energetic relations, 325 But certain of the components S are energy transformers, 325 Fundamental characteristics of energy transformers, 325 Cyclic working; output and efficiency, 326 Thermodynamic law of maximum output, 326 Reversible and irreversible processes, 327 Composite and coupled transformers, 327 Accumulators, 328 Chemical accumulators, 328 Growth, 328 Law of growth, 328 Anabions and catabions, 329 Systems of transformers, 329 Plant and animal as coupled transformer, 330 The World Engine, 331 Share of sun's energy that falls to different constituents of world, 331 Share falling to organic circulation, 331 Relation of transformer cycle to circulation of the elements, 334 Influence of limiting factors upon working of world engine, 334 Evolution of the World Engine, 335. Chapter XXV. Relation of the Transformer to Available Sources. Distributed and localized sources of energy, 336 Random and aimed collisions, 337 Negative correlation, 337 The correlating apparatus, 338 Component elements of correlating apparatus: Depictors, Receptors, Elaborators, Adjusters, 339 Receptor-effector circuit begins and ends in environment, 340 Significance of this, 340 Correlating apparatus not peculiar to living organisms, 340 Mechanical imitations of living beings (automatons) 341 Chess as a conventional model of the battlefield of life, 343 The biological contest considered in the light of the chess analogy, 343 Topographic map, centers of mobility and centers of influence as the elements of the game, 343 Zones of influence, 344 Collisions or encounters, 344 Zones of mobility, 345 Analytical statement of problem of organic conflict, 345 The behavior schedxile, 346 Specific productivity, 347 Effect of change in zone pattern, (Intraspecies evolution), 348 Biologic relation of economic value, 350 Effect of change in behavior schedule, 350 Rigid or automaton type and elastic or free-choice type of behavior schedule, 350 Relation between ideal and actual organism, 352 Effect of small departure from perfect adjustment, 353 Relation of economic value to physical energy, 354 Economic conversion factors of energy, 355 General or aggregate effect of individual ANALYTICAL SYNOPSIS OF CHAPTERS XXIX struggles for energy capture, 356 The law of evolution adumbrated as a law of maximum energy flux, 357- Statistical mechanics of a system of organisms, 358 Mean free path, 358 Frequency of collision and capture, 359 Influence of size of organism, 359 Curves of pursuit, 360 Random motion under a bias, 360 Use of models, 360. Chapter XXVI. The Correlating Apparatus, 362 Receptors, 363- Artificial receptors, 364 Significance of these in evolution of modern man, 364 Effectors, 366 Artificial effectors; industrial evolution, 367 Singular effects of industrial evolution, 368. Chapter XXVII. Extension of the Sensuous World Picture. The Elaborators, 371 The scientific world picture : Systems of coordinates, 372 The ego as a coordinate reference frame, 372 The ego immaterial, 373 Interpenetration of the egos, 374 Where is Mind?, 375 Fundamental premises and implicit assumptions, 376 Difficulty of shaking off preconceived premises, 377 Obstacle which this raises to understanding, 377 The communicators, 378 Orthogenesis in human evolution, 378 Orthogenesis does not suspend selection, 380 Importance of curiosity in evolution, 380. Chapter XXVIII. The Adjusters. Mechanistic and teleological interpretation of adjusters, 381 Significance of the future in the operation of adjustors, 382 The future that may be and the future that will be, 382 The doubtful cases, 383 Final causes or purposes not usually postulated when sufficient account can be given of events in terms of efficient causes (e.g., in terms of mechanistic explanation), 384 Adaptive adjustment of tastes, 385 Spencer's hedonistic principle, 386 Genuine utility for social service, 386. Chapter XXIX. Consciousness. Relation of consciousness to physical conditions, 388 Conditional relations, 388 A fundamental hypothesis admitted, 389 Consciousness is closely bound up with life processes and structures, 390 Consciousness dependent on metabolism. The personal element, 391 Consciousness possibly a general property of matter, 392. Chapter XXX. The Function of Consciousness. The contents of consciousness determined by past and present bodily states, 394 Operative relations of consciousness to physical conditions, 394 Not only knowledge but motive required in the working of the human organism, 394 Motivation in lower organisms appears fatalistic (simple tropisms), 395 Purposive action, 395 Dynamic psychology, instinctive drives to action, 396 Individual traits. Instinct of workmanship and self-expression, 396 Influence of special aptitudes, 399 The industrial and the personal problem of satisfying instincts, 400. Chapter XXXI. The Origin of Consciousness in Living Organisms. Why has nature resorted to consciousness as means for effecting adaptive reactions of organisms? 402 The problem of psycho-physical parallelism, 402 The double aspect theory of consciousness, 403 Physical analogies, 403 Physicochemical theory of consciousness as a state related to the transitional state of molecules in chemical reaction, 403 Argument of simplicity of structure may be invoked in favor of this theory, 404 Origin of consciousness, 404 Some elementary forms of consciousness perhaps a general property of all matter, 404 In that case not consciousness has been evolved, but only a particular type of consciousness, a consciousness integrated around an ego, 404. XXX ANALYTICAL SYNOPSIS OF CHAPTEBS Chapter XXXII, Energy Relations of Consciousness. Seeming conflict between directive power of consciousness and determinate character of physical events, 406 Possible explanations : First alternative possible inaccuracy of laws of dynamics, 406 Second alternative singular orbits with indeterminate motion, 407 Conception of Clerk Maxwell and of J. Boussinesq, 407 Third alternative possible influence of factors eliminated from equations of dynamics, 408. Chapter XXXIII. Review of the Correlating Apparatus. Tabular synopsis and classification of Depictors or Informants, 410 Epictors or Transformants, 411 Adjusters, 412 Internal adjusters, 412 Tabular synopsis of adjusters, 413 External adjustors, 414 Anatomical and physiological adjustment of social activities, 414 Economic adjustment of social activities, 415 Disadvantages of latter form of adjustment, 415 Its advantages or necessity in the human community, 415. Chapter XXXIV. Conclusion; Retrospect and Prospect, The life struggle in the modern community, 417 New character of this struggle : competition is principally within the species, 417 Organization of motives lags behind industrial organization, 418 Philosophy as a necessary part of scientific enquiry, 418 Classification of Sciences in relation to Self and External World, 419 Bertrand Russell's viewpoint regarding object and subject, 420 This leads to a natural division and classification of the sciences, 421 The ego as at once a Knower and a Wilier; hence the reaction of knowledge upon the emotions, 421, 424 The poetry of science, 425 Significance of emotional reaction of knowledge for our future evolution, 425 Evolution of the Self may have overshot the mark, 426 Man's opportunity to influence the destiny of his species by his own initiative, 427 Desirability of concerted action, 427 Of constructive optimism, 428 Evolutionary value of nurture and tradition, 428 Fallacy of cynical deprecation of potency of nurture, 429 Extension of Spencer's hedonistic principle, 430 How it explains the appearance of design in nature, 430 Such design can be neither proved nor disproved, and may therefore be made an article of faith, 430 Man may embrace the World Purpose for his own, 430 Survival value of such attitude, 430 Orthogenesis in field of ethics, 430 Once more the reaction of knowledge upon the emotion, 432 Evolution is not achieved by struggling against cosmic forces, but by adaptation to them (Claude Bernard, Sir Charles Sherrington), 433 He that survives must be in some measure a collaborator with Nature, 433 Evolution towards fusion of personal will with natural law, 433. I GENERAL PRINCIPLES CHAPTER I REGARDING DEFINITIONS Truth comes out of error more readily than out of confusion. Bacon. A definition is a purely arbitrary thing. If I choose to define a triangle as a plane figure bounded by four sides and having four angles; and if, also, I define a quadrilateral as a plane figure bounded by three sides and having three angles, I shall run into no logical conflicts; my geometry need in no wise depart from that of Euclid; I shall need to make no changes in existing works on geometry, beyond that of substituting throughout the word triangle for the word quadrilateral, and vice versa. But while a definition is in this sense, from the point of view of logic, a purely arbitrary thing, while my definition of a triangle as a four-sided figure may be admissible, it is by no means expedient. Thus the definition of terms, which naturally forms one of the first steps in the systematic treatment of any subject, may present no particular problems of logic, but it does present certain problems of expediency. In the geometrical example cited, the unusual definitions given, though quite permissible, are inexpedient for simple etymological reasons. Such a choice of terms would be misleading, and, instead of assisting the memory, would impose upon it an unnecessary burden. In this case the application of the principle of expediency is obvious to the point of being grotesque, the example having purposely been chosen to illustrate the principle in drastic fashion. But the framing of definitions at times involves more subtle considerations of expediency, so subtle in fact, that they may be overlooked, or misunderstood, and a problem which is, in truth, a problem of definition, falsely masquerades as a problem of fact. Certain pseudo-problems of science have owed their origin to a failure to realize this circumstance. 1 1 On the other hand, some very fundamental advances of science are, upon critical examination, found to rest essentially upon the establishment of a 3 4 ELEMENTS OF PHYSICAL BIOLOGY The writer of the book of Genesis shows good judgment. Our legendary forebear, the originator of the first biological system of nomenclature, sees each creature first, and thereupon names it. We have not always been equally wise. Sometimes we have tried to invert the method; we have found or made a name, and then gaily set forth on an expedition to discover the thing that should answer to that name; we have hunted the Jabberwock. Forgetful of the wisdom of Mephistopheles : Derm eben wo Gedanken fehlen Da stellt ein Wort zur rechten Zeit sich ein we have given way to an inherent bias of the human ,mind described in characteristic fashion by H. G. Wells2 : . . . . when we have a name we are predisposed and sometimes it is a very vicious predisposition to imagine forthwith something answering to the name If I say Wodget or Crump, you find yourself passing over the fact that these are nothings, .... and trying to think what sort of a thing a Wodget or a Crump may be. You find yourself insensibly, by subtle associations of sound and ideas, giving these blank terms attributes. 8 So the biologist of the past generation, finding in his native vocabulary the words animal and plant, forthwith proceeded in an effort to establish precise distinctions between animals and plants, never giving any thought, it would seem, to the fact that these names had already been parceled out generations ago, by "popular" consent, by unscientific persons without any regard to fine distinctions. There is clearly, here, the tacit assumption that because two distinct words are found in the vocabulary, therefore two correspondingly distinct things exist in nature. In point of fact, we know well enough (though we may not at all times have this knowledge clearly in the focus of our consciousness) that in nature many things form finely graded series, with extremes at the two ends, extremes to which judicious definition. A notable instance of this is the enunciation of the principle of the survival of the fittest, which is essentially of the nature of a definition, since the fit is that which survives. Regarding the epistemological significance of definitions compare A. N. Whitehead and B. Russell, Principia Mathematica 1910, vol. 1, p. 12. * H. G. Wells, First and Last Things, 1908, p. 32. 8 "Gewohnlich glaubt der Mensch, wenn er nur Worte Es mtisse sich dabei auch etwas denken lassen." REGARDING DEFINITIONS 5 ^ our vocabulary has lent more or less definitely associated names, but with no definite line of demarcation between. Examples of this are \ innumerable. We speak of objects as being red, orange, yellow, green, blue, violet, etc. There is nothing in nature to correspond to such staccato classification of colors: the visible spectrum runs continuously from a wavelength of about 8 x 10 ~* mm. (extreme red) to about 4 X 10~4 mm. (extreme violet). Cases therefore must necessarily arise when we are in doubt whether to call a thing blue, or green, for example; and such doubt can be resolved, if at all, only by arbitrary definition. The question is not "what is green, and what is blue," but, at best, "what shall we agree to call green, and what blue." It lies in the nature of the mechanism by which we enter into possession of our knowledge, that problems of definition of this kind *- arise. We are equipped with two separate and distinct senses, the one responding to electromagnetic waves ranging from about 4 x 10 ~4 to 8 x 10 ~4 mm., light waves; the other to somewhat longer waves otherwise of the same character, heat waves. Accordingly we have two separate terms in our language light and heat, to denote two phenomena which, objectively considered, are not separated by any line of division, but merge into one another by gradual transition. Here the question might be raised whether an electromagnetic wave of a length of 9 x 10 ~ 4 mm. is a light wave or a heat wave. The answer is obvious: Call it what you please, it is merely a question of arbitrary definition. We must beware of .... that false secondary power '* By which we multiply distinctions, then Deem that our puny boundaries are things That we perceive, and not that we have made. Wordsworth. Definitions in Biology. The attempt to establish a rigorous distinction between "animals" and "plants" may be similarly regarded. Expediency demands that if these terms are appropriated for exact scientific use, their sense, when so used, shall, if possible, be reasonably near akin to the sense commonly associated with these words. The difficulties encountered in seeking to establish a satisfactory line of division between animals and plants were long regarded as difficulties in a problem of fact. It was thought that some biologi* cal principle must be sought which divided animals from plants. 6 ELEMENTS OF PHYSICAL BIOLOGY The truth is, of course, that we may define "animals" and "plants" any way we please- as for instance by reserving the term, plant for an organism possessing cellulose' but whether such definition is "correct" or "satisfactory" is not a question of biological fact, it is a question of expediency. It is not a question whether there is any definable difference between animals as a class and plants as a class, nor what this difference is, but whether it is expedient to retain for purposes of strict scientific classification the popular terms "animals" and "plants," which were not originally founded upon any rigorous examination of facts; and if so, where we should, by definition, draw the line of separation. When the problem is viewed in this way the difficulty of distinguishing between animals and plants vanishes. In the case of the higher forms of life it is easy to establish biological distinctions that do not conflict with the popularly drawn lines of division. In the case of certain lowly forms of life popular distinctions cannot exist, since these forms are not known to the public except through biological publications. And the biological line of demarcation we can, by definition, draw arbitarily where we choose, or, better perhaps, we may say that the terms "animal," "plant," do not correspond to any fundamental objective distinction and, though conveniently applied to certain common forms of living matter, are entirely unnecessary 4 and only introduce difficulties of definition and classification when applied to certain simple organisms. What difference does it make whether we call Volvox a plant or an animal? Whether it is a plant or an animal is merely a matter of definition, not a question of biological fact. Somewhat similar remarks apply to the narrower divisions into which the biologist divides the world of living organisms. Disputes as to what constitutes a species are fruitless. "A species is a thing described as such." This is simply a matter of definition. If on grounds of expediency one definition is preferable to another, it may be well to urge its general adoption. But its adoption or rejection will neither add nor subtract one jot from our stock of ascertained facts. It is necessary to guard against the error of disputing about mere words. Not always does this error strut about in such blatant form as in the example quoted by Fechner: S. Sachs, in a book published 4 R. W. Glaser, Science, 1918, vol. 48, pp. 301-302: "We are justified at present in not classifying viruses either wit|i plants or animals." KEGARDING DEFINITIONS 7 in 1850, takes the astronomers to task for their presumptuous speculations: "How do they know that the star they call Uranus is Uranus?" If any one should think that in our day it is no longer necessary to guard against errors of this kind (though less gross, perhaps), let him consider such a question as this: Is not the perennial debate between vitalism and mechanism a quibble about words? Is not the whole situation summed up accurately in the words of L. J. Briggs: 5 "The mechanism of plant processes not at present explainable on a physico-chemical basis would be termed by the vitalistic school "vital," by the physico-chemical school "unknown"? And in searching for the essential characteristics of life, those that should finally and conclusively distinguish the living from the nonliving, are we not just searching for the thing in nature that should correspond to a word in our vocabulary? Are we not hunting the Jabberwock? Definitions of Life. The difficulty of giving a precise meaning to the word life has been realized probably by everyone who has ever seriously attempted a definition. Herbert Spencer remarks: Classifications are subjective concepts, which have no absolute demarcations in Nature corresponding to them .... Consequently, when we attempt to define anything complex .... we can scarcely ever avoid including more than we intended, or leaving out something that should be taken in. Thus it happens that on seeking a definition of life, we have great difficulty in finding one that is neither more nor less than sufficient. Nevertheless he proceeds to establish his definition of life: "The continuous adjustment of internal relations to external relations." 8 It cannot be said that Spencer has been very happy in this choice of a definition or that he has been at all successful in avoiding the very pitfalls which he himself so clearly points out. For obviously many purely mechanical systems fall under this definition. It would, for example, include a windmill provided with a device automatically turning its arms into the most favorable plane according to the direction of the wind. 7 Indeed, in a sense it is true of every physical 6 L. J. Briggs, Jour. Washington Acad. Sci., 1917, vol. 7, p. 89; compare also E. M. East, Mankind at the Crossroads, 1923, p. 21. 6 Herbert Spencer, Principles of Biology, section 30. 7 Compare the following : "No one has yet succeeded in formulating a cleancut definition of the limits of the reflex either at its lower or its higher extreme, and perhaps no one ever will; for the whole list of behavior types, from machines to men, probably form a closely graded series." C. J. Herrick: The Evolution of Intelligence and Its Organs. Science, 1910, vol. 31, p. 18. 8 ELEMENTS OF PHYSICAL BIOLOGY system that it "adjusts its internal relations to external relations." For this statement simply implies that there is a tendency for the establishment of equilibrium between a selected portion of a physical system, and the remainder, the environment. Thus, for example, if the system 2H2 + 2 is left to itself hi a suitable vessel at 1480C.8 H2 and one atmosphere pressure, the ratio ^rp: which we may term an "internal relation" of the system, assumes the value 0.0002. If now the external conditions of temperature and pressure are changed "FT to 2929C. and one atmosphere pressure, the internal relation rrr-z adjusts itself to the new external condition and acquires the value 0.11. With better judgment than Herbert Spencer, Sir Edward Schafer9 frankly evades the definition of life. He remarks : The ordinary dictionary definition of life is "the state of living." Dastre, following Claude Bernard, defines it as "the sum total of the phenomena common to all living beings." Both these definitions are, however, of the same character as Sidney Smith's definition of an Archdeacon as "a person who performs archidiaconal functions." I am not myself proposing to grapple with a task that has proved too great for the intellectual giants of philosophy, and I have the less inclination to do so because recent advances in knowledge have suggested the probability that the dividing line between animate and inanimate matter is less sharp than it has hitherto been regarded, so that the difficulty of finding an inclusive definition is correspondingly increased. It is, indeed, an elementary historical fact that, as knowledge has advanced, the scope embraced in the term "vital" processes has continually decreased, since Wohler took the first cut out of it in 1828 by the synthesis of a "vital product" (urea) in the laboratory; and the field of known physico-chemical processes going on in living organisms has correspondingly increased. For the rest, the most uncompromising vitalist does not deny that some, at least, of the processes going on in living matter are physico-chemical. Even so fundamentally biological a process as the stimulation of an ovum to development we have learnt to effect by purely physical means. Alleged Characteristics of Living Matter. On the other hand some of the features commonly ascribed to living matter as its peculiar 8 W. Nernst, Theoretische Chemie, 1913, p. 713. 9 E. A. Schaefer, Presidential Address at Dundee Meeting of Brit Assoc Adv. Sci. 1912. EEGAEDING DEFINITIONS and characteristic attributes seem Irrelevant to the point of triviality. "^his.remark applies particularly to the distinction sometimes claimed for living matter, that it grows "from within," as distinguished from crystals, which, in a suitable mother liquor, "grow from without." There may or may not be many and profound differences between a bacterial colony growing in a culture medium, on the one hand, and on the other hand a mass of crystals growing in a supersaturated solution. But whether the growth takes place from within or without is merely an accident of structure. If a droplet of chloroform is brought near to a glass particle coated with shellac, the drop flows around the particle, engulfs it, absorbs the shellac coating and finally rejects the "undigested" glass particle. 10 The droplet thus grows "from within." In point of fact "growth from within" is the rule and not the exception in chemical systems. For what do we mean by growth? We mean the increase of the mass of one component of a system at the expense of another. It is precisely the same thing as that which occupies the center of attention of the physical chemist, though he does not ordinarily call it growth. In fact, he does not find it necessary to give it any particular name, for, being accustomed to the use Ci'YYI of mathematical methods and symbols, he simply writes it -=- , rate Cit d /m\of increase of mass with time, or, more often, T.\ I, rate of increase of concentration (mass/volume) with time. And in homogenous systems, at least, which (on account of their comparative ease of theoretical and experimental treatment) figure prominently in the physical chemistry of today, growth is necessarily from within. Some writers (J. Loeb, The Organism as a Whole, 1916, p. 28) have seen a characteristic feature, peculiar to living organisms, as distinguished, for example from crystals growing out of a solution, 10 "Let it be clearly understood that this illustration is here quoted, not as an example of life-like analogies in the world of non-living matter; nor as a veiled suggestion that such a drop of chloroform represents even a modest degree of success in the artificial imitation of life; nor yet again as an argument that the conduct of amoeba can today be fully accounted for on a physicochemical basis; this example was cited merely to show that "growth from within" cannot be claimed as a distinguishing characteristic of living matter. For further discussion of so-called simulacra vitae see McClendon, Physical Chemistry of Vital Phenomena; Burns and Paton, Biophysics, 1921, p. 403. 10 ELEMENTS OF PHYSICAL BIOLOGY in the fact that the latter grow by a physical process, the former by chemical processes. Leaving aside the question as to whether there exists any fundamental distinction between physical and chemical processes, at most the point to which attention is drawn by these authors would class living organisms with chemical, as distinguished from physical systems, but would furnish no basis whatever for separating organisms in a class by themselves from other chemical systems. This is not saying that they are not in a class by themselves, but only that the distinction suggested fails in effect. It has similarly been urged, as a distinction between the growth of a crystal and that of an organism, that the former will grow only in a supersaturated solution of its own substance, while the latter extracts from an unsaturated solution the substance needed for its anabolism. This is really the same distinction in another form. It may distinguish the organism from the growing crystal, but leaves it m... one class with any chemically reacting system whatever, since in the case of the latter also there is "growth," i.e., formation of one or more products of reaction, in a system which need not be physically supersaturated in the narrow sense in which the crystallizing solution is. In a wider sense11 the system may indeed be said to be supersaturated with regard to a chemical substance that is formed within it but in the same sense a system can probably be said to be supersaturated with regard to the substance of a bacterial colony growing therein. Neither can we subscribe to the view set forth by J. Loeb (The Organism as a Whole, 1906, p. 29), that the synthesis of specific materials from simple compounds of non-specific character distinguishes living from non-living matter. In every chemical reaction specific materials are formed. In a mixture of hydrogen, chlorine, and nitrogen, the hydrogen and the chlorine unite, leaving the nitrogen on one side unchanged. This is merely a brutally simple example of a universal fact. Chemical reaction is always selective. And if "complexity" is to be made the characteristic of life processes, then the question immediately arises, what degree of complexity is required to place a given process in the category of life processes? "Namely in the sense that it is metastable, that is, its thermodynamic potential is not at a minimum. EEGARDING DEFINITIONS 11 Reproduction. Another characteristic that has been cited by some as exclusively peculiar to living organisms is the power of reproducing their kind. "How, says Driesch in effect, can a mechanism provide for its own reconstitution? No machine known to us is able to construct another like itself, nor can it repair its own parts." 12 Undue emphasis on this alleged distinction between living and nonliving machines seems ill advised, for two reasons. In the first place, though it may be true that no man-made engine exists that performs the functions of self-repair and self-reproduction, no one has ever attempted, so far as I know, to demonstrate that no such engine can be built. Anyone who should be disposed to regard this objection as specious should reflect for a moment on the amazing development in technical arts within the last thirty or forty years. Half a century ago one might with equal justice have pronounced flight a fundamental, essentially biological characteristic of birds, incapable of duplication by man-made engines. But in another, perhaps more significant respect, we must regard as misplaced the emphasis sometimes laid on the power of reproduction in organisms, and its absence in human artefacts. It is based on an exaggerated conception of the part played by the parent in the making of the offspring. This probably has its origin in the instance of reproduction that to us is naturally of supreme interest, the reproduction of man. As a mammal, the young human organism grows within the parent body, and seems to us to be in some way fashioned by the parent; this conception must be at the basis ofThe alleged ! distinction between organic reproduction and the incapacity of ; '. ; non-living engines to reproduce their kind, for without such conception the comparison would lack all parallel. Now, in point of fact, we need but call to mind the familiar hatching of a chick to realize that the part necessarily played by the parent in the formation of the young individual is really very restricted. The process in this case goes on, for the most part, in complete isolation from the parent. 13 12 H. C. Warren, Jour. Philos., Psychol. and Scientific Method, vol. 13, 1916, p. 36. 13 Compare E. G. Conklin, Heredity and Environment, 1918, pp. 99,45, 109: "The hen does not produce the egg, but the egg produces the hen and also other eggs We know that the child comes from the germ cells and not from the highly differentiated bodies of the parents, and furthermore that these cells are not made by the parents' bodies but IZ ELEMENTS OF .PJtilKlUAJLi As for the initiation of cell division of the ovum, we now know that, in some cases at least, this can be effected by ordinary physical means. Recent development in experimental embryology suggest a more rational view of this process of self-reproduction of the living engine, a view which strips it of at least some of its mystery, and which certainly takes from it any force it might otherwise have had as a basis for distinction between living and non-living matter. If, after the first division of the ovum of a frog, the two cells are separated, each will under suitable conditions develop into a separate and complete, normal organism. These two organisms A and B are, in fact twin brothers or sisters. No one would for a moment entertain the thought that in this case A reproduces B, or vice versa. Now suppose that in some way, after the first division, A alone grows into a complete mature organism, while the single cell B remains attached to it, say for six months. At the end of this time it is separated, and stimulated to start its growth into a frog. We would ordinarily describe this state of affairs by saying that A reproduced B as offspring, that B was the child of A. In point of fact it is merely a delayed twin brother or sister of its elder brother or sister A. u A had little or nothing to do with the production of B; the latter grew, very much in the same way as A grew in its own time. That nature has evolved, in surviving races, this method of delayed development, so as to stretch out the totality of living organisms in a long chain, a succession in tune, is of course a fact of most fundamental importance, the significance of which will deserve our profound contemplation. One of its consequences has been to render possible a practically infinite number of organisms, built from a finite and quite restricted amount of matter, the same substance being used over and over again, for it is literally true that we live on our forefathers. Had all these cells have arisen by the division of antecedent germ cells Parents da not transmit their characters to their offspring, but these germ cells in the course of long development give rise to adult characters similar to those of the parent." 14 The perhaps somewhat doubtfully authenticated cases of fetus in fetu, "those strange instances in which one might almost say that a man may be pregnant with his brother or sister," add a touch of realism to the discussion here presented. For further data on this singular subject see G. M. Gould and W. L. Pyle, Anomalies and Curiosities of Medicine, 1897, pp. 199 et seq. Compare also in this connection, the phenomenon of pedogenesis; see for example, G. H. Parker, Psyche, 1922, vol. 29, p. 127. , these organisms sought to grow simultaneously, their career would have been stopped by lack of material. , If anyone should object that these reflections leave out of account entirely the r61e of sex in reproduction, with all the complex phenomena of the fusion of gametes, the mingling of chromosomes, and biparental inheritance, the obvious reply is that these phenomena are now known to be less fundamental than they formerly appeared; that reproduction of an organism can very well take place without them; and that therefore they may at most serve to distinguish certain forms of life from non-living matter, but they cannot possibly be made the basis of a distinction between living matter in general and that which we commonly describe as non-h'ving. , Vital Force. If we have cause to hesitate in defining hie,_ still more is it the part of wisdom to be very conservative in the coming and use of such phrases as vital force, nerve energy, and the like. Shall we not do well to follow the biblical example, and wait, to name the animal, until it is physically present to our senses? Or, to pass from legend to the world of scientific fact, let us borrow, if we^ can, the method of the physicist: He discovers that a quantity f mv possesses certain important properties. Then, he proceeds to name it: Energy, in particular, kinetic energy. But biologists have been disposed sometimes to adopt the reverse procedure: they have named a vital force, a nerve energy, a mental energy, and what not, and now they entertain the pious hope that in due time they may discover these "things." That there is something radically at fault with such terms is evident from the fact that forces and energy are magnitudes, and "to define a magnitude and to say how it is measured are one and the same thing." 15 But who has ever told us how to measure vital force18 and such like? Physical Chemistry of Structured Systems. In the physical chemistry of today structure, that is to say, geometrical configuration, plays a subordinate rdle. For obvious reasons the theory of chemical reaction in homogeneous, or in heterogeneous systems of comparatively simple form, is more approachable than that of systems which possess intricate structure, resulting in complicated mechanical 18 Nature, September 25, 1922, p. 405. 18 G. Bunge, in his Physiologic and Pathologic Chemistry, 1902, p. 1, remarks : "I regard vital force as a convenient resting place where, to quote Kant, 'reason can repose on the pillow of obscure relations.'" Curiously enough this damning admission is made by an advocate of vitalism. 14 ELEMENTS OF PHYSICAL BIOLOGY interactions of their parts, in accompaniment of chemical reaction. In technical practise, too, reactions in homogeneous systems (solution, gas) are common, and where there is heterogeneous structure, this is usually of a form very simple as compared with the complex biological structures. But this comparative absence, from physico-chemical discussion, of reference to structure, to geometrical features, is not due to any inherent characteristic property of chemical systems, as contrasted with the structurally complex organic systems: the reason for the simplicity is to be found in ourselves. It is not a physical phenomenon of the thing observed, but a psychological phenomenon in the observer. Physical chemistry is still a comparatively young science, and naturally the simpler phenomena have been sought out for first attention. This is not because complex physico-chemical structures do not exist, nor even because they are unimportant. On the contrary, it is to be expected that the future will bring important developments in this direction, as followed, for example by Sir William Bayliss in his work Interfacial Forces in Physiology, The rate of formation, the rate of growth, of a chemical substance, is a definite function of its environment. In a structureless system the nature and state of this environment is defined in comparatively simple terms (e.g., by stating the concentration of each of the reacting substances) . But in a system possessing structure, the environment of a given portion of the system depends on the structure, the topography of the system, which, in general, will be variable with the time. In particular, the structure may be such that a given substance or complex of substances carries its own immediate environment around with it. The rate of formation (growth) of that substance will then depend largely upon the mechanical properties of those portions of the system which accompany this substance or complex in its travels through the system. The complete discussion of a system of this kind may well fall outside the scope of present day physical chemistry, not because it is inherently foreign to that branch of science, but because no case of this kind, sufficiently simple to invite discussion on a mathematical and physico-chemical basis, has clearly presented itself.17 ^Compare W. M. Bayliss, Physiology, 1915, p. XI, "All that we are justified in stating is that, up to the present, no physico-chemical system has beea-**l|| EBGARDING DEFINITIONS JLO Yet there is absolutely nothing in such a case that in principle places it outside the pale of physico-chemical science. It is largely as the result of intentional selection of simple conditions that the systems with which the chemist ordinarily deals (outside of biological chemistry) are comparatively structureless. We can, in fact, even now lay down certain general observations with regard to structured physico-chemical systems. Let us consider a system of this kind in which local conditions are subject to variation from point to point and from instant to instant. We fix our attention on some one component which requires for its growth certain definite conditions of its immediate environment. If this component is associated with a structure whose geometrical and mechanical properties secure and maintain for it a comparatively constant suitable environment amid the changing conditions of the system, then that component will grow. Furthermore, the several components will compete with greater or less success for the material available for their growth, in proportion as their structure is more or less perfectly adapted to secure and maintain for them a suitable environment. The chemical dynamics of such a system, that is to say, the laws governing the distribution of matter among its several components, may evidently assume a fundamentally different character from that to which we are accustomed from our study of ordinary structureless systems. For in these latter the arrangement and rearrangement of matter within the system depends chiefly on chemical coefficients (affinity coefficients), and scarcely at all on geometrical features. In structured systems, on the other hand, there is the possibility that geometrical and mechanical features may play the dominant role. This possibility will present itself particularly in those systems which receive a continuous or periodic supply of free energy, for instance in the form of illumination. Here the advantage will go to those structures that are adapted to direct available energy into such channels as lead to the maintenance of the environment required for their growth. 1* But a little reflection shows that this is precisely the princimet with having the same properties as those known as vital; in other words, none have, as yet, been prepared of similar complexity and internal coordination. 18 It should be observed that nothing has been said of life in describing the system. The system may or may not comprise living organisms, the argument pie which governs survival in the struggle for existence among living organisms. Hence we may say: The laws of the chemical dynamics of a structured system of the kind^ described will be precisely those laws, or at least a very important section of those laws, which govern the evolution of a system comprising living organisms. For it is precisely structured systems of the kind considered above that are presented to us in living organisms growing in an "environ- ment." Application to Biology. The several organisms that make up the earth's living population, together with their environment, constitute one system, 19 which receives a d :1 y supply of available energy from the sun. Each Individual is composed of various chemical substances assembled into a definite structure and capable of growth, i.e., of accretion out of the environment by chemical reaction1 provided a suitable medium or environment is offered. Moreover, each mobile organism carries with it a travelling environment, suitable for the growth of its substance. It maintains this environment by virtue of the peculiar mechanical properties associated with its structure, whereby it is enabled to turn to this use, directly or indirectly, the available energy of the sun's light. And while the travelling environment may not be absolutely constant, remains the same. This suggests that a term, such as life, so vague that it defies definition, is perhaps not likely to play an important part in any exact argument; -we may, indeed, find it wholly unnecessary. It may, in time, in the literature of exact science, meet with the fate of the word cause: a term of rare and at best incidental occurrence in records of exact investigations. 19 This fact deserves emphasis. It is customary to discuss the "evolution of a species of organisms. 3 ' As we proceed we shall see many reasons why we should constantly take in view the evolution, as a whole, of the system [organism plus environment]. It may appear at first sight as if this should prove a more complicated problem than the consideration of the evolution of a part only of the system. But it will become apparent, as we proceed, that the physical laws governing evolution in all probability take on a simpler form when referred to the system as a whole than to any portion thereof. It is not so much the organism or the species that evolves, but the entire system, species and environment. The two are inseparable. "The organism, as Uexkull teaches us, must be studied, not as a congeries of anatomical and physiological abstraction, but as a piece of machinery, at work among external conditions," 0, C. Glaser, Science, vol. 21, 1910, p. 303. it is more nearly so than the more remote portions of the system, and keeps within such limits of variation as are compatible with the survival of the organism or its species. A concrete illustration may help to make this point clear. Many aquatic forms of life are constantly bathed in a saline solution sea water. Their body fluids are accordingly in equilibrium with this environment. Variations in the salinity of their environment, if they exceed certain comparatively narrow bounds, are apt to be fatal to such organisms. The higher organisms have made themselves (largely) independent of their immediate environment. Their tissues are bathed from within by a fluid (the blood) which they carry around with them, a sort of "internal environment." 20 The degree of perfection with which this constancy of the internal or traveling environment, independently of the external environment, is developed, increases as we ascend the biologic scale. This is lucidly set forth, for example, by Claude Bernard:21 Chez tous les 6tres vivants le milieu inte'rieur qui est un produit de 1'organisme, conserve les rapports ne'ce'ssaires d'Schange avec le milieu e'xte'rieur ; mais & mesure que 1'organisme devient plus parfait, le milieu organique se sp< cifie et s'isole en quelque sorte de plus en plus du milieu ambiant. It is the peculiar structure and the mechanical properties of the organism that enable it to secure and maintain the required environment (including the milieu interieur). The higher animals, in particular, are provided with an intricate apparatus, comprising many members, for securing food (internal environment) as well as for warding off hostile influences. 20 "Etant donne* que 1'eau de mer a un contact si intime avec les organismes de la mer et que non seulement elle les entoure de ses flots, mais qu'elle traverse leurs branchies et impregne en partie les corps des inverte"bre"s, il semble assez justind de la placer dans la m&ne cate"gorie que les autres liquides physiologiques." S. Palitzsch, Comptes Rendus de Carlsberg, vol. 10, part 1, 1911, p. 93. Compare also the following: "Not only do the body fluids of the lower forms of marine life correspond exactly with sea water in their composition, but there are at least strong indications that the fluids of the highest animals are really descended from sea water .... the same substances are present in both cases, and in both cases sodium chloride largely predominates." L. J. Henderson, The Fitness of the Environment, 1913, pp. 187-188. See also ibid., pp. 116 and 153; H. F. Osborn, The Evolution and Origin of Life, 1917, p. 37 ; D'Arcy W. Thompson, Growth and Form, 1917, p. 127. 21 Introduction a l'6tude de la me'decine expe"rimentelle, 1885, p. 110. The increasing independence, as we ascend the biological; ~ jale, which the organism displays toward its more remote environment, is thus accompanied by a parallel increase in the perfection of the apparatus by which this independence is earned. Here again we may quote Claude Bernard : 22 A mesure que 1'ori s'eleve dans l'e"chelle des etres, ces appareils deviennent plus parfaits et plus eomplique's; ils tendent & affranchir completement 1'organisme des influences et des changements survenus dans le milieu exte"rieur. Chez les animaux inverte'bre's, au contraire, cette independence visa-vis du milieu exte"rieur n' est que relative. The Policy of Resignation : Its Parallel in Other Sciences. Whatever may be our ultimate conclusions, we may do well to adopt at least as a temporary expedient the policy of resignation; with Sir Edward Schafer we may abandon the attempt to define life. Perhaps, in doing this, we are following historical precedents : Geometers have had to resign themselves to the fact that Euclid's parallel axiom cannot be proved. But as the reward of this resignation came the new geometries of Bolyai, Lobatchewski and Riernann. Enlightened inventors have abandoned the attempt to build a perpetual motion machine; but again, resignation is rewarded with the recognition of a fundamental law, the law of conservation of energy. Physicists, following Einstein, have abandoned, for the time being at any rate, the attempt to determine experimentally the earth's absolute motion through space. The reward has been the theory of relativity, one of the greatest events in the history of science. The whole development of science, especially in recent years, is a record of tearing down barriers between separate fields of knowledge and investigation. Little harm, and perhaps much gain, can come from a frank avowal that we are unable to state clearly the difference ;' between living and non-living matter. This does not in any way ' commit us to the view that no such difference exists. l For the present, then, we shall adopt the position that the problem is essentially one of definition. The question is not so much "What is life," but rather, "What shall we agree to call life?" And the answer, for the present at any rate, seems to be that it is immaterial how we define life; that the progress of science and our understanding of natural phenomena is quite independent of such a definition. 22 Ibid. We shall, wherever convenient, continue to employ the terms life, living organism, merely as a matter of convenience. This use of the terms does not imply or presuppose any precise distinction between living and non-living matter; it merely rests upon the fact that in most cases ordinarily met there is essentially universal agreement as to whether a portion of matter is to be classed in the first or in the second category. We will adopt the policy of Sir William Bayliss : If asked to define life I should be inclined to do as Poinsot, the mathematician did, as related by Claude Bernard: "If anyone asked me to define time, I should reply: Do you know what it is that you speak of? If he said Yes, I should say, Very well, let us talk about it. If he said No, I should say, Very well, let us talk about something else." The ideal definition is, undoubtedly, the quantitative definition, one that tells us how to measure the thing defined; or, at the least, one that furnishes a basis for the quantitative treatment of the subject to which it relates. We have already spoken of evolution. Most of what follows will relate directly or indirectly to evolution. It will be well here, while discussing definitions, to establish a definition, a conception, of evolution that shall, as far as may be, have the quantitative stamp. CHAPTER II EVOLUTION DEFINED Nature must be considered as a whole if she is to be understood in detail. Bunge. As has been abundantly made plain, the choice of a definition is a matter of expediency. In adopting, for special use in exact science, a term already in general use, we must seek, so far as possible, to embody in our definition the fundamental and essential features of the concept denoted by the term as used popularly and by the best workers, thinkers and writers. 1 In so far as there is divergence in the use of the term, it may be well to frame the definition broadly, so as to cover a wide range of phenomena and lead to a comprehensive view of natural events, corresponding to the essential unity of nature. In this way we shall be most likely to see the facts of nature arraying themselves in a natural order, and to achieve that economy of thought which is secured by a well devised system of classification. Facts which naturally belong together will, then, be found together, in our system, in the same or in neighboring pigeon- holes. Now if we seek to analyze what is in our minds when we speak of the evolution of a given system, we find' and on this probably all are agreed that the fundamental, the central thought, is that of the history of the system. But the concepts of the history and of the evolution of a system, though related, are not identical if they were, one word would suffice to denote the single concept. The popular and also the scientific conception of evolution contains as an essential feature the element of progress, of development. We would not ordinarily class as evolution the history of such a system as a swinging pendulum, or a celestial body circling in its orbit, in so far 1 Compare Bertrand Russell, Analysis of Mind, 1921, p. 197: "The use of the word comes first, and the meaning is to be distilled out of it by observation and analysis." "In each case the work consists chiefly in making explicit processes which are instinctive," as J. W. N. Sullivan (Aspects of Science, 1923, p. 24) remarks apropos of certain other matters. 20 EVOLUTION DEFINED 21 as these motions are purely periodic or cyclic. In the history of such systems the element of progression in time, of development, is lacking. They repeat in endless succession the same series of events. The hand of the clock, like a symbol of perpetual youth, goes through its daily double cycle, making no distinction between yesterday, today and tomorrow. It is the calendar that reminds us we grow older year by year, the calendar that turns a new and different leaf each o!ay. "The book of Nature is the book of Fate. She turns the gigantic pages leaf after leaf, never returning one. . . . . "2 But, to characterize the kind of history we speak of as evolution, it is not enough that each day be unlike every other; it is not merely that a system never passes twice through the same state; 3 not merely that a biological species never retraces its steps, 4 or that "when a race has lived its term it comes no more again." 5 Evolution not a Mere "Changeful Sequence." Such a statement as those cited in the preceding paragraph alone is insufficient to distinguish evolution as a progress from merely a changeful sequence', it is insufficient to define the direction of evolution.6 For if the world's events taken in historical order A, B, C . . . are a changeful sequence, the same is also true of the inverted series . . . C, B, A, Mere unlikeness of two days is insufficient to tell us which is antecedent to the other. To determine this we must know something regarding the character of the unlikeness. In a vague way this character is indicated by the term progress, which, as already remarked, is closely associated, in popular conception, with evolution. And the more rigorous scientific disciplines of biology, too, leave us with a not very clearly defined idea of progression as one of the fundamental characteristics of those changes which are embraced by the term evolution. Such phrases as "the passage from lower to higher forms" which are often used to describe the direction of evolution, are vague, and 2 Emerson, Conduct of Life, Everyman's Library Edition, 1915, p. 157. Compare also Lee Wilson Dodd's lines: " . . . . Nor do the stars retrace their glistening snail marks of slow destiny." 3 J. Perrin, Traite" de Chimie Physique, 1903, vol. 1, p. 142. 4 Petronievics, Science Progress, 1919, p. 406. 6 Emerson, Conduct of Life, p. 158. 6 For this reason the characterization of the trend of evolution given by Petronievics, loc. cit., is inadequate. 22 ELEMENTS OP PHYSICAL BIOLOGY undoubtedly contain an anthropomorphic element. 7 At best they give every opportunity for divergence of opinion as to what constitutes a "higher form." If, on the other hand it is stated that evolution proceeds from simpler to more complex forms, or from less specialized to more specialized forms, then the direction of evolution is but poorly defined, for the rule is at best one with many exceptions. It should be particularly noted that all these efforts to specify the direction of evolution attempt to do so in terms of a single component of the evolving system. Such definitions of the direction of evolution are foredoomed to failure. It is the system as a whole that evolves, and we can hope to establish a definition of the direction of evolution only in terms of the system as a whole. Evidently, we must seek a more precise indication of the direction of evolution if our definition is to be truly expedient. We must analyze further the contents of our mind when it contemplates the concept of evolution. We return to our examples of the pendulum, or of the earth in its orbit. When frictional resistances are neglibible, or are disregarded, the periodic series of events in the system may be history, but seems hardly worthy of the name evolution. In actual fact the motion of the pendulum bob gradually dies down, owing to friction and other dissipative forces. The motion is not strictly periodic. The pendulum does not, actually, count out similar seconds, unidentified, but marks, by its greater amplitude, an earlier vibration as distinguished from a later. So also, the earth in its motion is slightly delayed by frictional forces introduced by the tides; it slows down a little as the centuries pass. The strictly periodic process is changed into one in which successive days differ by a trifle in length. The process has a definite direction in time. We feel justified in speaking of the system as "evolving." Now the thing to mark is that what has imparted to the process its directed character is frictional resistance, dissipative forces, typical irreversible effects, to speak in the language of the physicist. 7 "Evolution is thus almost synonymous with progress, though the latter term is usually confined to processes of development in the moral, as distinguished from the physical world. Further, this idea, as Mr. Spencer remarks,has rather a subjective value in existence, as judged by our feelings" (Encycl' Brit., 9th edition, vol. 8, p. 751). Compare also Bertrand Russell Our Knowledge of the Eternal World, 1914, p. 12. "A process which led from amoeba to man appeared to the philosophers to be obviously a progress though whether the amoeba would agree with this opinion is not known." EVOLUTION DEFINED 23 Again, consider a typical example of what we are all agreed to speak of as evolution: the history of the earth and its living inhabitants. The readjustments, the re-adaptations of life-forms which have here taken place, were undoubtedly due in part to changes in external conditions, such as climate, geographic distribution of land and sea, etc. In part, also, such changes have gone on and are going on before our eyes independently of any external changes, and under approximately constant conditions. Organic evolution being a slow process, it takes a certain time, when equilibrium or near-equilibrium is disturbed, for a new equilibrium or near-equilibrium to become established. There is therefore a tendency for internal readjustments or changes to lag behind the external changes by which they are conditioned. As a special case, if an external change is followed by constant external conditions, internal changes may continue to proceed under constant external conditions. Now such internal changes in a material system, which lag behind the determining external changes, or which go on under constant external conditions, are typically irreversible processes.* 8 A. process is said to take place reversibly, if the direction of the change is reversed by a suitable alteration, however small, of the (generalized) force applied to produce the change. For example, if two equal weights are suspended from the ends of a string passed over a simple pulley, then, the weights being initially at rest, any weight however small, added on one side of the system will produce motion downward on that side, provided there is no friction at the pulley and no stiffness in the string. If, on the contrary, a weight, however small, is lifted off from the same side of the system, motion will be initiated in the opposite direction. Note that if there is friction at the pulley, these statements are no longer true. It will now require a weight of definite size, perhaps a decigram, or a milligram, to start or reverse the motion. In the first instance the change is reversible, in the second it is said to be irreversible. Note that in this example the circumstance that imparts to the process an irreversible character is the presence of friction, which causes the dissipation of energy, that is to say, its conversion into heat at the temperature of the surroundings. Again, consider a vessel containing water at a temperature Ti in a room at temperature Tj. If TI is ever so slightly greater than T2, heat passes from the vessel to the surroundings, and vice versa. When, therefore, TI and Ts are very nearly equal, the passage of heat from the vessel to the surroundings is essentially reversible. If there is a material difference between TI and T8 , the heat transference is irreversible. For example, if the vessel is at 50C. and the room at 20C., heat will pass from the vessel to the room. And the direction of this heat transfer will remain unchanged if the temperature of the vessel is 24 ELEMENTS OF PHYSICAL BIOLOGY We are thus led, from two slightly different points of view to the following definition of evolution: Evolution is the history of a system undergoing irreversible changes. Scope of Definition, It is worth while at this point to consider briefly what kind of history this definition excludes and what it includes. It has already been noted that we have excluded certain purely mechanical systems of periodic habit, such as the frictionless pendulum and the planet circling in its orbit through empty space, in absence of tidal effects. 9 It is not the case, however, that all purely mechanical systems are excluded, that is to say, all systems in which all energy is either kinetic or potential (configurational), all forces either inertia forces or positional forces. If our knowledge of such a system is statistical in character, if we know only averages of certain of the variables defining the state of the system, it may happen that certain changes therein appear to us irreversible, and would accordingly be classed, by our definition, among processes of evolution.10 This leads to the seemingly embarrassing conclusion that a process is or is not a process of evolution, according to the reduced 1, 2 or even 10. Not until the vessel is cooled by more than 30 will the stream of heat be reversed. The passage of heat in such case, from a body at one temperature to another at essentially lower temperature, is irreversible in this sense, the sense in which the term is employed by the physicist in discussions of this kind. In the case in which internal readjustments lag behind changes in external conditions, there is necessarily a finite difference between the applied (generalized) force, and the opposing resistance. Such processes are, therefore, of necessity, irreversible. From the examples given, it will be seen that during a reversible change a system is at all times (very nearly) in equilibrium. It can therefore be said that a reversible change is one in which the system passes through a continuous succession of equilibria. In fact, the change is strictly reversible only if the difference in the applied (generalized) force and the resistance is infinitesimal, and the change is infinitely slow. 6 Such tidal effects act as brakes and destroy the exact periodicity of the motion. 1S The irreversibility also of those changes occurring in a system whose internal adjustments lag behind changes in the applied forces, may be apparent, and may disappear when detailed knowledge of the individual parts of the system takes the place of statistical data. The reason for this is that when the reaction or readjustment is expressed in a statistical way, an average of individual reactions may show a lag, although each individual reaction itself maybe immediate. EVOLUTION DEFINED 25 nature and extent of our knowledge regarding the system. So, for example, the establishment of thermal equilibrium in a body of gas initially at non-uniform temperature is evolution if we merely know its total mass, composition, volume, pressure and initial temperature distribution. But should we be informed of the exact initial state of each molecule, then the process by which thermal equilibrium is established (if this does occur) would be classed, together with the journey of the earth in its orbit, among the cases excluded, as mere history, from our definition. This, upon reflection is neither as strange, nor as embarrassing as it may at first sight appear. For problems of evolution are in large measure problems of probabilities, statistical problems. Incidentally, this reflection disposes of the rather foolish objection sometimes raised against the theory of evolution, that it ascribes the course of events in an evolving system to chance. When we describe a phenomenon as being governed by chance, we do not, of course, mean that there are no definite causes (determining factors) at work; we merely state in these terms that the causes are complex and not known to us in detail. Practically there is no cause for embarrassment, since we never do know material systems in sufficient detail to compute their state at every instant from the initial state, except in terms of averages. In principle, however, it is necessary to make the admission that, in the last analysis, whether we class the history of a system as evolution or not must depend on the extent and detail of our knowledge of that system. 11 It will thus be seen that the line of division between reversible (purely mechanical) and irreversible (dissipative) processes is not 11 To be quite exact, evolution, according to this, should be defined in terms of a point of view, say about as follows : Evolution is the history of a system, regarded as a progressive change or development, to which its unidirectional character is imparted by irreversible changes going on in the system. That a point of view is involved is also implied in the following definition given by Karl Pearson: "A causal description of the appearance of successive stages in the history of a system forms a theory of the evolution of that system. "If the theory be so satisfactory that it resumes in some simple statement the whole range of organic change, we term it the law of evolution," (Grammar of Science, 1900, p. 375). 26 ELEMENTS OF PHYSICAL BIOLOGY so very sharply drawn. Furthermore, the cases excluded are, in point of fact, ideal cases. Real processes are always irreversible. Hence, after all, history, real history, is always evolution, and, though f . in principle the two concepts may be distinct, in practice they "-(' coincide in scope. What then is gained by our definition of evolution? This is the gain: Having analyzed the submerged implications of the term evolution as commonly used, so as to bring them into the focus of our consciousness, and having recognized that evolution, so understood, is the history of a system in the course of irreversible transformation; we at once recognize also that the law of evolution is the law of irreversible transformations; that the direction of evolution (which, we saw, had baffled description or definition in ordinary biological terms), is the direction of irreversible transformations. ' . And this direction the physicist can define or describe in exact terms. Jl For an isolated system, it is the direction of increasing entropy. 12 The law of evolution is, hi this sense, the second law of thermo- dynamics. 13 12 More generally, it is the direction of decreasing thermodynamic potential, this potential being variously defined, according to the conditions of transformation. 13 "The second law (of thermodynamics) is the law of evolution of the world accessible to our observation" (Chwolson, Lehrbuch der Physik, 1905, vol. iii, p. 499; Scientia, 1910, vol. iii, p. 51. the second law of the theory of energy is now generally regarded as essentially a statistical law. So viewed, the second law of energy becomes a principle stated wholly in terms of the theory of probability. It is the law that the physical world tends, in each of its parts, to pass from certain - -v less probable to certain more probable configurations of its moving particles. As thus stated the second principle .... becomes a law of evolution" (Josiah Royee, Science, 1914, vol. xxxix, p. 551.) "Tin systeme isole ne passe jamais deux fois par le me'me e"tat. "Le second principe affirme un ordre nece"ssaire dans la succession de deux phenomenes, sans retour possible aux etats deja traverse's. C'est pourquoi j'ai cru expressif d' appeler ce principe un principe devolution. II se trouve qu'en proposant ce nom je suis fidele a la pens^e de Clausius, car le mot farpomft, d'oti ii a tire" entropie, signifie precisement Evolution." (J.Perrin, Trait6 de Chimie Physique, 1903, vol. 1, pp. 142-143.) "II est hautement improbable qu'un systeme isole" passe deux fois par le mgme e"tat; cela est d'autant plus improbable que la complication du systeme est plus grande, et pratiquement il serait insensS de se placer dans cette hypothec d'un retour a I'Stat initial." (J. Perrin, loc. cit., p. 146) . A EVOLUTION DEFINED 27 Simple Mechanical Example. It will be desirable, at this point, to consider, by the aid of a simple example, the manner in which some of the facts considered in the preceding pages find expression in the analytical formulation of the behavior of mechanical systems. Take the example of the simple pendulum. For small vibrations the restoring force, tending to draw back the bob to its lowest position, 3/ is easily shown to be mg -, where x is the horizontal displacement, 6 m the mass of the bob, and g the acceleration of gravity. This force is expended upon two items, first, in overcoming the inertia of the bob, and producing an acceleration a. The force so expended is cc measured by ma. Second, a part of the force mg - is expended in b overcoming the resistance of the air. If v is the velocity of the bob, this part of the force is measured (for ordinary velocities) by kv, where k is a constant depending on the shape of the bob, etc. We have then ma + kv = mg (1) /Jj* or, since the velocity v is the rate of change of x with time, i.e., =-> GlV fiir nD (i y and a is the rate of change of with time, i.e. a = = , at at ctt d?x dx x . . Now there are certain general characteristics to be observed in this equation, characteristics which are typical of the equations of motion of mechanical systems. The equation contains the first and second derivatives of x with regard to t and no higher derivatives, The first derivative is introduced by the frictional force, and disappears if this force is zero, Le., if the coefficient k in (2) is zero. The equation then takes the simpler form Now in this simplified form the equation has the following peculiarity: It is indifferent to the sign of t. For, in differentiating twice in succession with regard to t, the positive sign of the second deriva- 28 ELEMENTS OP PHYSICAL BIOLOGY tive is restored. This is the analytical symptom, as it were, of the reversibility of the process. 14 It should be noted that this peculiarity disappears at once if the frictional term k ~ is present, for a single differentiation with regard to-* yields a result with sign opposite to that of differentiation with regard to t. The presence of a frictional force, therefore, imparts to the process an irreversible character, it establishes a distinction between t and-i; it singles out one direction in time as a peculiar direction, the forward direction, the direction of progression. Now, in point of fact, in the equations of motion of all real systems j the frictional term (viscosity term) k j or its equivalent is present, d?x though it may be small as compared with the inertia term *-^, The reversible system, in which this term is wholly absent (zero) is an ideal case, it represents a limit towards which real systems may approach; an abstraction. Inertia-Free or Completely Damped Systems. There is another such ideal limiting case, another abstraction, which is of much interest because certain important classes of real systems approach it very closely. This is the case in which the inertia term m is negligible, so that in the case of the pendulum, difor example, the equation representing the history of the system reduces to , dx x /, N k = -mg r (4) at I The history of such inertia-free systems is typically of the irreversible kind. They have, furthermore, a property illustrated by certain features in the equation (4) above : dx It will be observed that if cc is zero, then --=- also is zero, or, as we may put it, the velocity vanishes with the displacement from equilibrium. Moreover, differentiation of (4) gives di* I dt u Compare H. PoincarS, Thermodynamique, 1908, p. 441. EVOLUTION DEFINED 29 from which it is seen that the acceleration also vanishes with the velocity. 15 This implies that when the system is in its equilibrium position, it is also actually at r$si, unlike the pendulum, which swings twice through its equilibrium position in each vibration. The former property, the vanishing of the accelerations with the velocities, so that the equilibrium position is necessarily the position of rest, is characteristic of an important class of systems, including those with which we shall here be chiefly concerned. Another important characteristic of such systems, which is also exemplified by equation (4), is that the velocity is uniquely determined for every value of x. This is not the case in the motion represented by (3). This latter equation gives, upon integration, --.C-* (6) dx so that for every value of x there are two possible values of . (M> W.e have, then, at the one extreme the "purely mechanical" system free from frictional (Viscosity) effects, and, in its most typical form, periodic in habit. As an intermediate link we have systems exhibiting both inertia and frictional effects. Their action may resemble that of a pendulum swinging in air; typically the history of such a system exhibits the phenomenon of damped oscillations, a periodicity over which there is superimposed the dying away of the motion. The damping is introduced by the frictional effects. At the other extreme we have inertia-free, or, as we might say, completely damped systems/ 6 typically irreversible in their history. The system and processes with which we shall largely be concerned here seem to belong essentially to this third type, as will be seen in the development of the theme. Compare E. Buckingham, Theory of Thermodynamics, 1900, p. 33. 16 This does not, however, preclude the possibility of oscillations. More will be said on this point later. IISC Lib B'lore 574 N25 2544 CHAPTER III THE STATISTICAL MEANING OF IRREVERSIBILITY Supposons que nous voulions placer un grain d'avoine au milieu d'un tas de hie": cella sera facile; supposons que nous voulions ensuite 1'y retrouver et 1'en retirer; nous ne pourrons pas y parvenir. Tous les phe*nom6nes irr6versibles, d'apres certains physiciens, seraient construits sur ce modele. JET. Poincari. One point, to which, allusion has been made incidentally, calls for comment. Many processes which, viewed in the gross, present the appearance of typically dissipative, irreversible phenomena, have long been suspected, and have in recent years been fully demonstrated to be, in fact, of the reversible type, "purely mechanical" processes, the details of which are merely hidden from our view owing to the diminutive dimensions (and correspondingly immense number) of the units at play. So, for example, consider the case of two vessels A and B at equal pressures, communicating by a tube that can be closed by means of a turncock. Let the vessel A contain 1 gram of nitrogen gas, and let B contain 1 gram of oxygen gas, the communication between A and B being closed. It is a matter of common knowledge that if the stopcock is now opened, the gas from the A will flow over into the vessel B and vice versa, and in a short time an equilibrium is reached in which each vessel contains 0.5 gram of each gas. Now, in point of fact, the molecules of the gas behave (approximately) like a number of elastic spheres, their equations of motion contain no dissipative term, but are of the type (3) (Chapter II). We should therefore expect the system to exhibit periodic motion, we should expect that after a certain lapse of time the initial condition should return, and that all the nitrogen should once more be contained in the vesel A, all the oxygen in B. In actuality, such a thing is never observed. How is this discrepancy to be explained? Let us replace the two vessels and the gas molecules by some simple analogues of dimensions readily accessible to our senses, and let us., watch a process analogous to the diffusion of the gas from one vessel into the other. We provide ourselves with two boxes 30 STATISTICAL MEANING OF IRREVERSIBILITY 31 or urns.1 In one of these, A we place 50 black balls; in the other B, we place 50 white balls. We shuffle both boxes thoroughly, and then draw blindly a ball from A, and one from B, and we return them to opposite urns. We continue this as long as desired. The more lightly drawn curve in figure 1 shows the graphic record of an actual series of drafts of this kind. The stair-case-like line shows how in successive drafts the number of black balls in box A gradually diminished until at last there remained about 25, onehalf of the original number, in box A. But note that there are fluctuations, sometimes the box contains 26, 27, 28, then again 3O 4O NUMBEff Cl 9060 (DOUBLE.) Fia. 1. GRAPH OF MODEL PROCESS ILLUSTRATING THE STATISTICAL MEANING OF IRREVERSTBILITY The more lightly drawn curve records the number of black tickets remaining in urn A after successive drafts. The heavier curve records the previous and ensuing history of 50 tickets found in urn A at the end of the fiftieth draft, (Reproduced from A. J. Lotka, Two Models in Statistical Mechanics, Am. Math. Monthly, vol. 31, 1924, p. 122.) 27, 26, etc. of the original balls. It is nowise impossible that, if we continue the drafts for a long time, some time or other all the original 50 black balls will be back in box A; but it is highly improbable that this should happen within any reasonable time. Curiously enough, the urn model is competent to illustrate also this highly improbable course of events. For this purpose, instead of starting with 50 black and 50 white balls, we start with the balls, or in this case more conveniently tickets, all white, and numbered from 1 to 50 in urn A, and from 51 to 100 in urn B. After a suit- 1 A. J. Lotka, Am. Math. Monthly, March, 1924; Science, 1924, vol. 59, p. 532. 32 ELEMENTS OP PHYSICAL BIOLOGY able number of drafts, say 50 double drafts, in which a record is kept of all the numbers drawn, the urns are opened, and the tickets in the second urn are now blackened. The drawing is then continued, for, say, another 50 drafts, recording each time the numbers drawn. The numbers on the tickets enable us to trace the previous history of the 50 black tickets, before they were blackened. In an experiment actually carried out it was found that these 50 black tickets were originally distributed essentially evenly in the two urns. The curve representing the first 50 drafts is an ascending curve, the system passed, during this stage of the process, from more probable to less probable states, as shown in the first, ascending portion of the more heavily drawn curve in figure 1. In the second series of fifty drafts the curve descends in normal fashion, with increasing probability of the successive states of the system. It may seem like a contradiction of terms that what amounts practically to an infinitely improbable series of drafts should be capable of actual realization at will. But if the series of drafts described were extended to great length in both directions, say one million drafts before blackening the tickets, and one million after, it would be seen that the peak on the curve is indeed a very exceptional feature. It is a perfectly safe bet that in two million drafts not more than one such peak, going up to 50 black balls in one urn, would be encountered. The model described exemplifies among others the fact that in an exceedingly long lapse of time it may some time occur that the system will return to its original state. This is quite in accord with the laws of mechanics; in fact, as already noted, these laws actually demand that every mechanical system of finite dimensions must,, ultimately return to its initial state, and must do this not onee only, but in everlasting reiteration at regular intervals: the motion is periodic. This property also is capable of illustration by a simple model, such as the following: Twenty-six pendulums of periods T = 0.5, 0.6, . . . 2.9, 3.0 seconds are started simultaneously to the left from their equilibrium position, and are then allowed to oscillate undisturbed. Count is then made, at the end of every tenth of a second, of the number of pendulums on the left of ^ the median. In this way the staircase curve figure 2 was obtained (computation here taking the place of actual observation). It will be seen that in the brief fragment of a period covered by the STATISTICAL MEANING OF IKREVEBSIBILITY 33 record, this exhibits all the characteristics of a "passage from a less probable to a more probable distribution," though, in point of fact, we know that the system has a perfectly definite period of 7385 years. The appearance of chance in this wholly determinate mechanical process is brought into still greater prominence if we plot the deviations, from the mean, of the number of pendulums on the left of the median position, at successive counts. We thus obtain the points indicated by small circles in figure 3. These group themselves very obviously about a typical Gaussian curve of random distribution, namely one having a standard deviation of y2L', this curve has been drawn in the diagram, and, as will be seen, the agreement is good, considering the smallness of the sample FIG. 2. GBAPH OF SECOND MODEL PEOCESS ILLUSTRATING THE STATISTICAL MEANING OF IEEEVEESIBILITY Number of pendulums found on left of median position at successive epochs. (Reproduced from A. J. Lotka, Two Models in Statistical Mechanics, Am. Math. Monthly, vol. 31, 1924, p. 124.) (412 observations, extending over 41.2 seconds, out of a total period of 7385 years). Thus for long stretches of time the periodicity of the motion of the system of pendulums is very effectively masked under an aspect of "chance." These simple models illustrate very clearly how the seeming conflict between the periodicity of all mechanical motions and the apparently one-sided course of events, directed toward one definite end state, is resolved. The actual process of isothermal gaseous diffusion is, in fact, periodic, but with a period so long that humanly speaking, the return to the initial state never occurs at all. For all stretches of time that can have any real significance in human thought (and this includes the vast historical ranges of all geology and astronomy), it may therefore be said in a certain sense that evo- 34 ELEMENTS OF PHYSICAL BIOLOGY lution proceeds, in all but a vanisMngly small class of- exceptional cases, from less probable states (e.g., uneven distribution of the 50 black balls in the two urns) to more probable states, tending ultimately toward a most probable state. This statement cannot however be allowed to pass without a word of caution. It is mean- -/ft 83 FIG. 3. FREQUENCY DIAGRAM FOE THE DEVIATIONS FROM THE MEAN APPEARING IN FIGURE 2 Abscissae represent deviations from the mean (13) in number of pendulums on left of median; ordinates represent corresponding frequencies, among the observations recorded in figure 2. (Reproduced from A. J. Lotka, Two Models in Statistical Mechanics, Am. Math. Monthly, vol. 31, 1924 t> 125.) '*' STATISTICAL MEANING OF IEREVEESIBILITY 35 ingless unless the characteristic with regard to which probability is reckoned is explicitly or implicitly indicated. Probability is essentially a matter of classification. An improbable event is one that is a member of a small class, and whether it is so or not depends, clearly, on our system of classification. For this reason the broad statement which has sometimes been made, 2 that the direction of evolution is from less probable to more probable states, is not only inadequate, but is really meaningless. It is indefinite In failing to specify with regard to what characteristic probability is to be reckoned; and it is incomplete in failing to call attention to the fundamentally important connection between the particular probabilities in question and available energy. Another point, which has not hitherto perhaps received its deserved attention is clearly brought out by the two models described, namely, that irreversibility is a relative term. For, obviously, if we use our visual discrimination in selecting the balls drawn from the boxes (instead of drawing blindly), we can easily bring it about that in short order all the black balls are back in box A. Thus a process may be reversible or not, according to the means that are naturally available or arbitrarily permitted in operating upon the system under consideration; somewhat as the trisection of an angle is or is not an impossible geometric construction, according as we are or are not forbidden the use of instruments other than ruler and compass. In the case of molecular aggregates this fact has long been duly appreciated, having been first pointed out by Clerk Maxwell, who remarked that a demon capable of dealing with individual molecules would be able to cheat the second law of thermodynamics. But it seems to have been pretty generally overlooked that the relative character of irreversibility has an important significance in certain natural processes taking place on a macroscopic scale. In point of fact this is a matter whose importance in the world of living organisms can hardly be rated too high. For there are certain diffusive processes going on in nature which, from the standpoint of thermodynamics, are not of the irreversible type; but which might as well be, so far as any benefit derived from their reversibility by the organism (and, in particular, by man) is concerned. If I should be the fortunate 2 See for example, J. Royce, Science, 1914, vol. 34, p. 551. 36 ELEMENTS OF PHYSICAL BIOLOGY possessor of a pound of gold dust, and some malicious person should take it and scatter it far and wide, so that it became hopelessly diluted with dust and refuse, it would be a small comfort to me to know that it were merely mechanically commingled with such foreign matters, that it had not irreversibly undergone solution or chemical transformation, and that therefore it could theoretically be recovered without the expenditure of work. In practice its recovery might entail the expenditure of far more energy than if the gold were present in reasonably concentrated solution. The point is that in practice I am restricted to operations in bulk upon reasonably large quantities, in reasonably concentrated form, otherwise the theoretical ideal of recovery without work is very far from being attained. And with this restriction placed upon my operations, certain processes acquire an irreversibility which they do not possess apart from that restriction. The illustration of the pound of gold has the advantage of simplicity and cogency. But if by any chance it has conveyed the impression that only in peculiar and far-fetched cases does this kind of irreversibility enter into play, then it is an unfortunate example indeed, for nothing could be farther from the truth. The fact is that nature abounds in just such dissipative processes as the scattering to the four winds, to utter inutility, of materials of the highest importance to life; and one of the central problems which the organism has to solve in the struggle for existence, is the reconcentration, into his immediate environment and into his body, of valuable materials that have become scattered by agencies beyond his control. It is not the least of the triumphs which have made man the lord of creation, that he has learnt, beyond all comparison more effectively than any of his competitors, to carry out this process of reconcentration to satisfy his needs. So a fleet of ships, year by year, bear a burden of saltpeter from Chile to all civilized countries, to balance the losses from our depleted fields. So, in his most recent technical achievement, man has learnt to draw from the air a supply that will continue unfailing, long after the Chilean nitre beds are exhausted. The fact is, in dealing with the physics of such macroscopically irreversible effects, it will ultimately be necessary to develop a method of mathematical analysis that shall be competent to distinguish and handle not only the extremes the case of a primitive organism that can deal only in the gross, without intelligent or STATISTICAL MEANING OF IKREVEBSIBILITY 37 other discrimination, with, the matter and situations presented to it; and an ideally perfect organism, that should expend just the minimum of effort, directed with absolute precision toward the attainment of its ends. A method must be devised that shall duly take account of, and use as a fundamental datum for its deductions, the particular character, the particular degree of perfection of the mechanical and psychic equipment or organization by which each organism reacts more or less selectively upon its environment. We shall have occasion to refer to this matter again in greater detail in a~ later section. But here it is well to note that our two models are suggestive also with regard to this aspect of the subject. For it appears at first sight as if there were a fundamental difference in character between the first and the second model, since it is essential for the operation of the urn model that the drawing be done blindly, so as to give chance a part in the process, as we would say; whereas the pendulum model we operate with our eyes open, apparently in full consciousness of what is going on. Chance seems to play no part here, the system is mechanically determinate. But there is a blindness which is not of the eye, and there is a vision that surpasses optical vision. The same struggle for existence which has developed in man the organ of sight, to depict for him the external world, to furnish him with a map on which to base his plan of campaign, has also, in latter days, developed his internal vision, whereby he extends his world-picture beyond the powers of the bodily eye. It is immaterial by which process his map is drawn 'its function is the same; whether I peep into the urn and manipulate the drafts by the light of my eyes; or whether, in the light of my knowledge of mechanics, I adjust the pendulums to equal lengths and phases; or again, whether, in the more serious affairs of life I employ these same faculties to diverse ends, the effect is the same: In greater measure or less these organs and faculties emancipate me from the bonds of the fortuitous and make me a controller of events. Their function is to substitute choice for chance, to introduce aimed collisions in place of random encounters. Origin of Subjective Sense of Direction-in-Time. The failure of the differential equations of dynamics to discriminate between t and t raises the question as to the physical significance and origin of our subjective conviction of a fundamental difference between the forward and the backward direction in time, a con- 38 ELEMENTS OP PHYSICAL BIOLOGY viction that is intimately bound up with the concept of evolution, for, whatever may ultimately be found to be the law of evolution, it is plain that no trend of any kind can be denned or even described without reference to a favored direction in time. One view which suggests itself is that this conviction is our subjective appreciation of the trend from less probable to more probable states recognized in statistical mechanics. But this does not seem very satisfying, for we somehow feel that our conviction must rest on something more fundamental than this somewhat accidental circumstance, which, as the models described clearly show, is fundamentally incompetent to distinguish between the forward and the backward direction in time. For the pr ^in figure 1, for example, may indifferently be traversed from lefTto right or vice versa, it presents the same general character in either sense. Another alternative is to suppose that the differential equations of dynamics, as formulated by us today, are either an incorrect, or else an incomplete statement of facts. The latter view is, indeed, upon reflection, found to have a certain warrant. For the differential equations of motion alone do not fully determine the actual course of events; this depends further on the value of certain arbitrary constants of integration; or, to speak in terms of physical entities, upon the initial velocities of the particle of which the system is composed. Strictly speaking it is only when the initial velocities are zero, that the equations of motion, considered in their totality, are indifferent to the substitution t' = t. From this point of view our sense of the forward direction in time would appear as our subjective appreciation of the fact that, once a material system has been started on a certain course, with certain initial velocities, there then remains no further freedom; its history must continue to unfold in the direction determined by the initial veloc- ities. It seems, however, that it is not with this perfectly general type of irreversibility of the course of events that we are chiefly concerned in the study of evolution. The concept of evolution, according to the analysis which has been made of it in preceding pages, applies principally, if not exclusively, to systems that outwardly at least affect the aperiodic habit, systems that do not return periodically to their initial state, but show a definite trend, whereby yesterday and tomorrow are never alike, and differ more- STATISTICAL MEANING OF IEEEVEESIBILITY 39 over in some definite and characteristic fashion, even though we may not be fully competent, at the present epoch of science, to specify exactly wherein lies the characteristic difference.3 Inadequacy of Thermodynamic Method. Our reflections so far have linked the fundamental problem of the direction, the trend of evolution, with the disciplines of thermodynamics and statistical mechanics. From this point of view the direction of evolution is identified with the direction of the unfolding of irreversible processes, the direction of increase of entropy (in thermodynamics) or of increasing probability (in statistical mechanics). A certain mental satisfaction may be derived from, this conclusion. It gives us, in principle at least, an answer to our question "Quo vadis?" But practically the answer is very inadequate. If the conclusions, the methods of thermodynamics, or of statistical mechanics, are to be applied to a concrete case, the data of the problem must be presented in a veiy particular form. So long as we deal with volumes, pressures, temperatures, etc., our thermodynamics serve us well. But the variables in terms of which we find it convenient to define the state of biological (life-bearing) systems are other than these. We may have little doubt that the principles of thermodynamics or of statistical mechanics do actually control the processes occurring in systems in the course of organic evolution. But if we seek to make concrete application we find that the systems under consideration are far too complicated to yield fruitfully to thermodynamic reasoning; and such phases of statistical mechanics as relate to aggregation of atoms or molecules, seem no better adapted for the task. To attempt application of these methods to the prime problems of organic evolution is much like attempting to study the habits of an elephant by means of a microscope. It is not that the substance of the elephant is inherently unfitted to be viewed with the microscope; the instrument is ill adapted to the scale of the object and the investigation. It would seem, then, that what is needed is an altogether new instrument; one that shall envisage the units of a biological population as the established statistical mechanics envisage molecules, atoms and electrons; that shall deal with such average effects as 3 Perhaps the objective interpretation of our subjective sense of direction in time must be sought in quantum mechanics. Cf. A. J. Lotka, loc. cit., p, 126, and, W. S. Franklin, Science, 1924, vol. 60, p. 258. 40 ELEMENTS OF PHYSICAL BIOLOGY population density, population pressure, and the like, after the manner in which thermodynamics deal with the average effects of gas concentration, gas pressures, etc.; that shall accept its problems in terms of common biological data, as thermodynamics accepts problems stated in terms of physical data; and that shall give the answer to the problem in the terms in which it was presented. What is needed, in brief, is something of the nature of what has been termed "Allgemeine Zustandslehre," 4 a general method or Theory of State. It is somewhat along these lines that the system now to be sketched is conceived. A term introduced by J. R. Rydberg, quoted by C. Benedicks, Zeitschr. f. phys. Chemie, 1922, vol. 100, p. 42. CHAPTER IV EVOLUTION CONCEIVED AS A REDISTRIBUTION Toutes ces choses ne peuvent se determiner surement que par des mesures precises que nous chercherons plus tard; mais auparavant il fallait au moins sentir ie besoin de les chercher. /. B. Biot. It now behooves us to establish, with respect to the problem of evolution, a viewpoint, a perspective, a method of approach, which has hitherto received its_ principal development and application outside the boundaries of biological science. Such prior development and applications, however extraneous to our chief line of interest here, may well serve us in our present interrogations, since we shall be in a position to profit by the precedents established in methods, in conclusions, and, most particularly, in habit of thought. This perspective is that which contemplates an evolving system as an aggregation of numbered or measured components of several specified kinds, and which observes and enregisters the history of that system as a record of progressive changes taking place in the distribution, among those components, of the material of which the system is built up. It is thus that physical chemistry views the progressive changes in a system comprising several chemical species, that is to say elements, compounds, phases, etc. It describes the system by enumerating these components, by stating their character and extent (mass); and by further indicating the values of certain quantities or parameters, such as volume or pressure, temperature, etc., which, together with the masses of the components, are found experimentally to be both necessary and sufficient, for the purposes in view, to define the state of the system. With the instantaneous state of the system thus defined, physical chemistry investigates by observation and by deductive reasoning (theory) the history, the evolution of the system, and gives analytical expression to that history, by establishing relations, or equations, between the variables denning these states (after the manner set forth above), and the time. It is commonly found that these fundamental equations assume the simplest, the most perspicuous form, when they are written 41 42 ELEMENTS OF PHYSICAL BIOLOGY relative to rates of change of the state of the system, rather than relative to this state itself. That is to say, it is found that the expressions for the rate of increase in mass, the velocity of growth, of the several components, are simpler, more primitive in form, than the expressions giving directly the mass of each component as a function of the time. In the language of the calculus, the differential equations display a certain simplicity in form, and are therefore, in the handling of the theory at least, taken as the starting point, from which the equations relating to the progressive states themselves, as functions of the time, are then derived by integration. 1 So, for example, a simple system may be defined as comprising 4 grarn-rnoleeules of hydrogen, 2 gram-molecules of oxygen, and 100 gram-molecules of steam, at one atmosphere pressure, and at 1800C. The fundamental relation expressing the law of evolution, the historical pattern, of the system, is in this case given by the law of mass action: . /{^ (_-! } v dt v 3 v2 where v is the volume, mi is the mass of steam, m2 the mass of hydrogen, and ms, the mass of oxygen (all expressed in gram-molecules). The coefficients h, h, are functions of the temperature, or, for a given temperature, are characteristic constants of the re- action. We are not, here, interested in the particular form of the law of mass action. What does interest us is the general form of the equation (1). It states that the rate of increase in mass, the velocity of growth of one component, steam (mass mi), is a function of the masses m*, nis, of the other components, as well as of the mass mi itself, and, besides, of the parameters v (volume) and T (temperature), the latter being contained in the coefficients fc x , /c2 . This statement, in its more general form, is written, according to established notation2 1 In experimental observation usually (though not always) the reverse attitude is adopted. 2 For the benefit of the non-mathematical reader it may here be explained that aquation (2) is merely a short-hand expression, so to speak, of the simple statement: The rate of increase of mass with time of the component Si is dt & junction of, or is determined by, the masses mi, m2 , ma, of the components Si, S%, Ss, as well as by the volume v and the temperature T. Precisely similar ia the construction to be placed on the equations (3). EVOLUTION CONCEIVED AS REDISTRIBUTION 43 dni-i = F (nn, mz, ms ; v, T) (2) at Now it is this habit of thought, expressed in equation (2) , that is to be transplanted into the contemplation of problems of evolution in general, and organic evolution in particular; this point of view, this perspective, which regards evolution as a process of redistribution of matter among the several components of a system, under specified conditions.3 Having thus passed from the specific to the general from the case of physico-chemical systems to a general formulation -we now retrace our steps to the particular, but in a new direction. We now contemplate the kind of systems that form the object of study of the biological sciences. With the outlook gained in our preceding reflections we envisage the life-bearing system, in the progress of evolution, as an assembly of a number of components: Biological species; collections or aggregations of certain inorganic materials such as water, oxygen, carbon dioxide, nitrogen, free and in various combinations, phosphorus, sulphur, etc. These components are placed in various relations of mutual interaction under specific conditions of area, topography, climate, etc. Under these conditions each may grow, decay, or maintain equilibrium. In general the rate of growth ~7T~of any one of these components will depend upon, will be a function of, the abundance in which it and each of the others is presented; this rate of growth will also be a function of the topography, 4 climate, etc. If these latter features are defined in terms of a set of parameters Pi P2 . . . PJ, we may write, in the same sense as equation (2) 3 Compare F. B. Jevons, "Evolution," Macmillan, 1902, Chapter VI, p. 72. 4 Terrestial species have an essentially two-dimensional distribution, so that area functions here in a manner somewhat analogous to that in which volume enters into physico-chemical relations. Aquatic life, with its threedimensional sphere of activity, is enacted in systems whose extension is described in terms of volume. More detailed topographic parameters may be required to define in sufficient completeness the configuration, the structure of these systems. The absence of such detail from the more familiar formulations of chemical dynamics is due to the purely accidental circumstance that the systems commonly dealt with in that branch of science are either homogeneous, or of comparatively simple heterogeneous structure. 44 ELEMENTS OF PHYSICAL BIOLOGY ~ = Fx (Z 1; Z,, . . . XnJ Pi, Pt, . . . Pi) CW j~v = Ft (Xi, Xz, . . . Xn', Pi, Pa, PI) (3) at j-y= Fn (Xi, X^ . . . XR ; PI, Pj, . . . Pj) at In general there will be n such equations, one for each of the n components. The purport of these equations (3) remains uncertain so long as the components (e.g., biological species, etc.) Si Sz . . $n are undefined. What definitions we may adopt for these is, in accordance with the principles discussed anteriorly, a matter for arbitrary disposition; though we may be guided in our choice by considerations of expediency. These may advise different policies from case to case, according to the particular phase of the problem taken in view. The conclusions reached will, of course, depend upon the particular definitions chosen. This is as it should be; the conclusions apply to the components as defined, and, in general, to no other. This seems clear enough, but if any further exposition is needed, it will be found In examples shortly to be considered. Intra-Group Evolution. While the precise definition of the components Si S2 . . , SB may, and indeed must, be held over for determination as each separate phase of the general problem is singled out for treatment, yet there is one class of cases regarding which it is appropriate to set forth certain reflections at this juncture. It may have been observed that so far nothing has been said regarding one aspect of or/ganic evolution which, in the history of the subject in the past, and hi the minds and writings of its exponents and students today, occupies a dominating position namely, the relation of evolution to the modification of species with the passage of time, and, in particular, to the origin of new species. Now a biological species, however defined, is not a homogenous group. It comprises portions (individuals) varying more or less widely with regard to numerous features, such as stature, weight, etc. If our description of the distribution of matter in the system is to be at all exhaustive, we shall need to know, not only the extent EVOLUTION CONCEIVED AS EEDISTEIBUTION 45 (total mass) of each species, but also its constitution, as expressed by the frequency, the relative abundance, of each statistical type within the species. In the case of man, for example, we may wish to know the fraction F (56) of the total population whose height is comprised within the limits 58 and 57 inches at a given instant. And in observing the evolution of the system of which this population forms part, we shall be interested, not only in the growth (or decay) of the population as a whole, but also in the rate of change of the abundance (frequency) of each statistical type. This phase of the problem does not differ essentially, in character, firom that first considered : it is essentially a question of distribution and changes in distribution of mass in the system among its several cornponent; only now we have fixed our attention on a different set of components, components defined in a different way, on a finer scale. In the first instance we had taken in view the distribution and changes in distribution of the matter of the system among the several major groups or species; now we are considering the distribution within each such group. This division of the general problem of organic evolution into two aspects has certain practical advantages, and it will be convenient to have names to designate the two separate aspects or domains of evolution. We shall accordingly speak of inter-group evolution on the one hand, when referring to changes in the distribution of the matter of the system among several component groups; and we shall speak of intra-group evolution when referring to changes in the distribution of matter within the group, among its statistical types, however defined. It is possible to set up equations relating to intra-group evolution, similar in general character to those set forth above relative to inter-group evolution. However, this phase of the problem is probably treated more satisfactorily in other ways, of which some examples will arise in due course.5 It is nevertheless, desirable, to indicate in the system, of equations (3) the incidence of intra-group evolution. Conveniently this may be done by writing the ith equation, for example, in more detailed form: = Fi (X1} Z,, . . . Xn ; Pi, PSj . . . PI; Qi, Q, . . . Qk) (4) at 5 See Chapter IX, p. 122; Chapter XIII, p. 170; Chapter XXV, pp. 348 et seq. 46 ELEMENTS OF PHYSICAL BIOLOGY where Qi, Q2) , . . Qk are parameters defining the character of several components (e.g., biological species) S; such definition may take the form of a set of characteristic frequency functions, or some other form. These parameters will, in general, be functions of the time, that is to say, each component may, in general, be variable in character through the occurrence of intra-group evolution. Whether this variability is limited, or constrained to follow a certain course (orthogenesis), whether variations take place in continuously graded series or per saltum, or in any or all of these ways, are questions which will not be discussed at this point. At present all that need be said is that the origination of a new species in any of these ways falls within the scheme of our description of evolution as a change in the distribution of matter among the components of the system. 6 It may be remarked, in passing, that in general a complete definition of the system may require an infinite number of parameters P and Q; this does not necessarily cause any undue complication in practise, since in many cases certain of the parameters P, Q either remain constant, or change so slowly that, in discussing changes in the variables X, we may treat these parameters as if they were constant. The parameters Q, defining the character of the species, are in general functions of the time, as has already been remarked. In this respect organic evolution exhibits a very important distinction as compared with chemical evolution, i.e., the evolution of a system in the course of chemical transformation. In such a system the character of the components is usually fixed once for all. Water is H2 for all time, unlike a species of organism which is subject to change in character. One important result of this is that, so far as we know, organic evolution is a process without end, for there seems to be no limit to the variety of forms of living matter, as there is no limit to the variety of geometric configurations and mechanical systems that can be formed from a given portion of matter. Chemical evolution, on the contrary, terminates, under constant condition, in a definite equilibrium, determined once for all, by those conditions. 8 This is not a new definition of evolution, it is a conception of evolution wholly compatible with the definition that has been laid down in preceding pages. EVOLUTION CONCEIVED AS BEJHSTRIBTJTION 47 It will be observed that the fundamental equations (3) resemble in form the equation (4) of Chapter II, which was given as a typical example of the equation for an inertia-free or completely JV damped system. The velocities -37 are single-valued functions F of the variables X. It is the single-valued character of the functions F that gives the system its stamp as an inertia-free or completely damped system; a system in the course of typically irreversible transformation. It is not maintained that these equations cover all cases that may be brought within the purview of the present study; nor shall we, in all cases, be tied down to the scope of these equations. They are, however, of very broad scope, and, upon reflection, will be found to cover at least a large and significant portion of the field of our interests here. To one point, however, it may be well to draw attention. To read these equations in their broadest interpretation we must be prepared to consider cases in which the phenomenon of lag or lead enters. Perhaps the terms lag and lead require explanation. In some cases the course of events today depends on certain features in the state of the world at a previous date. So, for example, the number of persons of age 50 in the year 1924 depends (among other things) on the birthrate in the year 1874. Or, to quote another instance, the number of new cases of scarlet fever today depends on the number of infections a week ago. There is thus a lag in the appearance of the observable effect in the system. In other cases there may be a lead. The price of land on Church Street today may suffer an increase or perhaps decrease because it becomes known that in a year's time a railway station is to be built nearby. Since effects of this kind must be contemplated as a possibility, we must be prepared to read our equations in the following sense: The rate of increase ~T7~of the mass of the component Si at the at present instant, is a function of the masses Xi} Xz, etc., at some other instant of time, say Xi at (t pi), X2 at (t p2), etc., where some of the p's may be negative (corresponding to a lead). 48 ELEMENTS OF PHYSICAL BIOLOGY We must be prepared to consider our equations in this interpretation. Illustrative examples will not be offered here, as the mathematical treatment of these cases is somewhat troublesome. The interested reader will find an illustration in the author's monograph on the Ross Malaria equations, Am. Jour. Hygiene, vol. 3, January Supplement, 1923. Only a reflection of general character shall find its place here. It is characteristic of systems whose history is defined by equations thus involving a lag, that, in general, the course of events at a v a instant is dependent upon the previous history of the system over a certain finite range of time. The consequences of this feature are somewhat singular. If the world's events followed a system of equations of this kind, we might have two worlds, in every respect identical today, but each with a different past, and, in consequence each with a different future. And a similar reflection necessarily applies in the case of lead. This conclusion is perhaps not in harmony with a mechanistic conception of the universe. But the phenomena of memory and of will are of precisely such character as to introduce lags and leads into the world's equation, and we may be well advised to keep our minds open as to the possible effects of this circumstance upon the course of events. It should be observed, that the appearance of a lag or lead in our equation may be spurious. It may be due to a species of mathematical shorthand. It is easier to describe a person as having become infected with scarlet fever three days ago, than to describe precisely his present state today ensuant upon that infection. Hence we may prefer to, or, for lack of detailed knowledge we may be forced to write our equations in terms of (t p), although, if all the facts were known, we could, were we so disposed, write them in terms of t. And the same reflection applies to the appearance of a lead in our equations. Whether, with complete knowledge of all circumstances bearing on the situation, there should still remain a residuum of influences that could find expression only in terms of a lag or lead, this, perhaps, is fundamentally the nature of the problem of the influence of consciousness upon the course of the world's historv. CHAPTER V THE PROGRAM OF PHYSICAL BIOLOGY . . . . It will be the function of this new branch of science to investigate biological phenomena as regards their physical aspects, just as Physical Chomistry has treated the physical aspects of chemical phenomena. Because thiy field has not yet been systematically explored .... the individual data of Physical Biology appear, as yet, as more or less disconnected facts, or as regularities for which no proper place is found in the existing scheme of pre,Bent-day science; and the investigations of isolated problems in this field are as yet carried on as something of a scientific hobby by amateurs, with the result that they are guided by chance rather than by plan. . . . and are often totally lacking in any fundamental guiding principles or connecting theo.'y. As results gathered in this disconnected fashion accumulate, the need of their unification into a harmonious whole, into a distinct discipline of science, becomes more and more acutely felt. Such unification necessarily involves the working out of a viewpoint that shall make the several facts and relations fall in line naturally in an orderly system; in other words, what is needed is a labor of organisation. In the course of this, new and unforeseen problems will inevitably arise, and a fruitful field of scientific endeavor should thus be opened for the investigator. Porstmann. A first use to which we may with advantage put the results of the preceding analysis, is to systematise the subject here treated; there will thus be gained a general plan of work and a division of the topic into natural sections, upon which the arrangement of the succeeding chapters will, in the main, be based. Physical Biology, 1 as here conceived and discussed, is essentially a branch of the greater discipline of the General Mechanics oj Evolution, the mechanics of systems undergoing irreversible changes in the distribution of matter among the several components of such system. 1 In introducing the term Physical Biology the writer would suggest that the term Biophysics be employed (as hitherto) to denote that branch of science which treats of the physics of individual life processes, as exhibited in the individual organism (e.g., conduction of an impulse along nerve or muscle); and that the term Physical Biology be reserved to denote the broader field of the application of physical principles in the study of life-bearing systems as a whole. Physical biology would, in this terminology, include biophysics as a subordinate province. For a summary statement of what might be termed the program of biophysics see A. Forbes, Science, 1920, vol. 52, p. 331. 49 50 ELEMENTS OF PHYSICAL BIOLOGY It so happens that many of the components that play an tant role In nature, both organic and inorganic, are built large numbers of individuals, themselves very small as compe The with the aggregations which they form. Accordingly the stud^ono- S3 r stenis of this kind can be taken up in two separate aspects, nam x- 3, first with the attention centered upon the phenomena displaceby the component aggregates in bulk; we may speak of this as hose Bulk Mechanics or Macro-Mechanics of the evolving system. A^al, secondly, the study of such systems may be conducted with f eviattention centered primarily upon the phenomena displayed The the individuals of which the aggregates are composed. This brand's of the subject may suitably be termed the Micro-Mechanics^wo the evolving system. It is evident that between these two branc'ent or aspects of the general discipline there is an inherent relat-ilar arising from the fact that the bulk effects observed are of the na of a statistical manifestation or resultant of the detail workiiistic the micro-individuals. The study of this inherent connected of accordingly, the special concern of a separate branch which w^ads speak of as Statistical Mechanics, This terminology is i]P our coincident with accepted usage, but in part must be unden the to refer to an expansion of the subject beyond the bounds h covered, whereby its scope shall be extended so as to inched in statistical treatment of the dynamical problems presented &thegregates of living organisms; that is to say, aggregates of ? betransformers possessing certain significant special properties sribe Each of the branches of the mechanics of evolution enur'SAce so far naturally splits up into two subdivisions, according v be devote our attention to the material changes or to the energy ch all involved. By an extension of prior usage in physical chemistr^n may employ the term Stoichiometry to denote that branch of " science which concerns itself with the material transformations., with the relations between the masses of the components. The discussion of this branch presents itself as the more elementary task, and will therefore be taken up first; after this has been disposed of we shall be better prepared to discuss the second aspect, the Energetics or Dynamics of Evolution. Taking now a survey of the Stoichiometry of systems in evolutionary transformation, we can hardly find a better guide, for the organization of this subject, than the fundamental equations PROGRAM OF PHYSICAL BIOLOGY ^7 = F, (X, X,, . . . Xn; P, Q) at which we may speak of as the fundamental equations of the Kinetics of Evolution, since they furnish expressions for the velocities of transformation and exhibit the relations between these velocities and the masses of the several components, as well as the parameters P, Q. The very form of these equations suggests, as the first and most elementary problem, the treatment of the case of evolution under constant conditions, as defined by constant P's and Q's. This will, accordingly be the coarse here adopted, treating first the general case of n variables Xi, X2 , . . . Xn , and then some special cases in which the number of variables is restricted to 1, 2 and 3. The perfectly general case, of evolution under conditions of wholly unrestrained variability of the P's and Q's, is mathematically uninviting (though not wholly intractable), and is also of minor interest in practice. Little will therefore be said of this. Certain special types of changes in the P's and Q's (e.g., slow changes) will find a place in the next subdivision of the general subject, the Statics of evolving systems. This branch is, in a sense, a special division of the Kinetics of Evolution, namely that which concerns itself with systems in which the velocities of transformation are zero, so that there is Equilibrium, or, to be more exact, a Steady State. This, of course, implies, strictly speaking, constancy of the parameters P, Q. But something very much like equilibrium presents itself in certain cases when these parameters change slowly. There may then arise what has been termed a Moving Equilibrium. In view of the important role which such moving equilibria play in nature, their discussion must form a part of the program of Physical Biology. A second special problem of evolution under changing conditions (changing parameters P) that lends itself to treatment with comparative ease, is that which concerns itself with initial and end states (equilibria), as influenced by changing conditions, without demanding any information regarding the intermediate steps passed through by the evolving system. So, in physical chemistry, we may enquire what will be the effect, upon equilibrium, of a change in pressure or in temperature. Similar questions may be raised regarding 52 ELEMENTS OP PHYSICAL BIOLOGY equilibria or steady states in life-bearing systems, and the matter calls for at least passing notice. This leads to the consideration of the Principle of Le Chatelier and, as a natural sequel of the train of thought thus started, to the examination of relations which may exist between certain of the parameters P, somewhat as, in physical chemistry, significant relations exist between pressure and volume, for example. It is found that some, at any rate, of the parameters P present analogy to the intensity and the capacity factors of an energy; out of this have arisen in the past sporadic efforts to establish systems of social dynamics and the like, which, however, have been based upon an acceptance as identity of what is only analogy. Those who have followed this road have been led, not so much perhaps to erroneous conclusions, as to blind alleys, to barren fields. True progress can be expected only by retracing one's steps from such tentative excursions and striking out in a new direction; forsaking the way of quasi-dynamics, and breaking a trail toward a system of true dynamics, both of the individual (micro-dynamics) and of the system as a whole (macro-dynamics). Of intra-species evolution, as expressed in changes in the parameters Q that define the character of the several species, little will be said here. The reasons and justification for this step-fatherly treatment of so important an aspect of our topic have been set forth in the preceding text. A discussion of at least one phase of intra-species evolution, falling under the head of dynamics, will, however, be presented when dealing with that phase of the subject; and we shall briefly note, in due course, some aspects of intraspecies evolution, as discussed more particularly by J. B. S. Haldane. These, in broad outline, are some of the principal land-marks in the territory ultimately to be covered by Physical Biology, and to be given a preliminary survey here. In concentrated form the lay of the land, as set forth above, is sketched in the diagram or scheme table 1, which should be found helpful both in presenting to the eye the salient features of the field of investigation, and als'i in furnishing a logical basis for the systematic arrangement of the subject in the ensuing chapters. It remains, in this chapter, to enumerate the methods by which Physical Biology may be expected to develop. For the gathering of data two methods are available: observation in natural condi- 1 .2 -S Q, 1H O " 54 ELEMENTS OP PHYSICAL BIOLOGY tions, and observation under experimental (laboratory) conditions. Examples of both these methods will be noted. For the elaboration of data, the establishment of regularities (Jaws/, there is available in this field, as everywhere in science, the method of induction, aided, if need be, by statistical technique. In this volume, however, emphasis will be laid upon deductive methods of mathematical analysis, as applied either to data furnished by observation, or to "unknown" quantities, blanks, as it were, in our formulae, ready for numerical substitution whenever concrete data become available. The principal subdivisions of our topic, and the relations between them, as outlined above, are summarised graphically in table 1. KINETICS CHAPTER VI THE FUNDAMENTAL EQUATIONS OF KINETICS OF EVOLVING SYSTEMS L'emploi des signea mathe'matiques est chose naturelle toutes les fois qu'il s'agit de discuter des relations entre des grandeurs. A. Cournot. General Case. We now proceed to the systematic study of the subject in accordance with the general plan laid down in the preceding survey of the Program of Physical Biology. According to this schedule (table l)we approach first of all the section of Macromechanics (that is to say, the mechanics of evolving systems regarded as bujlt up of component species in the gross), without carrying the analysis down to the finer details of individual organisms. And, of the field of Macromechanics, we shall here take up the section of Stoichiometry, that is to say, we shall for the present confine our attention to the relations between the masses involved, leaving aside for a later section the associated energy changes. Of the general field of Stoichiometry the first division to be taken up, according to our schedule, is the Kinetics of Evolution, and we shall here begin with a brief consideration of the Fundamental Equations in their general form = Fi (* Xtl . . . XK ; P, Q) (1) at One phase of the general problem before us must evidently be the study (by observation, experiment, or any other method available) of the character or form of the functions F which tell us how the growth of each component is dependent upon the other components and the parameters P and Q. It might be supposed, indeed, that until this phase of the problem had received consideration, the system of equations (1), would be at best a barren expression of facts. But this is a misconception. Without knowing anything regarding the precise form of these functions, a good deal of information of considerable interest can be derived from these equations; and before proceeding to the consideration of concrete 57 58 ELEMENTS OF PHYSICAL BIOLOGY cases, in which something is known regarding the particular form of the functions F, it is proper, at this point, to extract from the fundamental equations (1) all the information that we can. This requires a little mathematical manipulation of comparatively simple character, The variables X, the masses of the several components of the system, are not, in general, wholly independent. They are subject to certain constraining relations. For example, for any self-contained system, we shall have an equation of the form X, Xa + . , .+Xn = SZ = A = const. (2) expressing the constancy of the total mass of the system; and a similar equation holds separately for every chemical element. 1 These equations prohibit certain changes of mass in the system. They are analogous to equations introduced in mechanical problems^^,^ /by the geometric constraints that limit possible displacements (as in the case of a ball rolling down an inclined surface, and prevented, by the resistance of the surface, from falling vertically). They are commonly spoken of as equations of constraint. Equations of constraint such as 2Z = A = const. will in general enable us to eliminate certain of the variables X, expressing them in terms of the other X's and of certain constants A. If, by the aid of m such equations of constraint, m variables have been eliminated, the system of equations (1) can be reduced to a simpler one, of identical form, but containing only (n m) variables ^.. ( and the same number of equations. .-. { In all that follows we shall assume that this has been done, that we now read equations (1) in this sense : the n variables Xi X% . . . . Xn are those left over after eliminating as many of the X's as the equations of constraint permit. The functions F will in general, after this elimination, contain constants A introduced by the equations of constraint. We shall now, except where otherwise stated, restrict our considerations to the case in which the parameters P and Q and A are either constant, or change so slowly that we may disregard ff /"' 1 Except in those rare cases in which radioactive or other atomic disintegra- /' ticms occur. / *_ FUNDAMENTAL EQUATIONS OF KINETICS 59 their variation. This means that we restrict ourselves to the consideration of simple inter-group evolution under constant condi- tions. With this understanding, the first point we may observe about the system of equations (1) is that they define certain conditions of equilibrium, or, to be more precise, of steady states. For such a state ensues whenever all the velocities vanish, that is to say, according to (1) whenever Fi = F, = . . . = Fn = (3) We thus have n equations between the n variables Xi, XZi . . . Xn, which, in general, determine certain values (4) such that when masses of the several components have these values, they persist in these values; the system is at rest, as regards changes in the distribution of matter among its components Si, S2 , . . . Sn . In general there will be a number of such possible equilibria, some of which will be stable, some unstable. The determination of their number and character is a technical point in the theory of equations, for the general treatment of which the reader must be referred to the pertinent literature (see, for example, Picard, Traite" d' Analyse, vol. 1, 1891, pp. 83, 123; vol. 2, 1893, pp. 183, 193, 196, footnote) . To give a touch of concreteness to the discussion at this stage a very simple example may be given to illustrate how several equilibria may occur in a life-bearing system. A perfectly screened dwelling may be kept indefinitely free from flies. This is a condition of equilibrium, but of unstable equilibrium; for if only a few flies gain access, presently these will breed, and the room will become inhabited by a population of flies whose number will depend on the amount of food present, on the measures taken to combat the pest, etc. Unless these measures are v,ery active, the flies will not be wholly exterminated, but the population will attain some approximately steady number (for a given season) . There are, then, in this case, two possible equilibria; one with a zero population of flies, the other with some positive number of fly population. 60 ELEMENTS OF PHYSICAL BIOLOGY The equilibria in nature, involving countless species, are of course much more complicated in character, but the general principle is the same; and we must expect that in general a variety of different equilibria are possible, some unstable and some stable. For the further discussion of the equations (1) it is now desirable to express these relations, not in terms of the masses X} but in terms of the excess of each mass Xi over its corresponding equilibrium value, xi = Xi-d (5) The equation (1) then takes the form , ~r- = / i at (6) the parameters P, Q being omitted, for the sake of brevity. Expanding the right hand member by Taylor's theorem we obtain the system of equations dt dt + + + . -f dt A general solution of this system of equation is (7) (8) where the (?'s are constants, of which n are arbitrary, and Xi, X2 . . . Xn are the n roots of the equation 2 for X Oil X 0,ii . . . dm - 2)(X) = (9) 2 This equation is commonly spoken of as the characteristic equation. For greater detail see A. J. Lotka, Proc. Am. Acad. Sci., vol. 55, 1920, pp. 137-153. FUNDAMENTAL EQUATIONS OF EJNETIC3 61 It is seen by inspection of the solution (8) that if all the X's are real and negative, xi} x2 , . . , xn all approach zero as t increases toward infinity, since e~m = 0. But according to (5)., as the re's approach zero, the X's approach their equilibrium valu_es C. In this case, obviously, equilibrium is stable, since, by allowing sufficient time to elapse, we can always make the system approach as near as we please to Xi = Ci, for all values of the subscript i. Precisely similar conclusions hold if some or all of the X's are complex, and the real parts of all the X's are negative. If all the roots X ar( e real (and negative), 3 each term in the solution (8) diminishes continually and approaches zero asymptotically as t approaches infinity. If all the constants G are of the same sign, the sum. of the series also will, evidently have a similar type of approach to equilibrium. If some of the G's are positive, others negative, there may be a species of irregular oscillations, the mass X of the component rising sometimes above its equilibrium value (7, sometimes falling below it. Ultimately, however, the equilibrium is approached from one side only, s,ince ultimately tbe term containing the numerically smallest X will predominate over all other terms. If some of the roots X are complex, the solution will contain truly oscillatory terms, since the exponential function, for complex exponents, assumes the trigonometric form g ft _}_ i gin ft) (10) In this case there will be regular oscillations about the equilibrium position; in general these oscillations will be damped, that is to say, their amplitude will diminish, so that equilibrium is approached more and more closely, but always with oscillation the equilibrium is approached from both sides at once, so to speak, the oscillations persisting forever, though on a diminishing and ultimately vanishing scajle. These conclusions are the analytical confirmation and extension of an inference drawn by Herbert Spencer 4 on qualitative grounds : 3 The analytical condition that the real parts of all the roots X shall be negative is given by Hurwitz, Math. Ann., vol. 46, 1895, p. 521. See also Blondel, Ann. de Physique, 1919, pp. 117, 153. It might be noted here that a necessary though by no means sufficient condition, evidently is that the absolute term in D (X), that is to say D (0), shall be positive when n is even, and negative when n is odd; for this absolute term is equal to the product of all the roots X. * Herbert Spencer, First Principles, Chapter 22, Section 173. 62 ELEMENTS OF PHYSICAL BIOLOGY Every species of plant and animal is perpetually undergoing a rhythmical variation in number now from abundance of food and absence of enemies rising above its average, and then by a consequent scarcity of food and abundance of enemies being depressed below its average .... amid these oscillations produced by their conflict, lies that average number of the species at which its expansive tendency is in equilibrium with surrounding repressive tendencies. Nor can it be questioned that this balancing of the preservative and destructive forces which we see going on in every race must necessarily go on. Since increase of numbers cannot but continue until increase of mortality stops it: and decrease of number cannot but continue until it is either arrested by fertility or extinguishes the race entirely. It will be observed, however, that our analysis enables us to be considerably more specific in distinguishing several modes of approach to equilibrium, and in indicating the particular conditions under which each occurs. A point that here deserves particular emphasis is that, in order to make these distinctions and indications, it is by no means necessary to have a complete knowledge, or even very extensive information regarding the functions F. Only the coefficients of the first (linear) terms in the Taylor expansion of these functions enters into the determinant D(X),, and only these need therefore be known to draw the requisite conclusions regarding the stability and mode of approach of equilibrium. Furthermore, Spencer's commentary relates specifically to the case of species related to each other in certain particular ways (food, enemies, etc.): the analysis here given is framed on perfectly general lines and covers any sort of interrelation, interdependence of the components Si, S . . . Sn . Certain particular interrelations will be duly considered in the course of the further development of the theme. Here it may be well to draw attention once for all to the fact that there is nothing whatever to restrict the application of the principles and methods set forth to systems in organic evolution. Indeed, a typical example to which these reflections apply is the case of a chain of elements in the course of radioactive trans- formation.5 It will be seen later, in considering a concrete example, that the equilibrium equation (12) may yield zero or negative roots for C. A zero root is simply interpreted; if the equilibrium to which it relates is a stable one, this means that the species in question will 5 A. J. Lotka, Proc. Am. Acad. Sci., vol. 55, 1920, p. 148; Proc. Natl. Acad. Sci., vol. 7, 1921, p. 168; Phil. Mag., August, 1912, p. 353. FUNDAMENTAL EQUATIONS OF KINETICS 63 become extinct 1 '. It is unfit, is unadapted ultimately 7 to survive under the existing conditions8 (as defined by the parameters P, etc.). A negative value of C may also signify that the species is incapable of survival under the existing conditions. Masses cannot assume negative values. As soon as any component passes through zero it ceases to function in the system, whose history is henceforth represented by a new set of equations in which this component does not appear. These conclusions must in one respect be accepted with a certain caution. Since there may be several equilibria, a species may be incapable of existence in the neighborhood of one such equilibrium, but might nevertheless succeed in maintaining itself in the neighborhood of another equilibrium. Whether such cases occur in practise may be left an open question. Our analysis suggests this possibility. e This conclusion does not apply, of course, if the equilibrium with X = O is unstable, as in the example of a fly population cited above. 7 It maj*, however, persist for a time, and, it may be, for a long time. An instance in point is furnished, outside the field of organic evolution, by a chain of elements in radioactive transformation. Although here the ultimate equilibrium is one with a single survivor, namely the last link in the chain, yet for millions of years the several products exist side by side in constant ratio though in slowly diminishing amount. At the head of such a chain is always found a "parent substance" which is the longest-lived in the chain. This is not accident. It is easily shown that if at some prior period this substance was preceded by a more rapidly decaying pre-parent, this latter must have disappeared in the course of the ages. It is totally unfit, unadapted, even for a temporary equilibrium, under present conditions. (See A. J. Lotka, Phil. Mag., August, 1911, p. 354.) 8 It should hardly be necessary to point out that adaptation is purely relative. CHAPTER VII FUNDAMENTAL EQUATIONS OF KINETICS (CONTINUED)- SPECIAL CASE: SINGLE DEPENDENT VARIABLE If arithmetic, mensuration and weighing be taken away from any art, that which remains will not be much Plato. Law of Population Growth. It will add concreteness to the present exposition to consider at this point a numerical illustration. The simplest possible example of numerical application of the equations set forth in the preceding pages will be one in which there is only a single variable X. The fundamental system of equations then reduces to a single equation f=F(JT) (1) at A. case in point arises when for any reason one particular biological species or group grows actively, while conditions otherwise remain substantial!}" constant. This seems to be essentially what has occurred in certain human populations. It is true that, in their growth, they have carried along with them a complicated industrial system or group, comprising both living and non-living elements. We may, however, look upon the number of the human population itself as a sort of single index or measure of the growth of the group as a whole.1 1 This is an example in which certain of the variables X are connected by equations of constraint. So, for example, the number of head of cattle Nc has for many years past, in the United States, been about six tenths of that of the human population, Nh so that we have an equation of constraint or, putting the average mass of cattle at 1000 pounds per head, that of a human being at 100 pounds (an average to include all ages) Xe = Similar equations of constraint apply to the other species of domesticated animals and plants, so that the mass of each can be (approximately) expressed / in terms of the single variable Xh. 64 FUNDAMENTAL EQUATIONS OF KINETICS 65 Applying to this case the equation (1) and the general method set forth in the preceding pages, we are led to consider first of all the equilibrium equation ^ - F OT) = (2) at This equation, obviously, has a root at X = 0, for at least one female is required to start the growth of a population. Expanding by Taylor's theorem we shall therefore have for F a series lacking the absolute term, 2 thus = F (X) = aX + 6X> + cX3 + . . . (3) dt Furthermore, the equation (2) will have at least one other root, since there must be some upper limit to the growth of the population. The simplest case satisfying this condition is that in which the right hand member of (3) terminates at the second degree term, i.e., ^f = oZ + &Z (4) at The characteristic equation 3 for X is in this case simply A - a = (5) and the solution of (4) therefore is X = (?*' + Sue20 ' Substituting this in (4) and equating coefficients of homologous terms we find Gn =-at -p at _ 1 dX2 Otherwise would not vanish, with X dt 3 Corresponding to equation (9), Chapter VI. 4 The series (6) is divergent for large values of t if a is positive. But the expression (9) for the sum of (6) remains a solution of (4). 66 ELEMENTS OF PHYSICAL BIOLOGY In formula (9) either Gi or the origin of time is arbitrary. A simplification can be effected by so adjusting the origin of time that (10) This fixes the value of the constant Gi (?:=-- (11) and the formula (9) becomes The equation (9) can also be written in another form. If we denote by X the value of X when t = o, and write x = X + 7, then (9) becomes a X = --- (13) "'- 1 Population of United States. Formula (12) has been applied by Pearl and Reed6 to the population growth of the United States. 7 The calculated curve for the number TV of the population fits the observed data over a long period of years (1790 to 1910) with remark- 5 This result can also be obtained by direct integration of (4) in finite form. The process given above has here been followed to illustrate the general method of the solution (S), (9), of Chapter VI. 6 P. F. Verhuist, Mem. Acad. Roy. Bruxelles, 1844, vol. 18, p. 1; 1846, vol. 20, p. 1; R. Pearl and L. J. Reed, Proc. Natl. Acad. ScL, vol. 6, 1920, p. 275; Scientific Monthly, 1921, p. 194; R. Pearl, The Biology of Death, 1922, p. 250. The last-mentioned work, especially, should be consulted for a detailed discussion. For a general treatment of the population problem see also particularity E. M. East, Mankind at the Crossroads, 1923 (Scribners). 7 Measured, in this case, by the increase in the number N of persons. This Is evidently, in first approximation at any rate, proportional to the total mass X of the population. FUNDAMENTAL EQUATIONS OF KINETICS 67 able faithfulness, as will be seen from table 2 and the graph shown in figure 4. Numerically the formula (12) here takes the form N = 197,273,000 1+e-,-0. 03134 1' (14) and the time t' (in years) is dated from April 1, 1914 (t 1 , being negative for dates anterior to this). This epoch is one of peculiar interest. It represents the turning point when the population passed from a progressively increasing to a progressively diminishing rate of growth. Incidentally it is interesting to note that if the population of the TABLE 2 Results of fitting United States population data 1790 to 1910 by equation (14) United States continues to follow this growth curve in future years, it will reach a maximum of some 197 million souls, about double its present population, by the year 2060 or so. Such a forecast as this, based on a rather heroic extrapolation, and made in ignorance of the physical factors that impose the limit, must, of course, be accepted with reserve. Stability of Equilibrium. The equilibrium at X = 0, i.e., with total absence of human population, is evidently unstable, since A = a and a is an essentially positive quantity, its numerical value being, for the population of the United States, 0.0313395. The second equilibrium, corresponding to the saturation point, is evidently at 88 ELEMENTS OF PHYSICAL BIOLOGY X = r , and here it is easily found by the substitution x = X + that X = a, the equilibrium is stable. FIG. 4. THE LAW OF POPULATION GROWTH FOR THE UNITED STATES ACCORDING TO PEARL AND REED The lower S-shaped limb corresponds to the actual approach to equilibrium from below. The upper limb represents the presumptive course of events for a diminishing population approaching equilibrium from above. FUNDAMENTAL EQUATIONS OF KINETICS Experimental Populations. Pearl has also fitted the same formula to the population of a number of countries, but the range covered by the available observation in these other cases is less extended, so that there is less opportunity for comparison with observed figures. Of particular interest is an application of the same formula, also by Pearl, to an experimental population of fruit flies (Drosophila). In this case practically the entire range of the S-shaped curve defined by equation (12) is realized, and a glance at the plot in figure 5 shows that the agreement of the observed figures (represented by small circles) and the calculated curve is exceedingly satisfactory. Still closer is the agreement in the case of bacterial cultures studied aso ss-s 125 JOO GftOWH Of DKOSOPHILA z Days. FIG. 5. GROWTH OF A POPULATION OF DROSOPHILA (FRUIT FLIES) TJNDEB CONTROLLED EXPERIMENTAL CONDITIONS, ACCORDING TO PEARL AND PARKER by H. G. Thornton8 (Annals of Appl. Biology, 1922, p. 265), whose observations are set forth in table 3 and are shown by the small circles in figure 6 ; the theoretical curve to fit these points, as computed here in the laboratory, is shown in the fully drawn line. As will be seen the agreement is excellent. This is due in part to the fact that the figures plotted represent the means of a number of individual cultures. A veiy particular interest attaches to this example, inasmuch as it forms, as it were, a connecting link between the law of growth of a 8 Similar results have been obtained by A. G. McKendrick and M. Kesava Pai, Proc. Roy. Soc. Edin., vol. 31, 1911; for a study of the growth of yeast, see A. Slator, Trans. Chem. Soc., 1921, vol. 119, p. 126. 70 ELEMENTS OF PHYSICAL population, and the law of growth of the individual. A colony of unicellular organisms, regarded as a whole, is analogous to the body of a multicellular organism . Or, to put the matter the other way about, a man, for example, may be regarded as a population of cells. We need not, therefore, be greatly surprised, if the growth of the multicellular organism should be found to follow a law similar to that exhibited by populations. And in point of fact, as will be shown a little further on, this expectation is in not a few instances fulfilled. TABLE 3 ifrowth of bacterial colony, according to H. G. Thornton (Ann. Appl, Biol., p. 865) For graph see figure 6 *According to the equation y = 0.2524 e +0.005125 Diminishing Population. It may be noted here that in one respect the formula (12), while particularly simple in form, is of more restricted scope than (13). The former defines the characteristic Sshaped curve that appears in the graphs of actual populations shown in figure 4. But formula (13) gives a more complete definition of a curve composed of two limbs; one of these is the S-shaped curve already considered. The other is a steeply descending arc, shown in the upper portion of figure 4. This portion of the curve has not been 4 FUNDAMENTAL EQUATIONS OF KINETICS 71 realized in any recorded population. It represents the computed course of events if the population initially exceeds its equilibrium strength, i.e., if is positive. so 43 Pays. FIG. 6. GEOWTH OF A BACTEBIAL COLONY (B. DENDEOIDES) Observations by H. G. Thornton Growth of Individual Organism. Although, strictly speaking, the growth of the individual organism is a subject properly belonging to the field that has here been termed "micromechanics" (Chapter V), yet, in view of the very close analogy which has been found to exist, in certain cases, between the law of growth of a population, and that of the individual, it may be noted here that the formula (9) has also 72 ELEMENTS OF PHYSICAL BIOLOGY been applied by T. B, Robertson9 and by Wo. Ostwald10 and others, to the growth of the individual organism. An example of such application Is shown in figure 1, which exhibits the growth day by day, of male white rats according to observations by H. H. Donaldson" and computations by T. B . Robertson. The fully drawn curve represents the calculated values of the mass of the rats (in grams) at different ages. The circles indicate selected observed values, namely, those which diverge most widely from the computed values. It will be seen that up to about the one hundredth day the agreement is good. Above this there is no agreement worthy of the name. Another example,, and one in which the computed curve fits the observed values with remarkable agreement, is the growth (in height) of sunflower plants as studied by H. S. Reed and R. H. Holland.12 The curve to fit these observations has been recomputed by the method of least squares by Dr. L. J. Reed, who has very kindly placed his results at the author's disposal. They are shown in figure 8. The observations on which they are based are shown in table 4. It will be seen that the fit is practically perfect through the whole range of observations. In practice we are not usually given the differential equation (4), but data corresponding to points on the integral curve (12). We then have the problem of determining from these points the characteristic constants of the curve. The detailed working out of theprob- 9 Archiv liir die Entwiekelungsmeehanik der Organismen, 1907, vol. 25, p. 4; 190S, vol. 26, p. 108; The Chemical Basis of Growth and Senescence, publ. Lippincott, 1923. T. B. Robertson also quotes A. Monnier, Publications of Irist. of Botany, Univ. Geneva, 1905, which in turn refers to Chodat as having recognized the analogy of organic to autocatalytic growth. The idea is rather an obvious one, which probably has occurred to many. The earliest reference noted by the writer is L. Errera, Revue de 1'Univeriste de Bruxelles, 1899-1900, May issue. Something very similar is found in Ostwald, Vorlesungen Ober Naturphilosophie, 1902, p. 342. These last-mentioned lectures were published in 1902. but were actually delivered somewhat prior to that date. The writer recalls that Ostwald referred to the matter in his lectures on General Chemistry in 1902, and probably others will recall similar references on earlier occasions. 10 Die Zeitlichen Eigenschaften der Entwickelungsvorgange, Leipzig, 1908. 11 Boas Memorial Volume, 1906, p. 5; see also the same author's book The Rat, 1915. 12 H. S. Reed and R. H. Holland, Proc. Natl. Acad. Sci., vol. 5, 1919, pp. 135-144. FUNDAMENTAL EQUATIONS OP KINETICS 73 lem may well be left to the reader, after pointing out the following interesting property of the curve (12). Taking reciprocals and writing A for a/b, we have _ _3 a_/o) A" log (A% -1) = - o(f-* ) (15) (16) oo O SO 100 (SO ZOO ZSQ 3CO Ays. in days. FIG. 7. GROWTH OF RAT ACCORDING TO H. H. DONALDSON AND T. B. ROBERTSON Circles indicate only those observations that diverge most widely from the calculated curve. where t is the time corresponding to the point of inflection of the Scurve. Thus if we plot A 1 against t on logarithmic curve paper, we shall obtain a straight line diagram. This is shown in figure 9 for the same data (growth of sunflower) which have already been 74 ELEMENTS OP PHYSICAL BIOLOGY 00 y- Z6/.I O 7 H 2/ 28 35 -?2 +9 ?& 63 TO 77" & $2 All animal species, and many plants also, thus derive their substance from other species on which they feed. And several different types of this form of interdependence are observed. In the first type, (a) the organism $2 kills Si outright in the process of feeding upon it. We might term S2 in such a case an episite of Si, in contradistinction from the second type, (&) in which 2 lives on Si without killing it outright, being parasitic upon Si. The host is in most cases more or less injured by the parasite, and all pathogenic organisms fall into this class. For this reason quantitative epidemiology appears as one of the special branches of the general subject under consideration here. A third type (c) of interdependence, is that in which S2 is saprophagous or saprophytic, feeding upon the cadavers of Si after death from other causes; or, /S2 may live on waste products discharged by Si. In contrast to episites and parasites, saprophagous species are presumably beneficial rather than injurious to the host species, since they function as scavengers. Still another type, (d), of interdependence is that of symbiosis, in which Si and *S2 live in partnership which, as a rule, is in some degree mutually beneficial. Man and his domesticated animals and plants are obvious examples of this type. 77 7S ELEMENTS OF PHYSICAL BIOLOGY In addition to these types (Id) to (Id), another large group of cases (2) are those in which two or more species compete for a common food supply. In their general form the fundamental equations of kinetics for the case of two dependent variables are dt dl -j- AuXi -r AitXz + . + AtiXi -r AttKi T . (1) or, after the transformation (5), of Chapter VI = anXi -f- at dxs ~dt = CsjXj + QssZs 4- . . . (2) We may note, first of all, as a general rule, the following observations regarding the coefficients a in the several types of interdependence enumerated above: la. S2 lives on Si by killing Si outright (episitic type). In this case, evidently S2 unfavorably influences the growth of Si} while, on the contrary, Si is advantageous to the growth of &, so that 5 dZi Z2 dt < 0, i.e., an < t ~ > O, i.e., an > oXi at (3) (4) lb. 82 parasitic upon Si. Here aiz < 0, 021 > 0, as in case la. Ic. S2 saprophytic upon Si, or living upon waste products of Si. Here we may expect that aiz ^ 0, a2i > 0. Id. S2 feeds on Si, but at the same time cultivates it in symbiosis. Here aiz > 0, a2i > 0. The characteristic equation for two variables is X X = (5) FUNDAMENTAL EQUATIONS OF KINETICS 79 or, In expanded form, X2 (an + o^X + (andn 021^:2) = (6) X = I { (au + a22) =*= V(au - a22 ) 2 + 4a2 iai2 } (7) Certain general conclusions follow immediately. So, for example, if ai, ais are both of the same sign, as in the case of saprophytes and of symbiosis, the quantity under the radical is necessarily positive, and hence both roots for X are real. The oscillatory type of approach to equilibrium is here excluded. In the case of two species of the type (la) or (16), the episitic or parasitic type, on the contrary, the possibility of oscillations is indicated, under conditions where the equations (1) are applicable. CONCRETE EXAMPLES Martini's Equations for Immtinizing Diseases. Numerical applications of the case of two dependent variables are not easily obtained. Of concrete examples in general terms (with unknown or very imperfectly known values of the constants involved) several are to be found in the literature. The simplest of these is a case for which the equations are given, without solution, by Martini in his Berechnungen und Beobachtungen zur Epidemiologie der Malaria (Gente, Hamburg, 1921, p. 70), namely, the case of the growth of an endemic disease of the type that confers acquired immunity upon persons who recover from it (e.g., measles, scarlet fever, etc.) Martini writes u = fraction of the population affected and infective i = fraction of the population not available for new infection (i.e., immune or already affected) (1 _ i ) = fraction of the population available for new infection p fraction of the population newly affected per unit of time q = fraction of the population of affected population that ceases to be so, per unit of time, by recovery or by death m = fraction of "unavailable" population that loses immunity or dies per unit of time a = infe.otivity (a proportionality factor) Martini puts the newly affected population, per unit of time, jointly proportional to the infective population u and to the population available for new infection, (1 i), so that p = a u(l t) 80 ELEMENTS OF PHYSICAL BIOLOGY Then, obviously, = a u(l - - qu = (a - q}u - a ui di I- (9) = a u(l i) mi = a u mi a ui di j The characteristic equation for X here reduces, near the origin, simply to l | (a _ q] _ A ) (m - X) = (10) and the solution, near the origin, is (7, ^-mt 4- . . 1 (11) from which it is seen that the equilibrium near the origin is stable if and only if a < q There is a second equilibrium at in (a q) = I (12) Since, however, i can in reality assume only positive values, this equilibrium has a meaning only if a > q, i.e., just in the case in which the equilibrium at the origin is unstable. Hence we conclude that if a. < q the equilibrium at the origin is the only possible one, and is stable, so that the disease will die out. In the other alternative, a > q, the second equilibrium has a real meaning, and we can develop a solution in series - = ' Xlt ' X!t 1 (13) i - I = (?'SlleXj *+ (?' 2 , 2 e X2t + . . . where X3 , X2 are given by q- 1 A. J. Lotka, Nature, vol. Ill, 1923, p. 633. gi FUNDAMENTAL EQUATIONS OF KINETICS Oi We need not here consider the case (a - q) < 0, for, as pointed out above, in this case the second equilibrium is meaningless. But when a > q, it is seen from (14) that the real parts of the two roots will then in any case be negative, so that the equilibrium, if it exists at all, is stable. Furthermore, there will be two real and distinct, two real and coincident, or two complex roots, according as a- q 1 m ~> _ ft K) 2. -1 - \i"J a" a 4 q < In the last-mentioned case equilibrium will be approached by a series of oscillations above and below the final state of equilibrium, so that a series of "epidemic" waves will appear, a feature which has an obvious interest in connection with the type of disease here discussed.2 The oscillations thus occasioned by the factors duly taken into account in this elementary analysis may in practise be enhanced by factors here neglected, such as varying virulence of the disease, exhaustion of susceptible population, seasonal influences, etc. The last-mentioned, however, will in general tend to produce a separate series of waves whose period will have no relation to that of the oscillations derived above. For the special case = 1, Prof. G. N. Watson has given a complete solution, which may be consulted in the original. 3 It is to be noted that this case cannot, according to the analysis here presented, lead to oscillations, since the condition for oscillations according to (15) reduces to ^" :o (16) and cannot be satisfied, as the square of a real quantity is necessarily positive. The Ross Malaria Equations. A system of equations has been established by Sir Ronald Ross4 to represent, under certain 2 Compare J. Brownlee, Investigation into the Periodicity of Infectious Diseases, Public Health, vol. 25, 1915, p. 125. 3 G. N. Watson, Nature, vol. Ill, 1923, p. 808. 4 Sir Ronald Ross, The Prevention of Malaria, second edition, 1911, p. 679. This volume also contains a bibliography. For a detaile ddiscussion of the Ross malaria equations see A. J. Lotka, Am. Jour. Hygiene, January Supplement, 1923. 82 ELEMENTS OF PHYSICAL BIOLOGY conditions, the course of events in the spread of malaria in a human population by the bites of certain breeds of mosquitoes infected with the malaria parasite. These equations are of the same form as Martini's equations discussed above, and inasmuch as Ross's malaria equations have been very fully treated by the writer in a separate monograph, 5 their detailed study may here be omitted. It will suffice to reproduce from this monograph one of the curves representing the course of events, the presumptive growth of malaria in a human population, as defined by the differential equations of Sir Ronald Ross. -4 ~ t years FIG. 10. CUHVE OF GROWTH OF ENDEMIC MALARIA ACCORDING TO SIB RONALD Ross's EQUATIONS The upper (S-shaped) curve relates to the particular case in which the initial malaria rates in the human and the mosquito population stand in the ratio which they have at equilibrium or are both small. The lower curve represents the course of events when the initial malaria rate is 4.2 per cent in the human population, and 1.4 per cent in the mosquito population. (The zero of the time scale is arbitrary.) Ordinates are malaria rates (human) expressed as fraction of unity. (Reproduced from A. J. Lotka, Am. Jour, of Hygiene, January Supplement, 1923.) 5 A. J. Lotka, loc. cit. FUNDAMENTAL EQUATIONS OP KINETICS 83 It will be observed (fig. 10) that the curve showi consists of two parts, the one an Srshaped limb which, in point of fact, is very nearly identical in type with the Verhulst-Pearl population curve. The second limb ascends very steeply, almost vertically, and finally bends to join the S-shaped limb. The meaning of these curves is as follows: If a small nucleus of malarial infection is introduced into a (constant) population of human beings and mosquitoes, both being previously free from such infection, then the growth of malaria in the human population will follow the course represented by the S-shaped limb. It will be seen that the process is a rather leisurely one, its essential completion occupying about ten years, according to Ross's figures. (Strictly speaking it is never quite complete in a finite time.) Seasonal effects are here disregarded. On the other hand, if at the start there is already present a certain malarial rate in the human population, and also in the mosquito population, then, in the case here depicted, there is for a time a very rapid increase of malaria in the human population, until, in the brief space of about two months, the S-shaped curve is reached. After that the course of events is the same as in the first case. In practise, in temperate climes, we can expect only short sections of the S-shaped curve to be realized, owing to the interruptions of the seasons. No data are available for a numerical comparison of these results with observed conditions. Close agreement is not to be expected, as the Ross equations refer to a rather highly idealised case, a constant population both of men and mosquitoes. The latter could be even distantly approached only in the tropics. There is room here for further analysis along more realistic lines. It must be admitted that this may lead to considerable mathematical difficulties. The case of periodic seasonal influences is perhaps the one that promises to yield most readily to mathematical treatment. The Ross malaria equations are a typical example of equations affected with a lag, owing to the period of incubation. For a detailed discussion of this feature the reader must be referred to the author's monograph published by the American Journal of Hygiene. An Example in Parasitology. An interesting and practically significant case of inter-group evolution, of conflict between two species, has been made the subject of an analytical study by W. R. 84 ELEMENTS OF PHYSICAL BIOLOGY Thompson. 6 He considers a host species^ numbering initially n individuals, and a parasite species, initially p individuals. On a number of simple assumptions, for which the reader must be referred to the original papers, he develops the following formula for the fraction a of the host population attacked, in the t ih generation, by parasites pa* a = (a* - a) n -p a 1 where a is the ratio of the "reproductive power" of the parasite to that of the host, the reproductive power being measured by the number of eggs deposited per female. It is assumed that only one egg is deposited in each host. Putting a1 = ert (18) and X (19) P P Thompson's formula becomes, after a simple transformation, -^r-i (20) which will be recognized, once more, as the equation of the law of simple autocatakinetic growth. According to the value of a and K several different cases may arise, whose graphs are shown in figure 11. It should be observed that K = 1 according as a= 1 (21) r = according as a= 1 (22) < > In the special case that a = 1 the formula (20) becomes indeterminate and a is then given by P n-p(t-l) a hyperbolic relation (see fig. 11, the last diagram). (23) W. R. Thompson, Comptes Rendus Acad. Sci., vol. 174, 1922, pp. 201, 1443, vol. 175, p. 65. See also R. A. Wardle and P. Buckle, The Principles of Insect Control, Longmans, Green & Co., 1924. FUNDAMENTAL EQUATIONS OF KINETICS 85 Thompson gives a number of numerical examples exhibited in table 5 . From these examples and from this formulae he concludes that the invasion of the host species by the parasite may at first Fia. 11. COTJESE OF PAKASITIC INVASION OF INSECT SPECIES ACCOBDINQ TO W. R, THOMPSON proceed only very slowly, and that nevertheless, after a certain time, the increase may become very rapid. From a practical standpoint this is important to observe, since it implies that the first effect of "sowing" the parasite among a species of insect hosts, ELEMENTS OF PHYSICAL BIOLOGY with a view to destroying them, may be quite discouraging, and that this must not be taken as indicative of ultimate failure. This TABLE 5 Percentage (IQOa) of host species attacked by parasite in t lh generation, according to W. R. Thompson p= initial number of parasite species. 7i=initial number of host species. parasite host a=ratio of reproductive powers The figures in the columns headed 1, 2, 3, etc., denote the values of 100 a in the 1st, 2d, 3d, etc., generation. 7i'm& in J>OO \ \ \ \ FIG. 12. INCREASING DIBTUSION-IN-TIME OF STJCCBSSIVH GENERATIONS IN THE PEOGENY OF A POPULATION ELEMENT observation is especially significant since in practise one must often be satisfied with the introduction of a relatively very small number of parasites. So, for example, in using the parasite species FUNDAMENTAL EQUATIONS OF KINETICS 87 Liparis di&par, commonly about one thousand individuals have been sown. Supposing that there were one thousand million hosts, and that the parasite reproduced twice as fast as the host, it would require, according to Thompson's calculations, about 19 generations to exterminate the host; and then, even to the sixteenth generation, only 10 per cent or less of the host species would be attacked, Thompson's formula is open to certain objections. Its derivation seems to involve the assumption that each generation of the parasite is coextensive in time with the corresponding generation of the host. Furthermore, the use of a generation as a sort of time unit is unsatisfactory, because a generation is a very diffuse thing, spread out over varying lengths of time. This is easily seen by considering the progeny of a batch of individuals all born at the same time t 0. If we call this the th generation, and if fli, ao are respectively the lower and the upper limit of the reproductive period, then it is clear that the next generation, the first, will extend over the interval of time from aL to a2 , the second from 2a^ to 2a2 , the nth from nai to naz , an interval which will ultimately become very large as n increases, as shown by successive intercepts between the two sloping lines in figure 12. Less objectionable, perhaps, is the fact that Thompson's formula is expressed in terms of the "rate of multiplication per generation" of the two species. This term is not as clear as it might be. From the context it appears that it refers to the number of eggs deposited per female. This number is closely and simply related to the ratio 12 of the total births in two successive generations. If an individual of age a reproduces, on an average /3 (a) individuals per unit of time, the ratio R is evidently given by f* = j Jo (a)p(a)do The relation of this R to the rate of increase r per head of the population is not altogether obvious and cannot be expressed in simple form. For a population with fixed age distribution, it will be shown in Chapter IX that r is given by = e -ra p(a)p(a)fa |"SO / = I @(a)p(d)da r I a^(a} Jo Jo + (25) 88 ELEMENTS OF PHYSICAL BIOLOGY Hence Jra aj3(a)p(a)da + . . . (26) In view of the doubtful features in Thompson's formula which have been indicated above, it appears desirable to attack his problem in quantitative parasitology from another angle. We may do this by following the general method which has here been set forth and exemplified. Treatment of the Problem by the Method of Kinetics. Let NI be the number of the host population, &i its birthrate per head, (the deposition of an egg being counted a birth), and di its death rate per head from causes other than invasion by the parasite. Let kNiN* be the death rate per head due to invasion by the parasite, in the host population, the coefficient k being, in general, a function of both jVi and JV2 , the latter symbol designating the number of the parasite population. The birth of a parasite is contingent upon the laying of an egg in a host, and the ultimate killing of the host thereby. To simplify matters we will consider the case in which only one egg is hatched from any invaded host. If an egg is hatched from every host killed by the invasion, then the total birthrate in the parasite population is evidently kNiN*. If only a fraction k' of the eggs hatch, then the total birthrate in the parasite population is evidently kk' NiN, which we will denote briefly by KNiN2 . Lastly, let the deathrate per head among the parasites be dz . Then we have, evidently dt (27) dt ~ i 2 - - where rx has been written for (b{ dt). Regarding the function k, we shall now make the very broad assumption that it can be expanded as power series in NI and Nz , thus k = a. + &Ni + yN-t + . . . (28) FUNDAMENTAL EQUATIONS OP KINETICS It will be convenient first of all to consider an approximation. 7 If the coefficients 3, 7, etc., are sufficiently small, we shall have, for values of A'i, X* not too large, essentially at (29) (30) Integrating, and putting k'a TI (^21 a. we obtain d2 Iog(x + p) + n \og(y + q) - h'ax - ay = M (33) where M is an arbitrary constant of integration. Expanding by Taylor's theorem we find M' (34) By giving successively different values to the arbitrary constant Mr a family of closed curves is obtained for the plot of (34) in rectangular coordinates, as indicated in figure 13. In the neighborhood of the origin, where terms of higher than second degree are negligible, (34) reduces simply to (-^ = constant (35) P~ _ . fAC\ J-tr V TJ"V~ ^ V*Q) and, if Xz is sufficiently large, the projection of the integral curves upon the XiX plane will slope upward from left to right in the positive quadrant. Such an integral curve may therefore cut through the X%X3 plane, that is to say, the species Si may be reduced to zero. Similarly, near the axis of Xi _J = ! r J. (47) j~Y V K'Tf J ^ tt-A. 2 "- 2 ^Vwti. I ~~" ti2 and hence an integral curve may cut through the XsXi, plane, thus reducing X3 to zero. This observation is of practical interest. It has been pointed out that in sea fisheries the accompanying presence of a common fish may cause the extermination of a rarer species which, were it present alone, would be protected by its very scarcity, since this would make fishing unprofitable. But the more abundant fish continues to render a balance of profit from the trawling operations, and thus the rarer species, so long as any of it remains, is gathered in with the same net that is cast primarily for common species. Replaceable and Irreplaceable or Indispensable Components. The last two examples present an illustration of a point which calls for brief comment. So long as the species Sz has only one source jy of food, Si} it is to be observed that becomes negative as soon dt 98 ELEMENTS OF PHYSICAL BIOLOGY as Xi is zero (see equation 40). In this sense Si is an essential component of the system, relatively to S, i.e., it is indispensable for the growth and even the mere continued existence of S. On the other hand, when two or more sources, such as Si and Ss are provided, the vanishing of either Xi or Xs singly does not bring j~y~ with it a negative value of . The components Si and $3 can more or less effectively replace, act as substitutes for, each other. When the feeding species ($2 in the example) is the human species, the facts indicated above find their expression in economic terms. It is an elementary fact of common knowledge that among the varied materials which the human race requires for its growth and sustenance are many that are more or less readily interchangeable. So, for example, a deficiency in the wheat crop may be in some degree met by increased supply of potatoes or other starchy food; or a deficiency in beef may be compensated by increased production in pork. On the other hand, there are certain requisites that are irreplaceable, and therefore absolutely essential. The most obvious example of such is our supply of oxygen. In terms of our general analysis these facts would be expressed somewhat as follows. If we survey the various components whose masses Xi,Xz . . . Xn appear in the function FI = Fi (Xi, Xa, . . . -X"n) at we may effect a classification by first of all dividing them into two classes, namely those that adversely affect the rate of growth of Xi, that is to say, those for which JL^< O dZj dt and those that promote the rate of growth of Xi, those for which dt Among the latter components, those favorable to the growth of X{, there is a special class distinguished by the following property : If X is the mass of a component of this special class, then dXi . ~j7 is invariably negative as soon as X^ is zero, no matter what FUNDAMENTAL EQUATIONS OP KINETICS ~ 97 may be the masses Xi, X , . . of the other components. Xk is indispensable for the growth and the sustenance of Xi] X& is an essential of irreplaceable component, relatively to Xi. The ground upon which we are here treading is evidently close to the biological basis of economics. A detailed analysis of -the relations involved belongs to the domain of the dynamics of lifebearing systems, and will in due course be considered in its natural place. Limiting Factors. In general the several components that promote the growth of the component of Si will be presented in varied abundance. If one essential component (or a group of components which jointly are essential) is presented in limited amount, any moderate increase or decrease in the ample supply of the other components will have little or no observable influence upon the rate" of growth Fi of Si. An essential component presented in limited supply thus acts as a check or brake, as a limiting factor, upon the growth of Si. The significance of such limiting factors seems to have been first pointed out by J. Liebig: 11 "Der Ertrag (des Bodens) ist von dem im minima in ihm enthaltenen Nahrstoff abhangig." And again : Fur die Wiederherstellung der Ertrage der durch die Cultur erschopften Felder durch Stallmistdiinguug ist die Zufuhr von alien den Nahrstoffen welche das Feld im tJberschuss enthalt, vollkommen gleichgiiltig, und es wirken nur diejenigen Bestandteile desselben gtinstig, durch. welche ein im Boden enstandener Mangel an einem oder zwei Nahrstoffen beseitigt wird. Limiting factors not only set certain bounds to the growth of the components to which they are thus related, but are competent also to give rise to the phenomenon of "moving equilibrium" the discussion of which is reserved for a later section dealing with equilibria generally, under the heading of Statics. This chapter may fittingly be concluded with table 6, which exhibits the principal modes of interdependence of biological species, and summarizes the analytical characters of these, as discussed above. 11 J. Liebig, Die Chemie in ihrer Anwendung auf Agricultur, 1876, p. 334. See also ibid., pp. 332, 333, 381, 382. O O Q! S s - i - .S ic "x ^ 'S H s ? -p S -^ H C S2 ,? Q -C T3 -J g ft _ -i-i .9 .2 T': .2 S v= ^3 > '42 Ml o a T3 g fcO - " HI as 'S -*S 1 S> & &o CQ L.2 ^' W cu 6 fl ^ ^3 tb ' ft CO fl 5,'x 53 r-s i o , 03 O L.g ^ a L-i c3 Pn 99 CHAPTER IX ANALYSIS OF THE GROWTH FUNCTION Elegant intellects which despise the theory of quantity are but half developed. A. N. Whitehead. The Form of the Growth Function F. The fundamental equations (1) of Chapter VI express in a very general, and for that reason somewhat colorless way, the interdependence of the several components of evolving systems of the kind here under discussion. * In the special cases with one, two and three dependent varial^teg that have been presented as examples, the particular form affif the ^&^ concrete meaning of the functions F appearing in these equations -* has been illustrated for these specific instances, without any attempt at systematization from a general standpoint. It is desirable now to make a somewhat detailed analysis of the functions F in their more general aspect. A natural step to take is, first of all, to split up the function F into a positive and a negative term; that is to say, to express the rate of increase of the mass Xi of the component & as the balance, the surplus, of the mass Ui added to that component per unit of time, over the mass Vi eliminated therefrom per unit of time. Thus dXi -~rt .i\-rt (i) Growth of Aggregates. Among the components of systems of the kind in which we are here mainly interested, a particularly important type are those built up of a large number of essentially similar units or individuals. Such are the aggregates of molecules that constitute the components (chemical elements and compounds) of the systems with which physical chemistry is concerned; such, also, are the aggregates of individual organisms that constitute the biological species, the component population groups, of which are built up the systems in which organic evolution takes its course. In the case of an aggregate of this kind, if N is the number of individuals, and m their average mass per head, we have 100 ANALYSIS OF GROWTH FUNCTION 101 Xi = miNi (2) dXi dNi dnii . . = mi + Nl - (3) If the average mass per individual, nii, is constant, the second term of the right hand member in (8) drops out, and we have simply, This holds strictly for aggregates of similar molecules, for example, whose masses are all equal and constant. It will often hold with close approximation (as will be set forth in greater detail shortly) for populations of living organisms of one species. dNi Now -J7 1 the rate of increase in numbers of the aggregate Si, naturally appears, after the manner indicated above, as the balance of the number of newly formed individuals Bi per unit of time, and the number Di eliminated per unit of time. When these symbols refer to a population of living organism, Bi is the (total) birth rate and Di the (total) death rate per unit of time. We have, then, f-^-A (5) at which it is often convenient to write at the lower case letters &, d denoting birth rate and death rate per head per unit of time. Combining (4) and (5) we have ^-(Ifc-DOmi (7) at Demographic Functions. The quantities B, D, or 6, d lend themselves to further analysis in terms of more fundamental characteristics of the aggregate. In a qualitative way everyone is familiar with the manner of the elimination of individuals from a population by death: some are carried off in infancy, some in child- 102 ELEMENTS OF PHYSICAL BIOLOGY hood, adolescence, and maturity, until the remnant is finally called in old age. Quantitatively this fact finds expression in an actuarian's life table, or the corresponding life curve, of which some examples are shown in figures 15 to 17. Starting with some large number,, say a million, of newly born individuals, counted at birth, if we follow this sample batch of population through life, we find them thinning out, at first rather rapidly in infancy and childhood (steep part of curve on left) : then more slowly (more gentle slope) in mid-life; and faster again as the natural term is approached. At any particular age a there are thus left, out of the original batch, a fraction p(a) of survivors. The fraction p(a), which we may speak of as the survival factor, 1 is a measure of the probability, at birth, that a random individual of the batch shall reach age a, under the conditions under which the data assembled in the life table were collected. The value of p(a) for every age of life depends, of course^" on the general conditions of life in the population. It therefore varies in different localities and at different epochs, as illustrated in figures 15, 16, 17. When it is desired to bring out the fact that p(a) depends on the time, it may be written p(a, f). But as a rule the change with time is not very rapid and we may often consider p(a) as a function of the age a alone. We shall do this in the present analysis^ which relates to a population in a selected locality under essentially constant conditions of life. If we denote by Na the survivors to age a, out of an original batch Ar counted at birth, we have JV = N p(a) (8) We will -write dNa /1A\ \LO)' or dNa d > r , j Nada da The coefficient jua thus defined is termed the force of mortality at age a. From its definition it is clear that it measures the death rate per head in a population composed entirely of individuals of age a. 1 The function p (a) is that commonly denoted by lx in actuarial notation, p.nd tabulated in the principal column of a "Life Table," SSfSS] \ \ \ \ \ \ \ s.ooo 70,000 64,000 FIG. 15. SOME HISTORICAL HUMAN SURVIVAL CURVES, EXHIBITING AN EVOLUTIONARY TREND TOWARD LONGBB AVERAGE DURATION OF LIFE The improvement is probably rather one of general hygiene than of man's physiological constitution. The earlier figures are of very doubtful accuracy. 103 104 ELEMENTS OF PHYSICAL BIOLOGY AGE IN YEARS 65,000 -45,000 40,000 35,000 30,000 25,000 20/500 15,000 IO.OOO. 5.000 x: X 4\ \ il 60 70 ASE IN YEARS 30,000 25,000 2O.OOO I5.OOO FIG. 16. STJEVIVAI, CUEVES FOB THE STATE OF MASSACHUSETTS, FOB THE THBEE DECADES 1890-1900-1910. AFTEB GLOYEB The data on -which these curves are based are naturally more reliable than those of the older life tables shown in figure 14, and exhibit very clearly the upward trend of the average length of human life in recent decades. ANALYSIS OF GROWTH FUNCTION 105 AEE M YEAJIS FIG. 17. SURVIVAL CURVES FOE DIFFERENT COUNTRIES, SHOWING INFLUENCE OP LOCAL CONDITIONS UPON LENGTH OF HUMAN LIFE. AFTER GLOVER A particularly simple case is that in which \ia is independent of a, the force of mortality is independent of the age, or is the same at all ages, We then have by integration of (10) and p(a) (11) (12) 106 ELEMENTS OF PHYSICAL BIOLOGY Such a simple life curve as this is not to be expected in a species of living organisms. It implies that the individual does not age, that his chance of living another year is just as good at ninety years of age as at fifty or at ten or at five; he can die, as it were, only by accident; he is perpetually young. Survival curves of this form do occur and play a significant role in the aggregates of atoms and molecules which the chemist and the physicist make it their province to study. The atoms of an element in radioactive transformation, for example, are picked off, one by one, according to a law of this form, and so are the molecules of a chemical compound decomposing by a monomolecular reaction. If, in such a case, the plot the function p(a) is drawn on logarithmic paper, evidently a straight line is obtained, since logep(a) = jua (13) (14) da The force of mortality is here seen as the (constant) slope of the curve representing loge p(a). In the more general case it is also often convenient to plot p(a) on a logarithmic scale. This has been done in figure 18 for the United States survival curve shown in figure 17. It is seen that the curve thus obtained is at first convex toward the axis of a, but soon becomes concave toward that axis and then remains so to the end. The significance of this is, of course, that the force of mortality is very high in infancy, decreases in early childhood, until it reaches a minimum about the twelfth year of life; and finally increases continually to the end of the life span. The detailed analysis of the human survival curve is a matter of interest not only to the student of evolution, but also to the guardian of public health and to the insurer of human life, the actuarian. The essentially practical requirements of these has led to a highly developed technique, amounting virtuaUy to a separate branch of science, in the preparation and analysis of life tables. Of this phase of the subject no more needs to be said here, since there is a voluminous special literature available. Only the more strictly biological aspect of the matter is for us here of immediate interest, and of this more will be said later, in discussing the physical basis underlying the survival curve. ANALYSIS OF GROWTH FUNCTION 107 Survival Curve Data. Without having recourse to any refinements of mathematical analysis it is clear that a close relation exists between the survival curve of a given species and its rate of increase, its fate in the straggle for existence and for dominance. It might 10,000 /o K O -? 8 IS. 16 SO & S3 X 36 -fO 44 -fff .52 S6 60 64 68 7S 76 80 ff* 88 9 -36 /OO Ag stable> in the sense that, if disturbed by a temporary changem the conditions of life (e.g., war), it will spontaneously return uponrestoration of normal conditions. 112 ELEMENTS OF PHYSICAL BIOLOGY A rigorous proof of this stability of the age distribution (23) cannot be briefly given, and for details of such proof the reader must be referred to the author's publications in the journal literature.8 The general character of the proof may, however, be indicated. If the original population has any arbitrary age distribution, such as that represented by the more heavily drawn curve in figure 20 by judicious trimming we could reduce the population to the normal distribution represented by the lower curve tangent to the heavy curve; or, we could, by filling in gaps, supplement the population to fit the upper tangent normal distribution curve. The trimmed down population, having the normal age distribution, would always retain it. The same is true of the supplemented population. The actual population will therefore always lie between the trimmed and the supplemented. Moreover, it can be shown that at intervals of about one hundred years (the span of life) new tangent curves can be drawn to the actual distribution curve, the new tangents lying between the old. Thus the two tangent curves ultimately approach until they coincide, and then, necessarily, the actual distribution curve lying between them coincides with them also. That is to say, the actual conforms with the normal age distribution.7 It must be understood that the normal or stable form of age distribution represents merely a broad type, toward which actual age distributions will tend. However, the approach seems to be at times very close, as is shown by the figures in table 7 giving the observed and the calculated age distribution for England and Wales in decennium 1871-1880. A graphic representation appears in figure 21, which shows the observational data, plotted (in dotted lines) as a stepped curve. The corresponding figures calculated by the formula (13) are plotted in two ways, namely, first as a stepped curve (drawn in full), for comparison with the observational data; and also as a continuous curve. The latter brings out a feature that may be noted in passing, namely the fact that the curve of age distribution is very flat, roughly linear, over a wide range, from the 7 An exceedingly interesting effort of early date to demonstrate the ultimate approach to geometric increase of the birthrate, independently of initial conditions (e.g. starting with a single pair of parents) is to be found in L. Euler, Recherches g6n a = age, FIG. 21. "STABLE" AGE DISTRIBUTION, AS EXEMPLIFIED BY THE POPULATION OF ENGLAND AND WALES IN THE DECADE 1871-1880 I IK ANALYSIS OF GHOWTH FUNCTION 1JLtJ fifth to the eightieth year of life. 5 This, of course, is a special feature of a human population when the natural rate of increase r lies in the neighborhood of a certain value. Minor fluctuations of the age distribution will not greatly affect the birth rate and the death rate. Since actual populations approximate the normal age distribution, i.e., that defined by equation (23), it seems permissible and it is certainly expedient to assume, in further discussion, that the normal age distribution is actually established; we may then virtually disregard the influence of the age distribution upon the rate of increase of the component. This element is, as it were, automatically ruled out of further discussion, by the natural establishment of the normal age distribution; 9 a circumstance which is in so far fortunate, as we are here interested in the relation of the rate of growth to the more fundamental biological characteristics; the age-distribution appearing merely as an adventitious element complicating the relation, without being essential to the fundamental characterization of the species. Demographic Relations in "Normal" Population, It is worth while to note briefly in passing that in the case of a population in normal age distribution, many demographic relations assume a simple form. So, for example, the relation between birth rate per head 6 and death rate per head d is here given by the formula10 1/b = g-rp( ) d (25) Jo which, to second order approximation, is reducible to the simple form 1 - U U____ + j=*L (26) where L is the mean length of life, defined as Compare J. Brownlee, The Use of Death Rates as a Measure of Hygienic Conditions, Report to Medical Research Council, London, 1922, pp 36-378 Of. G. Eijkman, Onthr " J.--.-TTI .. .. ~ . >j.r!, p. 269; 10 A. J. Lotka, Quart. Publ. Am. Statist. Assoc., 1918, p. 121; 1921, p. 998. 116 ELEMENTS OF PHYSICAL BIOLOGY Ceo p(a) da (27) while U is defined11 by /"6co L ' = ap(a) da (28) i)mi (3) at Aggregates of Variable Units. For aggregates of living organisms we can also write an equation identical in form with (3), as has already been noted in Chapter IX; Bi is in this case the total birth rate, DI the total death rate, and m^ the average mass per head of the living population. But this is an inadequate representation of the significant facts. The equation, thus written, glosses over certain important characteristics of living organisms. Unlike molecules in a system in the course of chemical transformation, each unit in an aggregate of living organisms does not retain its substance unchanged in identity or in total mass. In fact, each unit is itself an aggregate within the larger aggregate that constitutes the species or biological group, and for each individual unit (organism) separately we can write an equation analogous to equation (1) of Chapter IX where U'i is the total mass taken up (ingested) per unit of time by the unit organism, and Vi is the total mass eliminated therefrom per unit of time. So, for example, in the course of one year a boy ten years old and weighing 32.5 kgm. may consume about 600 kgm. of food (inclusive of water and oxygen), may eliminate about 599 kgm of wastes, and will grow in actual mass by about 1 kgm., so that we have ~ = 600 - 599 = 1 = O.OSmi (5) at The Stream of Substance Through, the Form of the Organism. It will be observed that a portion of the intake, but a portion only, is expended in adding to the total mass of the unit. The remainder ANALYSIS OF GROWTH FUNCTION 131 B,-17',-^ (6) at is expended without, apparently, 1 any resulting increase in the total mass of the unit. This constant expenditure of substance, and the equally constant intake required to balance it, is a fundamental characteristic of the units here under discussion. In the adult, whose mass is (on an average) approximately constant, we have simply and the entire intake goes to meet the requirements of maintaining the mass of the unit at constant level. 2 Turning now from the consideration of the individual unit to that of the aggregate of N such units, evidently, if the average intake per unit of time per individual is U'i, and if the average elimination is Vi, then we shall have for the rate of increase of the total mass Xi of the aggregate. cLTi _= NU'i- NV'i - Nm'idi (9) at where di is the death rate per head per unit of time and m'i is the average mass of a unit (organism) at death. Two Types of Organisms: Economical and Lavish Birth Rate. The relative importance of the second and the third term in the right hand member of the equation (9) differs greatly in different biological species. At the one extreme we have a type of which perhaps the most characteristic representative is man. With a mean length of life of about fifty years, his body must be replaced about twice in a century to maintain the population equilibrium. If we assume (as a rough but sufficient approximation) that the average weight of man at death is 50 kgm., this means that the third term, 1 Indirectly a part of the excess Ri of the mass intake over the mass increase may contribute to that increase, namely by furnishing some of the energy required for anabolism. But we are here discussing mass relations only. The energy relations are reserved for separate consideration later. Except during gestation, if the mass of the fetus is reckoned in with that of the mother. 132 ELEMENTS OF PHYSICAL BIOLOGY vy 50 in a stationary population, is about ^p kgrn. for the entire popu- ou lation, or just about 1 kgm., or say 2 pounds per head per annum. To put it crudely, of the food consumed by each human individual in a year, 2 pounds go, on an average, to replace the bodies of his fellows departed that year. This, it will be seen, is an insignificant, almost wholly negligible fraction of the 1000 pounds 3 or more than he consumes, in all, in a year. Of the total food consumed by the human race, then, about 0.2 per cent3 goes to replace the bodies eliminated by death. The remainder is for current maintenance of the living. And the total food consumption 3 may be of the order of 7 to 10 times the mass of the population per annum.4 But, as already stated, man represents an extreme type, the extreme economy of life, with low death rate and correspondingly low birth rate. Of the opposite extreme, lavish, seemingly wasteful extravagance, examples are exceedingly common, though it may not be easy to give full quantitative detail. Among the most wasteful breeders are, no doubt many aquatic species, including fish, since their young are ill protected and become ready victims of other species. So a ling weighing 54 pounds was found to be carrying twenty-eight million eggs. 5 An oyster may have sixty million eggs. But some familiar land animals are prolific enough, even if they do fall far behind the standards just exemplified. The brown rat may have five or six litters averaging about eight or ten each, in a year. 6 Domestic Animals Kept for Produce. Accurate figures can be obtained in case of domestic animals. While these do not represent so extreme an example, a special interest attaches to them owing to their direct relation to human food economics. The most prolific among domestic animals is the pig. In reasonably good farm conditions a sow should average three litters in two years, each of seven farrows, of which five are successfully raised and marketed. Even with the high mortality artificially induced by man in his domestic stock the item of running expenditure in feed for mere maintenance is far in excess of the replacement cost, that is to say, the feed 3 Exclusive of oxygen. 4 For quantitative data on growth in man see C. S. Minot, The Problem of Age, Growth and Death. 6 J. A. Thomson, The Wonders of Life, 1914, p. 130. s H. H. Donaldson, The Rat, 1915, p. 190. ANALYSIS OF GROWTH FUNCTION 133 stored up and finally utilized in the carcass of the slaughtered animal. From a detailed study of the vital economics of beef production made at the University of Missouri7 figure 20 is reproduced here to show these relations. The convex curve shows the average growth per head in a group of steers fed with a ration regulated to secure a maxi- MOOO /DO SOO 30O -90O 00 600 700 goo SCO /OOO //OO /200 t30O HOO OOO FIG. 26. FEED CONSUMED, AND INCREASE IN LIVE WEIGHT OF STEERS AT SEVERAL AGES Dry matter consumed is represented on one-tenth the scale of the live weight. After Moulton, Trowbridge and Haigh. mum of growth, without storage of surplus fat; the approximately straight line mounting upward shows the steadily increasing integrated amount of feed consumed since birth. Only the dry weight of the feed is plotted, and the scale employed is ten times more 7 University of Missouri, College of Agriculture, Bulletins 43, 54, 55 (E. C. Trowbridge and L. D. Haigh). 134 ELEMENTS OP PHYSICAL BIOLOGY condensed than that used for the live weight else the second would rise too steeply as to lie for the most part far beyond the HnvT of the page. Thus is shown the great disproportion between the feed TABLE 9 Average Yearly Gains of Steers* Srowth not body of the growing steer- and ceraM ; ' S &r M the interest of the P^uoer is concerned, in mere mamtenance, for the private satisfaction and benefit ANALYSIS OF GROWTH FUNCTION 135 of the animal, so to speak. The numerical data on which figure 26 is based are exhibited in table 9, together with the corresponding figures observed when the animals are somewhat underfed and overfed respectively. The instances that have been cited man on the one hand, and the highly prolific species, both feral and captive, on the other are eloquent illustrations of the elasticity of adaptation. Clearly, a species may hold its own, in the straggle for existence, either by the aid of well-developed protective devices resulting in a low death, rate, and requiring only a correspondingly low birth rate; or, a less well protected species may balance a high death rate by an equally high birth rate. Which of these two methods would be chosen in the natural course of events is a question that it might be difficult to answer on any general a priori principle, so long as attention remained fixed on a single species. Perhaps one would have expected evolution to turn in a favor of the more economical method of meeting a low death rate with a low birth rate. In point of fact both types of organism the economical type (as judged by its own standard) with low death rate, and the wasteful with high death rate exist side by side in abundance. This is a good example to illustrate the purely relative character of fitness, and to remind us once more that we cannot expect any success in attempts to define the direction of evolution in terms of a single species. It is not the individual species, the individual components of the system, that evolve, but the system as a whole, comprising all the species and their environment. The species of the economical type, with low death rate, are largely dependent for their subsistence on the presence of species of the opposite type; we must think here of a competition, not between individual species, but between groups of species, groups consisting, in the simplest case, of two species each, a food species or prey, and a feeding or predatory species. Of two such groups, that one will, other things equal, have the advantage in the struggle, in which high productivity of the food species is accompanied by economy of life on the part of the feeding species. From the point of view of the hog, so to speak, the high mortality in the pen is a disastrous inefficiency and maladaptation, a misfortune to be borne, as best it may, with porcine philosophy 1 . From the point of view of the consumer on the other hand, this high mortality is, quite on the contrary, a measure of the efficiency, the eminent fitness of swine as producers of pork; and his only regret 136 ELEMENTS OF PHYSICAL BIOLOGY is that so much of the feed placed in the trough goes merely to carry on "what may be called the personal activities of the animals themselves." 8 It is to be noted, however, that only a part of the material accountable as waste from the standpoint of the food species is gain for the feeding species. Deaths from disease are a pure loss to both species. Similar reflections, of course, apply, mutatis mutandis, to those cases in which the feeding species derives its nourishment from some current product of the life activity of the food species or host, instead of from its carcass. The most notable example of this in the food economy of man is his exploitation of the milch cow, who is a far more efficient producer than the beef steer. The latter at best consumes over 6 pounds of nutriment for every pound of product. 9 According to the investigations of the National Research Council about 18 per cent of the energy of grain fed to cattle is recovered for human consumption in milk, but only about 3.5 per cent in beef. Similarly, crops on a given area will yield about four to five times as much protein and energy when fed to dahy COWT S as when used for beef production. In providing mineral substances and vitamines the milk of cows contrasts even more favorably with the beef animal. The vitamines and calcium salts contained in hay and grain are stored in the muscular tissue only to a slight extent, but are in relative abundance in milk.10 From the standpoint of the dairyman a thoroughbred prize cow, such as Glista Ernestine (a Holstein), which gave in one year 833 pounds of butter fat, and in one hundred days 10,000 pounds of milk, is a very model of efficiency, producing more than her own weight in milk each month. But from the point of view of the bovine species such record performances are gross inefficiency, approaching in some cases perilously near to total biological unfitness, for some of the record Jersey cows are probably unable, under the conditions of the stable at any rate, to raise their own calves the over-rich milk would probably kill the young animal. Network of Chains of Interrelated Species. The relation between man and the domesticated species of animals and plants on which he 8 I have here borrowed a felicitous phrase from an anonymous writer on the editorial page of the New York Times, February 10, 1921. 9 University of Minnesota, Agr. Exp. Station Bulletin 193, pp. 68, 69 (T. L. Haecker). 10 Jour. Franklin Inst., vol. 190, 1920, p. 155. ANALYSIS OF GROWTH FUNCTION 137 EO largely depends for food, in the present state of civilization, is only a particularly tangible, a particularly accessible example of an intricate network of relationships that connect more or less closely all living species. In this network each species or component is interlaced, like a link in a meshed coat of mail, with other species, which in turn connect with still others, and so forth. In our effort to get some sort of mental grasp of the complicated interlocking of these elements we seize upon some one link, some one species or component, and we note, first of all, that whatever is eliminated from one component of a self-contained system must pass into one or more other components of the system. So, for example, the component Si may be a herd of cattle. The matter eliminated from this component goes in part as food to build up or sustain a human population; in part it goes as fertilizer on the fields to furnish nutriment for crops; still other parts are worked up into various industrial products, such as leather, glue, etc. We thus have, in schematic representation, Cattle \ Human population \ Leather s SS Fertilizer L \ \ sk On the other hand, the substance of the herd itself is recruited from certain other components of the system, grass, clover, corn, etc., so that we may further develop the scheme Clover Grass \ Corn / \ Cattle \ Human population \\ Leather \N Fertilizer Transformation Factors and Their Economic Significance. In general any one component thus appears as a link in a complicated chain or rather network of chains; the component St , for example 138 ELEMENTS OP PHYSICAL BIOLOGY receives a certain fraction at, i of the mass VtXt eliminated per unit of time from the component St', it passes on to the component S& a certain fraction ik of the mass ViXi eliminated from Xi itself. /l~y The rate of growth n2 of Xi is the balance of the sum Ui of all contributions it receives over and above the sum V\ of all the contributions which it makes to other components, thus dXi = mXi - viXi = Ui - Vi (10) at = ZatiVtXi - S/3iki>iXi (11) the first summation being extended over all those components St which contribute to Xi and the second over all those components 8k to which Si contributes. But we may also analyse the contributions to and from the component Si in another way. We may say that, of the total contributions per unit of time UiXi to the mass Xi, a certain fraction yuUiXi is derived from Sf. Then (12) = vfXf (13) 7it and, substituting (13) in (10), Lastly, if the system is not self-contained, we must add a term Ji for "imports" per unit of time, and a term EI for "exports" per unit of time, that is to say, -^ = vtXf - ViXi + Ii-Ei (15) dt 7n When Si is the human species, the coefficients a, jS, 7 have an obvious economic significance. The restriction of this remark to the human species must not be taken to imply that there is in this feature something wholly peculiar to man, but rather, that underlying our economic manifestations are biological phenomena which we share in common with other species; and that the laying bare and clearly formulating ANALYSIS OF GROWTH FUNCTION 139 of the relations thus involved In other words, the analysis of the biophysical foundations of economics is one of the problems coming \ within the program of physical biology. Hints as to the direction in which we may or must look for light on this phase of our problem have now been noted upon several occasions. So it was observed that the components of a life-bearing system can be divided into two classes, relative to the component Si, namely, on the one hand those components S-} for which -^ ~^T was positive, or, as we may say, those useful to the species Si, those having for it a positive value, and. on the other hand, components 8% for which ^ 3i l <0, comV.A ic at ponents harmful to Si, or having for it a negative value. Elsewhere we have noted the classification of components into replace, able and indispensable components, a classification that at once recalls elementary economic reflections. These hints we note in passing. They may serve to put our minds in a state of preparedness for the more formal and decisive attack of the problem, to which we shall be led in the last division of our enquiry, dealing with the dynamics of life-bearing systems. Jf STATICS CHAPTER XI GENERAL PRINCIPLES OF EQUILIBRIUM Repeatedly, in preceding chapters, occasion has arisen to refer to stationary states or equilibria. Inevitably, in the discussion of the kinetics of evolution, one is led to consider incidentally certain conditions and special cases in which the velocities of the changes in the evolving system are zero; when, that is to say, the system under discussion is in a steady or stationary state, in equilibrium. Viewed from this avenue of approach equilibrium presents itself as a special case of motion or change, namely motion or change with zero velocity. Indeed, something very like equilibrium occurs also with velocities that are merely small, not vanishingly small. In such case the phenomenon of moving equilibrium may present itself, as we shall have occasion to observe in greater detail in due course. Stationary states equilibria and near-equilibria play an important role in nature, and it is desirable at this point to give them something more than incidental consideration; to sketch, at least in outline, their systematic study; to stake out, in the rough, that field which, in our survey of the Program of Physical Biology (Chapter V) was designated as the Statics of Evolution, and was systematized according to the schedule Statics "I Equilibria Moving equilibria Displacement of (steady states) equilibrium It will be convenient, in the development of the subject, to follow, in the main, the schedule thus set forth. Kinetic, Dynamic, and Energetic Conceptions of Equilbrium. While we shall, in this section, conceive a stationaiy state from the standpoint of kinetics, defining it as a state in which certain velocities vanish, it must be noted that there are also other conceptions of equilibrium. Etymologically the word equilibrium is tied, in stricter usage, to a dynamic conception: Aequa libra, the poised balance, is symbolic of a state in which forces are balanced, in which the resultant force vanishes, 143 144 ELEMENTS OF PHYSICAL BIOLOGY A third conception of equilibrium, differing from the second, the dynamic, only in point of view, not in scope, is derived from a consideration of energy relations. A system in dynamic equilibrium is found to be characterized by the attainment of a minimum (or sometimes a maximum) of certain functions having the dimensions of energy; a state in which the virtual work done in any very small displacement compatible with the constraints vanishes.1 So, for example, a ball placed hi a hemispherical cup, is in equilibrium when its potential energy is a minimum compatible with the geometry of the system. More generally, equilibrium is, according to this view, defined as a state in which certain potentials have a minimum (or a maximum). Pedantic usage would demand that the term equilibrium be reserved for states satisfying the dynamic and energetic conditions of rest or invariability in time. It would deny the appellation equilibrium to certain states commonly so designated. Metabolic equilibrium, population equilibrium, and the like, are not true equilibria, in this narrower sense, but are steady states maintained with a constant expenditure, a constant dissipation, of energy. It is not necessary, however, at present, to lay any stress on this distinction. The occasional use of the word equilibrium in speaking of what is merely a steady state maintained with a continuous expenditure of free energy is not likely to cause any serious confusion; and we may as well take the usual liberties in the matter, whenever this course is dictated by convenience and does not offend against essential principles. Where express distinction becomes necessary, we may speak in specific terms of true equilibrium and quasi-equilibrium, respectively, to denote the two separate types included hi the generic term "stationary state" or "steady state." A complete treatment of the entire field of the statics of evolving systems should, to be entirely systematic, cover both types of stationary states. There are, however, two reasons for departing somewhat from such strictly systematic arrangement. The first is that the statics of true equilibria have been developed to a high degree in the discipline of thermodynamics, so that an exposition of the pertinent principles and conclusions would be little more than 1 Stability of equilibrium demands, further, that the work done on the system in any small, but finite, displacement, be positive, that the potential energy be a minimum (maximum being, in this case, excluded). GENERAL PRINCIPLES OF EQUILIBRIUM 145 a transcription into these pages of what can be found abundantly set forth elsewhere in the standard literature. However much one might be tempted, in the interest of a well rounded presentation, to sketch at this point at least an outline of the relevant chapters of thermodynamics, economy of space dictates the briefer expedient of referring the reader to the existing literature, so abundant that it seems superfluous to mention titles. A second reason for passing lightly over true equilibria at this point, is that the steady states with which we are most frequently and most closely concerned in the field of organic evolution (our main topic here), are of the second class; not true, equilibria in the dynamic sense, equilibria in which all forces are balanced; but what we have termed above quasi-equilibria, states maintained constant or approximately so with a continual expenditure, a continual dissipation or degradation of available energy. To such as these we shall give our chief attention, though in part our discussion will be framed broadly to cover indifferently either type of steady state. For the sake of example, too, reference will be made, on occasion, to systems evolving toward a true equilibrium; systems for which the law of evolution is capable of direct expression In comparatively simple thermodynamical terms; systems which, by that very fact, are peculiarly adapted to serve as paradigms exhibiting the characteristic form of a law of evolution. General Equilibrium Condition. As has already been noted incidentally, the general condition for equilibrium, or, to be more precise, for a stationary state, is obtained by equating to zero the velocity of growth of each component of the system, thus = Fi(Xi, Xz, . . . Xn) (1) at F! = Fz = . . . = Fn = (2) This condition, in general, furnishes n independent equations, which determine one or more sets of values of the variables X, thus Xz ~ * ' (3) 146 ELEMENTS OP PHYSICAL BIOLOGY If the values C thus determined are real and positive 2 they evidently define an equilibrium or a steady state, the character (stability mode of approach) of which depends upon the nature of the roots X of a certain characteristic equation, as has been indicated on an earlier occasion. Different Types of Equilibrium. Graphic Representation. A particularly graphic representation of the different types of equilibrium is obtained if, instead of seeking solutions of the fundamental equations (1) expressing Xi, X2 . . . Xn in terms of t, we on the contrary eliminate t from this system of equations. This is very readily effected by division, which leads to the new system dXi dXz dXn T! = ~F~* = ' ' ' " 71 (4) This system of equations defines a family of curves passing through the equilibrium points, which here appear as singular points. The situation is particularly transparent in the case of two variables Xi, X2, since this readily permits of plotting the integral curves in rectangular coordinates in the plane of the paper. We have already had occasion incidentally to employ this method of treatment in an example in Chapter VIII, in which the conflict between a host species and a parasite species was examined analytically. Without going into extensive technical details it is advisable now at least to enumerate and briefly describe the several types of equilibria and the topography, characteristic of each type, presented by the integral curves in and about a singular point. These types are somewhat numerous, even if we restrict ourselves to the case of two variables, and brevity is therefore imperative. Type 1. Roots Xi and X2 real and negative. Equilibrium is stable; integral curves run directly into singular point as in figure 27, A. Type 2. Roots Xi and X2 real and positive. The topography is similar to that of type 1, but integral curves are traversed outward from singular point. Unstable equilibrium, figure 27, B. Type 3. Roots Xi and X2 real and of opposite sign. Integral curves in general do not pass through singular points, but curve away from it. Unstable equilibrium, figure 27, C. 2 Masses cannot assume negative or imaginary values. Hence negative roots may fail to define equilibria; a similar statement holds regarding complex roots. GENERAL PKDSTCIPLES OF EQUILIBRIUM 147 Type 4. Roots Xi and X2 complex, real parts negative. The integral curves are spirals winding into the origin, forever approaching it without ever reaching it. Stable equilibrium, figure 27, D, Type 5. Boots Xi and X2 complex, real parts positive. The topography is similar to that of type 4, but integral curves are traversed outward from singular point. Unstable equilibrium, figure 27, E. Type 6. Roots Xi and X pure imaginaries. This gives rise to several distinct subtypes. Subtype F. Integral curves are closed loops enclosing the origin. Process is purely periodic. Figure 27, F. Subtype G. Integral curves are spirals winding inward. Stable equilibrium. This is the case treated in Chapter VIII, where a representative diagram will be found. Figure 27, G. Another subtype is similar to G but spiral winds outward. Unstable equilibrium. Subtype H. Integral curves are spirals winding about a closed loop. Types I AND J occur when \i = X2 . Figure 27, 1, J. As an example illustrating the occurrence of two types of equilibrium, two types of singular points, the topographic chart of the integral curves defined by the Ross equations for the spread of malaria under certain conditions is shown in figure 28. It will be seen that there are two singular points, one at the origin 0, unstable, of type C; the other at T, stable, of type A. This chart obviously suggests "stream lines" and a three dimensional model. Such a model (purely qualitative) is shown in figure 29. The feature of interest is that a singular point like 0, of type C, is represented by a col ("notch") in the landscape; whereas the stable equilibrium of type A is represented by a pit, as at the point T. While this model refers to a very particular case, it serves to bring out a noteworthy fact, namely, that there are necessarily certain regularities in the occurrence of the various types of equilibria. So, for example, it is clear that two pits of the character of the point T cannot occur without some other type of singular point between them, just as it is physically impossible for two mountains to rise from a landscape without some kind of a valley between. For a detailed study of this phase of the subject the reader must be referred to the mathematical literature. 3 3 For further discussion of the various types of singular points that may occur the reader is referred to the mathematical literature, of which the following may be mentioned: E. Picard, Trait<5 d'Analyse, 1891, vol. 1, pp. 83, 123; 1893, vol. 2, pp. 183, 193, 196 (footnote); 1896, vol. 3, pp. 228, 238; v. Dyk, Sitzungsber Bayer. Akad. Wissensch. Miinchen, March 6, 1909,^AbhandL 15; Abhandlungen derKgl. Bayer. Akad. Wissensch., March, 1913, vol. 26,Abhandl. 10; Sitzungsber, 1891, p. 23; 1892, p. 101; H. Liebmann, Lehrbuch der Differential gleichungen, 1901, pp. 101, 102, 134. ELEMENTS OF PHYSICAL BIOLOGY FIG. 27. SOME FUNDAMENTAL TYPES OP EQUILIBRIUM, IN A SYSTEM WITH Two DEPENDENT VAEIABLES GENERAL PRINCIPLES OF EQUILIBRIUM 149 FIG. 28. MAP OF INTEGRAL CURVES FOR THE Ross MALARIA EQUATIONS, AS AN EXAMPLE EXHIBITING Two SINGULAR POINTS, OP TYPE 1 AND 3 (SEE FIGURE 27, A AND C) The heavy lines are integral curves; the lighter lines are auxiliaries (isoclines) employed in constructing the graphic solution of the differential equations. (Reproduced from A. J. Lotka, Am. Jour. Hygiene, January Supplement, 1923.) 150 ELEMENTS OP PHYSICAL BIOLOGY . ,JH'/!' <>';'' X" \' A >' " "ft *M'ft' "'" s. '"-' ; GENERAL PRINCIPLES OF EQUILIBRIUM 151 Metastable Equilibrium. The graphic representations of the malaria equilibrium furnish the occasion for another remark of general character regarding certain equilibria. The circumstance that gives rise to the first malaria equilibrium, the one in which the malaria rate is zero, (point in figs. 28 and 29) is the autocatakinetic character of the growth, of a malaria endemic . This is a common characteristic of the growth of living systems; growth is initiated by a nucleus of the same species of matter that is added by the growth. Conversely, in the entire absence of any nucleus of a particular species of living matter, growth of that species cannot take place, even though all other conditions for such growth may be satisfied, even though the system may he, as it were, supersaturated with regard to that species of matter. In these circumstances an equilibrium may be presented which is unstable in the sense that, upon the introduction of a suitable nucleus, growth immediately sets in. 4 Equilibria of this type, which are stable in the absence of a suitable "nucleus" but in which change is immediately initiated upon introduction of such a nucleus, have been termed "metastable" equilibria. Exceptional Cases: A brief reference must suffice regarding certain exceptional cases that may arise. So it may happen tbat one of the roots X of the characteristic equation vanishes. An example of this was encountered in dealing with the Ross malaria equations. It was found that as the number of mosquitoes per head of the human population approaches a certain critical value, two singular points approach each other, and finally fuse, giving one "double" point. 5 Another special case that may arise, and whose mention must here suffice, is that of multiple roots of the characteristic equation, the case in which two or more of the roots are equal. 6 4 In inorganic systems an analogous state of affairs is observed in supersaturated solutions or vapors which, are brought to crystallization or to condensation by the introduction of a suitable nucleus. Dynamically the characteristic of a metastable equilibrium is that the thermodynamic potential of the system, though a minimum, is not an absolute minimum. 6 See A. J. Lotka, Am. Jour. Hygiene, 1923, vol. 3, January supplement, p. 12. 6 Compare H. Liebmann, loe. cit., pp. 102, 134; A. J. Lotka, Zeitschr. f. physikal. Chemie, 1912, vol. 80, p. 16. CHAPTER XII CHEMICAL EQUILIBRIUM AS AN EXAMPLE OF EVOLUTION UNDER A KNOWN LAW I wanted to remind the biologists that in the early stages of life what they are accustomed to speak of as natural selection passes over into what might be described as a mere physical selection of stabler compounds. K. Pearson. One of the simplest examples of equilibria in systems of the type that interests us here systems composed of several groups each consisting of numerous similar individuals as units is the equilibrium resulting from a pair of balanced or opposing chemical reactions. This case illustrates so well, in their simplest form, a number of typical traits of the phenomena here under discussion, that it will pay to give it brief consideration. We shall select for this purpose the simplest possible type of balanced chemical reaction at constant volume and temperature, namely a reaction which is monomolecular in both directions. A substance Si undergoes a transformation into S%, and Sz in turn is converted back into Si, one molecule alone taking part, in each case, in the transformation. If Xi and xz are the respective concentrations of Si and $2, we have, at a given temperature, by the law of mass action, the rate of decomposition of Si and Sz respectively. (Ztei) = - faxi (1) (D^) = - fax* (2) Or, since at constant volume concentrations x are proportional to numbers n of molecules (Dm) = - fciin (3) (Dnz) font (4) where fci, k2 are coefficients (functions of the temperature) characteristic of the reaction. 152 CHEMICAL BQUILIBBIUM 153 The rate of increase of the substance S is the excess of its rate of formation 6 over its rate of decomposition, in strict analogy to the birth rate and death rate in a human population (fti-fcOm (5) at (6) at In a population of living organisms the material for the formation of new individuals must ultimately be derived from the bodies of those that have died. But the connection is a complicated one involving many steps. In the population of molecules here under consideration the relation between birth rate and death rate is of the simplest possible form. Each molecule of Si that "dies" becomes a molecule of 82, and vice versa. Thus equations (5), (6) assume the form and in equilibrium , , kiUi (7) at - = kiHi ^22 (8) at K\ If we fix our attention upon HI molecules of Si at the moment of their formation, we can apply to these particular molecules the equation (3), from which we have, by integration 1 * (10) similarly for S2 = naCO)*-*** (ll) \ But 77:7 is the probability pi(a), at the moment of its formation, that a molecule of Si picked at random at such moment, will reach age o. The life curve for the molecules of Si is thus defined by Pi(a) = p. 464; F. M. Kannenstine, Astrophys. JL, 1924, vol. 59, p. 13. ^ CHEMICAL EQUILIBBIUM 157 departure and the final state remaining unchanged. For discussions of these technical details the reader must be referred to the literature, a few of the more recent publications being noted in a footnote below.6 While the details of the manner of the "birth" and "death" of the molecules in chemical transformation are, as yet beyond the range of the observation of the physicist, the fundamental laws of energetics, which hold true generally, and independently of particular features of mechanism, are competent to give substantial information as to the end product, at any rate, of the evolution of such a system as considered in the simple example above. The final equilibrium must accord, as regards its dependence on temperature, pressure and other factors, with the second law of thermodynamics, which may thus be said to function as a law of evolution for a system of this kind. This is a point worth dwelling on a little at length, inasmuch as our knowledge of the form and character of the law of evolution for this special type of system may be expected to serve as a guide in the search for the laws of evolution in the more complicated systems, belonging to an essentially different type, which confront us in the study of organic evolution. The second law of thermodynamics can be expressed in various ways, but the form in which it serves our present purpose best is that which states that the system evolves toward a state in which certain functions (thermodynamic potentials) of the variables defining its condition are at a mrnimum, somewhat as a ball placed in a hemispherical bowl ultimately comes to rest in the position in which its (gravitational) potential is a minimum, namely, at the lowest point of the bowl. Mary laws of nature are conveniently 7 expressed in this form, as minimum (or maximum) 8 Regarding the r61e played by thermal agitation and by radiation see G. W. Todd and S. P. Owen, Phil. Mag., vol. 37, 1919, p. 224; I. Langmuir, Jour. Am. Chem. Soc., 1920, vol. 42, p. 2190; W. H. Rodebush, Jour. Am. Chem. Soc., vol. 45, 1923, p. 606; J. M. Lowry, Trans. Faraday Soc., vol. 17, 1922, p. 596; J. A. Christiansen, Zeitschr. phys. chem., vol. 103, 1922, p. 91. Regarding the influence of radiation see especially the publications of Professor Baly. See also J. Mellor, Chemical Statics and Dynamics, 1904, pp. 394, 414, 415; and Perrin and Hammick, Atoms, 1923, p. 168. The literature on catalysis is so extensive that no attempt is made here to give even a key to it. 7 Fundamentally this is a matter of convenience, and does not predicate anything narrowly characteristic of natural laws. The fact that the course of events is uniquely determined implies that the laws which determine that course can be expressed in the manner referred to. For a discussion of this question see J. Petzoldt, Maxima and Minima und Okonomie, Altenburg, 1891, pp. 17 et seq. 158 ELEMENTS OF PHYSICAL BIOLOGY laws, and it is to be expected that the law of evolution in life-bearing systems also, (where, as we shall see later, mechanism cannot be lightly waved aside into the convenient catch-all of the laws of thermodynamics), will be found to receive its most convenient expression in this form. In another respect the case of chemical evolution may confidently be expected to be found a good model in the treatment of the broader problem of evolution. It is to be noted that the law of chemical evolution is expressed in terms of the system as a whole. It is the thermodynamic potential of the entire system that approaches a minimum. Biologists have rather been in the habit of reflecting upon the evolution of individual species. This point of view does not bear the promise of success, if our aim is to find expression for the fundamental law of evolution. We shall probably fare better if we constantly recall that the physical object before us is an undivided system, that the divisions we make therein are more or less arbitrary importations, psychological rather than physical, and as such, are likely to introduce complications into the expression of natural laws operating upon the system as a whole. As regards the formulation of the laws of evolution in form of a maximum or minimum principle, it should be remarked that one such principle follows directly from the fundamental equations of kinetics as set forth in Chapter VI. If we multiply the first of these equations by Xi, the second by X2, and so on, we obtain at -2 . ~TT ^ ^1X1X2 + 022X2- +...-}- a2n.Xn.X2 +at (17) dt K n "" " nn- n. Hence by addition A -S & = 2Q(xh xt, . . . xn) + . . . (18) where Q represents a quadratic form. The relation thus obtained is not of general utility in this form. However, by a linear substitution CHEMICAL EQUILIBRIUM 159 & = NlXl + N,X, + . . . + 2STna;n (19) the equation (18) can be transformed into ~ at (20) where Xi, X2 , . . . Xn are the n roots of the characteristic equation for X, the same X's that function as exponents in the series solution of the original system of equations. 8 Now it will be recalled that the condition for stability at the origin is that all the real parts of the roots shall be negative. But in that case the quadratic form Q' is definite and negative. Hence the condition for stability at the origin can be expressed by saying that the quadratic form Q' must be definite and negative; or, by saying that Q' must have a minimum at the origin. And the law of evolution, near the origin, evidently is, according to (20), that S 2 continually decreases. (At points remote from the origin the terms of higher order, which have here been omitted, may cause increases in S.) The chief interest of the minimum principle here indicated lies in its analogy 9 to certain theorems in dynamics and thermodynamics, for which reference must be made to the literature, in particular to P. Duhem, Traite d'Energetique, 1911, vol. 1, pp. 460 et seq.; F. Michaud, Ann. de Phys., 1921, vol. 16, pp. 148 et seq. 8 For the sake of simplicity the argument has here been presented in the form in which it appears when all the roots X are distinct and real. For a detailed discussion of the conditions of stability when some of the roots X are multiple or complex see E. Goursat, Cours d' Analyse, 1915, vol. 3, pp. 31-43. 9 The analogy to the dynamical cases treated in the reference cited becomes particularly plain if we bear in mind that = when i =j= j = 2Xi when i j so that the quadratic form Q' can be written ' dQ' 5Q' 160 ELEMENTS OP PHYSICAL BIOLOGY where the bracketed exponent (2) denotes the symbolic square, in which '- } is> replaced by \JTC w\x W vjj -, and the product =-r- >T~J ig replaced by -^ ^--. \ The condition that the form so defined shall be negative, is that the deter- minant shall be negative, and also all determinants derived from it by striking out the last p lines and the last p columns. In the present case the same condition, can be expressed in simpler form to the effect that Xi, \^, . . . \a must all be negative. But it is worth while, in order to bring out the analogy, to note also the more complicated general form of the condition. CHAPTER XIII INTER-SPECIES EQUILIBRIUM Since the struggle for existence is chiefly a struggle for subsistence, a careful comparative account of the food of various competing species and genera at different places and seasons and at all ages of the individual .... cannot fail to throw much light upon the details, causes and effects of the struggle. Forbes. Equilibrium Condition in More Particular Form. The fundamental relations of statics are derived immediately from the corresponding equations of kinetics by substituting in the latter the value zero for the several velocities. This has already been noted with regard to the equations of kinetics in their most general form. In somewhat more particular form, useful in common numerical applications, we have a condition for equilibrium derived from the system of equations (14) of Chapter X . Xt - ViXi (1) dt 7if (2) 7if Xf JIM i (3) It should be noted that these formulae hold equally well if the masses are measured in ordinary units (e.g., pounds) or if they are measured in "head of population," with the proviso, of course, that the coefficients ui, Vi, are in each case expressed in corresponding units. The equation (1) expresses the fact that, for each component, the total inflow is just balanced by the total outflow, so that nowhere in the system is any accumulation of mass going on. This clearly implies that, unless there is complete equilibrium, the matter in the system must be in circulation, it must be going through one or more cycles. Such cycles are, indeed, very characteristic features in the scheme of nature. 161 162 ELEMENTS OF PHYSICAL BIOLOGY Numerical Illustration. We may, by the way of illustration, apply the formula (3) to the equilibrium between the several biological species comprised in a life-bearing system. For obvious reasons numerical data are most readily available for man and the species directly under his control. So, for example, we may let Xt. represent the mass (or number) of a human population, and Xt the mass (or number) of a population of sheep serving as food for that human population. In the United States in 1918 the consumption of mutton (or lamb) per head of the population per annum was 5.417 pounds. This is not strictly an equilibrium ration, since our population is increasing. However, the difference between this and the equilibrium ration is probably small. In our example we will therefore put jitui = 5.417 pounds = 0.1096 sheep 1 (4) Again in the United States in 1918 the number of sheep slaughtered per annum was 23.22 per cent of the standing herd. Hence afit>i = 0.2322 (5) so that Xf = "^Xi (6)f 0.2322 = 0.4718 Xi W In 1918 Xi = 103,587,955 head (8) Hence Xt = 48,873,000 head (^ i According to the Year Book of the Department of Agriculture, 1920, p. 759 the number of sheep slaughtered under Federal inspection m 1918 was 8 769,498. According to R. Pearl, The Nation's Food, 1920, p. 61, this represented 77 per cent of all the sheep slaughtered in that year, so that the total number slaughtered was 1 1,370,000. The total dressed weight of these, according to the Year Book, p. 826, was 502,214,000 pounds, which makes the average of one Bhoop carcass 49.45 pounds. The standing herd of sheep in 1918, according to the Year Book, p. 701, was 48,C03,000 on farms, or, adding a correction for animals not on farms! say 48,963,000. The percentage of animals slaughtered in a year out of the standing herd, was therefore 23.2216 per cent. For a review of various estimates of the output of herds of cattle, sheep swine, etc., the reader ia referred to a paper by R. H. Rew in the Journal of the Royal Statistical Society, 1902, vol. 65, p. 666. INTER-SPECIES EQUILIBRIUM 163 The actual standing herd of sheep in 1918 was 48,963,000 head of which 90,000 head furnished mutton for export, the United States not being a self-contained system. It is to be noted that in this example the products 7jf U[ and oifi vi are more easily ascertained than the individual coefficients ri o I--- S.2 !- ft 02 .5 INTER-SPECIES EQUILIBRIUM 179 supplies of food for the human population. The sources of these sources also demand attention. The problem forces itself upon our notice primarily (in the present state of society) in connection with agriculture. The fields cannot continue indefinitely 'to yield undiminished annual crops if the materials drawn from them are not in some way replenished. One important constituent needs no human intervention: carbon dioxide, owing to its gaseous form, automatically seeps in by diffusion as fast as it is absorbed by the FIG. 30. KEY TO FIGUKK 3 green plants. The same is true in some degree of free nitrogen , though the capacity of plants to assimilate this element is ^ strictly limited. 5 Water, also, is, in most agricultural areas, provided by the automatic meteorological processes of evaporation and condensation in rainfall. But as to certain other essential materials, notably combined nitrogen, phosphorus, potash and sulphur, the inherently immoUW constituents of the fertile soil, for these auto- * Science. November 24, 1922, p. 605. "Fiir sicli micht beweglich," Liebig, Die Chemie in ihrer Anwendung auf Agricultur, 1876, p. 382. 180 ELEMENTS OF PHYSICAL BIOLOGY matio replacement does not occur in sufficient measure ^ to satisfy the agricultural needs of the densely populated countries of this age. It becomes necessary for man to feed his food. Early man and primitive man, may reap where he has not sown. BuMong ago our tribe turned from the life of a nomad and hunter to tilling the soil and to animal husbandry. Thus was established a system of symbiosis with the links next above us in the food chain : the harvest ripening on the plain; and the cattle, grazing upon the pasture in summer, fed from the crib in winter. But early agriculture was essentially of the nature of a mining industry. It drew from the soil as from a bottomless well, without thought of a possible exhaustion of the source, or of any feasible replenishment to diminishing resources. Except that, by a semi-automatic, semi-empirical process, natural fertilizer was allowed to restore to the soil at least a part of its strength to bring forth a crop. One more step forward and man graduated from mining farmer into manufacturing farmer. The field became a factory fed with raw materials in the form of saltpeter, potash salts and phosphate fertilizer, imported, if need be, from afar; and producing its output of agricultural flora arid fauna. Lastly, in our own generation, we have learned to divert into the life stream the sluggish element, so essential to life, so illnamed by the French -azote; to make ourselves independent of the saltpeter beds, to assure our future against a nitre famine by opening the inexhaustible mine of the atmosphere. It is a singular thing that this element, so accessible, so abundant, in which we arc literally bathed within and without, every instant of our life, should so long have remained foreign to our industrial economy. Strange circumstances, yet not without close parallel. For even now we are powerless to avail ourselves effectively of the golden flood of energy that daily pours upon us without limit from above while we turn earthward to dig laboriously for the plainly exhaustible supply of coal to supplement our limited bodily energies. Food Chains in Aquatic Species. The principle that long food chains are essentially wasteful finds particular application also in the practical problem of the economic and rational utilization of marine organisms for human sustenance. As Professor Martin observes, the most economical course would be to utilize marine vegetation directly as food for man and his domestic animals. The INTER-SPECIES EQUILIBRIUM 181 use of algae as food for the table can hardly be expected to become an item of any consequence. Its use as cattle fodder presents better prospects. But our chief reliance will no doubt continue to be on the assimilation of marine plants by fish. To quote again Professor Martin:7 Since man prefers to harvest the plant life of the sea indirectly, those animals which feed directly on the plants are able to increase with less waste and at a more rapid rate, considered in total populations, than those which feed on other animals. Most of our food fish, for example, feed on smaller fish; these in turn feed upon small crustaceans and the latter eat the microscopic plants and detritus, so that in many instances the fish we eat are removed three or four steps, perhaps more, from the original food source. This is more significant than may seem apparent at first glance, since it involves an enormous waste. Before any organism can grow, the energy needed merely to live must be supplied, and by the time a crustacean is eaten by a minnow, or a minnow by a food fish, it will, on the average, have consumed a quantity of food several times its own weight. These facts are well brought out in the statistics of Petersen, and the diagram figure 37 based thereon. The edible shellfish, however oysters, clams, mussels and the like feed for the most part directly on the marine plants and this is one reason why the extension of the shell fisheries represents so much promise. Another advantage of this branch of aquiculture is also to be noted, namely, that most shellfish, like land crops, stay where they are planted. Even the scallop, which can swim about after a fashion, is restricted in its movement, and could readily be controlled. Oyster culture is already a great and important industry, but it has not nearly approached its possibilities. Clam culture is still in an embryonic state, and scallop culture has yet merely been suggested. When some of the problems confronting the establishment of these industries have been solved, we may hope to have acquired additional information concerning the ecology of the sea, which will help us in our approach to the more difficult problems of the future. Primary, Secondary and Tertiary Foods. It is often convenient to classify the foods for human consumption according' to their relative position in that portion of the food chain which is under human control. Commonly the meats of domestic animals are 7 For some further bibliographic indications regarding the food consumed by fishes see A. S. Pearce, Ecology, vol. 1924, p, 258. See also W. A, Herdman, Founders of Oceanography, 1923; J. Johnstone, Introduction to Oceanography, 1923. 182 ELEMENTS OF PHYSICAL BIOLOGY classed as secondary foods, since the production of these meats takes plate in two steps, first the growing of the fodder (for the most part materials not comestible by man), and second the transformation of a part of this fodder, in the animal economy, into food adapted for human consumption. On the other hand the fisherman's haul is for us primary food, growing feral, without human intervention. This classification must not be pressed. Where fields are supplied with fertilizer it might well be maintained that the cr^ps of wheat, potatoes, etc., commonly classed as primary, are secondary foods, while butchers' meats are tertiary. Even the catch of fish, and huntsman's quarry may not be strictly primary, in so far as game laws and regulations regarding the pollution of lakes and rivers represent some degree of symbiotic intervention on the part of man. Fine points apart, the distinction between the primary foods (crops and fish) and the secondary foods (butchers' meats) is economically most significant, for the consumption of fodder by farm animals is an item not merely comparable with human food consumption, but exceeding this latter manyfold. The fact, of course is, that farm animals are far from being economical and efficient converters of raw materials into food for human consumption. They represent a luxury, a humoring of the tastes of men at the expense of their purses. With the present density of population we can afford the luxury. Presumably the future will see retrenchments, with pastures and cornfields converted to wheat. Still tastes arc not accidental thiogs. Allowing for vagaries and exceptions, the things we like are, on the whole, good for us and for the species. Whether man can maintain his present status with a materially abridged meat ration is perhaps an open question. Should the answer be in the negative, the conclusion would seem to be forced upon us that an overcrowding of the earth would react unfavorably upon the vigor of the race; quality would be sacrificed to quantity. How this might affect the ultimate fate of our species is a subject for speculation. The pessimist might take a cue from palaeontology, recalling that the extinction of a species seems to follow, not infrequently, close upon its period of greatest development. The optimist, on the other hand, might perhaps extend the suggestion that when overcrowding does come, the ones to survive most surely, if not most abundantly, will be those whose superior qualities INTER-SPECIES EQUILIBRIUM 183 will enable them, in spite of intensified competition, to draw to themselves a sufficiency of the more desirable, though perhaps not absolutely essential articles of consumption. Natural selection would thus operate by the preferential survival of an aristocracy, while a submerged tenth would furnish a drain for the discharge of the unfit. Certainly, in the interests of the species, it were better that the inferior constituents be purged from the system than that they should drag down the general level to mediocrity and perhaps below the line of viability. But these are speculative reflections. Cycles. Food chains, were we able to trace them through their entire course, would undoubtedly be found to form closed cycles or a network of cycles. This is indeed a practical necessity for the continued performance of the processes or organic nature, processes that have gone on essentially unchanged in their general character, however modified in detail, for many millions of years. A few of the simpler food chains we may be able to follow with something approaching completeness through their cycle. For the most part, however, the system of interlocking cycles in nature is complex beyond all reasonable hope of detailed analysis in its entirety. If we are satisfied to omit innumerable details, we can trace, for each of the most important chemical elements7 concerned, the broad outline of its cycle in nature. The elements and simple compounds principally concerned are Carbon (dioxide) COz Oxygen O2 Nitrogen free N, NH3 , nitrites and nitrates Water H2 O Phosphorus (phosphates, etc. ) Brief consideration will presently be given to each of these cycles in turn. First, however, it will be well to review some of the essential facts regarding the occurrence of the chemical elements, generally, in nature. For the drama of life is like a puppet show in which stage, scenery, actors and all are made of the same stuff. The players, indeed, "have their exits and their entrances," but the exit is by way of translation into the substance of the stage; and each entrance is a transformation scene. So stage and players are T}ound together in the close partnership of an intimate comedy; and 184 ELEMENTS OF PHYSICAL BIOLOGY if we would catch the spirit of the piece, our attention must not all be absorbed in the characters alone, but must be extended also to the scene, of which they are born, on which they play their part, and with which, in a little while, they merge again. 8 8 Since the words above were written I have run across the following singularly apposite passage in- John Morley's Introduction to Wordsworth Collected Poetic Works: "Wordsworth's claim, his special gift, his lasting contribution, lies in the extraordinary stremxousness, sincerity and insight with which he first idealizes and glorifies the vast universe around us, and then makes of it, not a theatre on which men play their parts, but an animate presence, intermingling with our works, pouring its companionable spirit about us, and 'breathing grandeur upon the very humblest face of human life,'" CHAPTER XV THE STAGE OF THE LIFE DRAMA When the elements have been mingled in the fashion of a man, and come to the light of day, or in the fashion of the race of wild beasts or plants or birds, then men say that these come into being', and when they are separated, they call that in common parlance, death .... let not the error prevail over the mind that there is any other source of all the perishable creatures that appear in countless numbers. Empedocles. Our stage is a tripartite world: The heavens above, the waters of the sea, and the solid ground beneath our feet; the atmosphere, TABLE 11 Principal components of earth's surface the hydrosphere and the lithosphere. The total mass of the earth is about 6.5 X 1021 tons. But it is only the outer crust that interests us here, for the deeper layers have little or no part in terrestrial life. If we arbitrarily take a layer ten miles thick for the crust, the distribution of the material among the three main divisions is, according to F. W. Clarke, about as shown in table 11. The Atmosphere. There are two ways of confining a gas. The one most familiar in the laboratory and in products of human workmanship generally, is to enclose the gas in a suitable envelope, such as a glass vessel, or the cylinder of an engine; to put something around the body of gas to be confined. The other way, nature's way on a large scale, is just the opposite, and consists in putting something into the gas, or putting the gas around something. It is so the earth holds her atmosphere by gravitational attraction. Her hold is not impartial. She draws closest to her the densest constituents, and 185 186 ELEMENTS OF PHYSICAL BIOLOGY gives longer leash to the lighter. The atmosphere, in consequence, is not a homogeneous body, but varies in composition with altitude. At the same time, owing to its elasticity, the air in its lower strata is compressed by the weight of the overlying atmosphere, so that 99 per cent of the whole is contained within a shell 30 km. (18| miles) thick. The remaining 1 per cent extends out into space without any Of CLOUDS * QROlMAW OUST J FIG. 40. CROSS SECTION OF THB ATMOSPHERE, SHOWING SOME FEATURES CHARACTERISTIC OF DIFFERENT ALTITUDES After W. J. Humphreys assignable limit, but at any rate to a height of some 300 km. (185 miles), as evidenced by the aurora. A graphic representation of the broad divisions of the atmosphere is shown in figure 40, adapted from Wegener and Humphreys. 1 A more detailed and exact statement of 1 Physikalische Zeitschrift, 1911, vol. 12, p. 172. See also W. J. Humphreys' work, The Physics of the Air (Lippincott, 1920), pp. 68, 69. Also, the same author, Bulletin Mt. Wilson Weather Observatory, vol. 2, 1909, p. 67; STAGE OF THE LIFE DRAMA 187 OF CONSTANT TffMPfMTVfie. FIG. 41. COMPOSITION OF THE ATMOSPHERE AT DIFFERENT LEVELS After W. J. Humphreys Journ. Franklin Institute, vol. 175, 1913, p. 208, 212. A singular view has lately been put forward by L. Ve"gard. He identified certain green lines in the auroral spectrum with lines observed when solid nitrogen is rendered phosphorescent by x-rays. He concludes that the upper atmosphere contains solid nitrogen. (See Nature 1924 vol.113 p. 716.) Ve"gard's view has been opposed by J. C. McLennan, Roy. Soc., June 19, 1924. 188 ELEMENTS OF PHYSICAL BIOLOGY its composition at different altitudes, up to 140 kin., is given in table 12 and illustrated graphically in figure 41, derived from Humphrey's work. A complete discussion of the r61e played by the atmosphere in the round of terrestrial life would amount to nothing less than a treatise on meteorology, such as forms no part of the present project. What TABLE 12 Percentage distribution of gases in the almosphere important factors weather and climate are in the business of providing the sustenance of life is a matter of common knowledge, and a very particular concern of the farmer. Yet we must here be satisfied with little more than a passing reference to meteorology, noting only a few elementary facts which bear directly upon the subject in hand, the circulation of the chemical elements in nature. Losses from the Atmosphere. A first question that suggests itself in this discussion of the economy of nature is this: Since the atmosphere is "open at the top," so to speak, is there not a loss, a constant leakage of gas out into space? The answer to this question must be STAGE OF THE LIFE DRAMA 189 sought in terms of the molecular constitution of the gases of our atmosphere. A cubic centimeter of air contains (at 0C.) about 3.15 X 1019 molecules. These are in continuous agitation, somewhat after the manner of a swarm of gnats, except that they flit about with speeds comparable with that of a rifle bullet (about 500 meters per second) rather than with the leisurely flight of an insect. At a temperature of 0C. a molecule of nitrogen has, on an average, a velocity of 492 meters per second. A molecule of hydrogen, under the same conditions, would have an average velocity of 1839 meters per second. It must be understood that these figures represent, in each case, a mean about which the velocities of individual molecules cluster, so that a certain proportion of them will fall below and others will exceed the figures stated. At the earth's surface the average distance travelled between two successive collisions is about ^iroTolTo cmBut in the upper ranges of the atmosphere conditions are very different. If we follow the estimates and computations of J. H. Jeans, we find that at an altitude of 3200 km. the atmospheric pressure is reduced to about 1/10 14 of its value at sea level; but even at this low pressure there are still about 300,000 hydrogen molecules per cubic centimetre. (At this altitude all other gases except hydrogen are practically absent) . The mean free path between collisions is now 10,000 km. or about If times the earth's radius. In such circumstances collisions between molecules are rare, and for the most part the molecules move freely through space in parabolic or elliptical orbits, and become virtually diminutive satellites of the earth. Since the day of Jules Verne's story From the Earth to the Moon it has been a matter of popular knowledge that a body projected from the earth with a velocity exceeding 7 miles per second will go off in a hyperbolic orbit, never to return. This applies to the molecules of a gas. Any of them that may be travelling outward with such a speed in the region where collisions are so rare as to be negligible, will leave the earth for good and will thus be lost to our atmosphere. The rate of leakage from the atmosphere thus depends on the number of molecules per unit of time that acquire the limiting (outward) velocity of 7 miles per second. This number, in turn, depends on the temperature in the region under consideration, a point regarding which our information is very uncertain. But an exact knowledge of this temperature is not needed to compute a major limit, a maximum figure which the rate of escape certainly cannot exceed. It 190 ELEMENTS OF PHYSICAL BIOLOGY is thus found that under present conditions2 the earth holds her atmosphere so effectively that there cannot be any appreciable leak even in many millions of years. Cosmic losses from the atmosphere then, are, for nil practical purposes; wholly negligible. Certain other subtractions from and accessions to the atmosphere we shall have occasion to note as we consider the circulation of the several elements. As a matter of fact the composition of the atmosphere in the region in which living organism have their habitation is very nearly uniform3 and constant, except TABLE 13 Constituents of the, atmosphere Earth's surface = 1,97 X 10 8 square iniloH ~ 5.5 X 1018 square foot. One square mile = 2.79 X 10 7 square fcofc. One metric ton = 2205 pounds. s It may be noted in passing that in the earth's pant history conditions may have been different. If at any time the temperature of the upper atmosphere was about 750C., then there must have been a very distinct loss of hydrogen by leakage into space. The moon, and certain of the planets having a lesser gravitational pull or a higher temperature (Mercury), have probably lost in this way any atmosphere that they may have had. For a detailed discussion of this and other points in connection with the escape of gases from the atmosphere the reader may be referred to J. H. Jeans's Dynamical Theory of Gases, 1921, Chapter XV. See also K A. Milne, Trans. Cambr. Phil. Soc., vol. 22, 1923, p. 483; J. E. Jones, ibid., p. 535. 8 Except in the neighborhood of volcanoes, and in lesser degree, in or near large cities or manufacturing centers, where large amounts of waste gases may be discharged into the atmosphere. STAGE OF THE LIFE DRAMA 191 192 ELEMENTS OF PHYSICAL BIOLOGY as regards its moisture content, and wo may accept for the composition of the atmosphere at the earth's surface, moisture excluded, the figures shown in the first two columns of table 13. The third column shows the total amounts of the several constituents of the entire atmosphere, according to W. J. Humphreys (Monthly Weather Review, vol. 49, June, 1921, p. 341). Cosmic Accessions to the Atmosphere. Meteorites falling upon the earth from space bring with them certain o entities of entangled or occluded gases. While this contribution tt the atmosphere is at the present time, presumably, of negligible dimrnsions (see also page 195, Cosmic Accessions to the Lilhospfwrc), yet in the course of the TABLE 15 Comparison of air and aqiutlic atmosphere * Measured at 0G. and 760 nun. Ug. f42.7ingm.; according to F. W. Clarke, Data of CicocluMnistry, Geological Survey Bulletin. 491, 1920, p. 142; G. Linck, KroiHlaufvorgiitige in dor ErdgescMchte, Jena, 1912, p. 6. long procession of ages past this source may not have been wholly insignificant. Data on this question, are at best very uncertain, and a mere passing reference must suffice. 4 The Hydrosphere. In comparison with the ocean alt other aggregations of water upon the earth are insignificant in aimmnt. The bald statement of the total volume of the ocean 302 million cubic miles 'conveys but little to the mind. More impressive it is to recall that the average depth of the sea is 2$ miles, and that, even if these waters were spread over the whole earth, leaving no continents, the average depths would still be If miles. The average composition of the ocean is shown in table 14. Here again, the figure for the volume of total dissolved solids, 4.8 million cubic miles, is made more readily comprehensible by a graphic illustration. The salts of the ocean, made into one solid block, would * F. W. Clarke, Data of Geochemistry, U, S. Geological Survey Bulletin 695, 1920, pp. 58, 269, 282. STAGE OF THE LIFE DRAMA 193 cover the entire United States and Alaska to a depth, of Ixfr miles; or according to J. Joly, they would encrust the whole earth to a depth of 112 feet. 5 The Aquatic Atmosphere. Aquatic species perform their respiration in contact with an atmosphere of gases held in solution in the water that surrounds them. This atmosphere is very different both in concentration and also in composition from, that in which we live, as is apparent from table 15. A comparison of the several columns in table 15 is an object lesson on the adaptability of living organisms to varied conditions. The atmosphere in which fish and other marine animals live in comfort would not only drown us with its principal constituent, water, but, even if this were removed, the residual gases would suffocate us for lack of oxygen; and if the deficiency in this gas were made up by the addition of the amount required to bring the percentage up to that to which we are accustomed, we would still be choked by the excessively high percentage of carbon dioxide.6 The Lithosphere. Immense as the ocean appears to us, with its average depth of 2| miles, yet it constitutes less than vsV'o At 7.30 A/a Z.S8 a p ra?o r F Mn /y n 0.11 ato o.og s O.I1- Fe O.Ol 63.0 0.10 O.H Z.S Compost ft'an a'f Human Boc/y. FIG. 42. COMPARISON OF COMPOSITION OF EARTH'S CRUST AND HUMAN BODY Figures indicate percentages STAGE OF THE LIFE DRAMA 197 cent for all the other elements, among them some quite indispensible for our existing civilization. 11 Relation to Composition of the Organism. Of the elements specifically significant for the living organism, only one, oxygen, is present in great abundance. Carbon, hydrogen and nitrogen, the principal "organic elements/' are among the less abundant constituents of the globe. On the whole it may be said the living organisms are composed of comparatively rare elements. We are, indeed, earthborn, but yet not altogether common clay. 12 This is well brought out TABLE 17 Average composition of human body in the chart figure 42, which shows, side by side, the average composition of the known terrestrial matter, and, in comparison, the approximate composition of the human body. This latter is not exactly a representative sample of the totality of living matter (see tables 17 11 H. S. Washington, Jour. Franklin Institute (1920), vol. 190, p. 7. Tho figures have been slightly modified in accordance with the latest data of F. W. Clarke and H. S. Washington, Jour. Natl. Acad. ScL, 1922, vol. 8 p. 114. 12 Indeed, taken literally the expression "common clay," as applied to man, is an extreme case of poetic license; for aluminum and silicon the chief constituents of clay, and taking second and third place in rank of abundance among the components of the earth's crust, are both present only in tracea in the human body. 198 ELEMENTS OP PHYSICAL BIOLOGY ^ STAGE OF THE LIFE DRAMA 199 d ft C 03 CQ 200 ELEMENTS OF rriYBTCAL BTOLOftY .a .a Ol VCJ m S M.O O tCJ JD S ft cu q H cu . y w l>> 2 ti .in a -fl STAGE OF THE LIFE DKAMA 201 and 18) but will serve well enough for the present pupose. The chart brings out very pointedly the selective character of the organism's activity in gathering to itself the substance of its body. Thus carbon, which both in function and in relative quantity figures so prominently in living matter, appears as an insignificant lifctle block in the chart of the earth's crust. A similar contrast, if not quite so extreme, is seen in the case of nitrogen. With aluminum and silicon the comparison works the other way about very plentiful in the earth's crust, these elements are practically absent from the human body. 13 Taking the mother earth as a whole, and the organism as a whole, it certainly cannot be said that there is much evidence of "inheritance TABLE 19 Composition of the salts in sea water and in blood serum in per cent* * Maccallum, Trans. Koy. Soc. Canada, 1908, II, p. 145. of parental characters" in their respective compositions. Still, resemblance is not wholly lacking. This becomes evident if we compare, not the entire organism with the whole of the earth's crust, but the blood of a mammalian, for example, with the water of the ocean. This comparison is made in table 19 and figure 43. The likeness thus seen, imperfect as it is, can hardly be ascribed to accident. The fact is, 13 Silica furnishes, however, the skeletal support in a variety of living forms (radiolaria, sponges, plants). Cf. G. Bunge, Physiological and Pathological Chemistry, 1902, p. 23-24. For a detailed discussion of the distribution of the chemical elements in organic nature see Vernadsky, Revue Ge"n. Sci. The reader interested in this phase of the subject should not fail to acquaint himself with this article, which came to the writer's attention too late to be given more than this passing note here. 202 ELEMENTS OF PHYSICAL BIOLOGY Cl 55.3 Na 30.6 SoJJds in 7.66 3.79 KU Br O.f3 O.O 0.4 1.0 2.7 0.4 Soh'ds in Blood Serum No 39 an a dry fi Cl 45 . 43. COMPARISON OF SEA WATER AND BLOOD SERUM STAGE OF THE LIFE DKAMA 203 as pointed out by Palitzsch, 14 that aquatic species are in such intimate contact, both at their body surface, and more particularly in their gills, with the surrounding water, that the latter might almost be considered continuous with their bloody fluids, so that sea water may justly be "placed in the same category as the other physiological fluids." "Frederiq 15 has shown that the amount of sodium chloride in the blood of Crustacea varies, and all but corresponds, with the density of the water in which the creature has been kept." More highly organized aquatic species have made themselves in greater degree independent of the salinity of their environment; 18 and finally, it would appear, when the marine ancestors of terrestrial vertebrates emerged from the sea and adventured life on dry land, they packed, as it were, a portion of their saline environment in their baggage, and took it along with them on their excursion as an essential part of their milieu interieur. And to this day, according to this view, we ourselves cany about with us in our arteries and veins, if not a portion of the actual ocean, at least a roughly approximate replica of its brine. For, as L. J. Henderson17 remarks: "Not only do the body fluids of the lower forms of marine life correspond with sea water in their composition, but there are at least strong indications that the fluids of the highest animals are really descended from sea water." Some such indications may be seen in the reflections (conceived from a slightly different point of view) of G. Bunge, 18 "I am convinced that the remarkably high percentage of salt in vertebrate animals, as well as the desire to take salt with our food, can be satisfactorily explained only by the theory of evolution." In support of this consideration Bunge points out that in the weathering of rocks by the action of rain-water charged with carbonic acid, the sodium is dissolved and carried off as carbonate, while the potassium largely remains behind in combination with silica. The sodium carbonate being washed to 14 Comptes-rendus, Laboratoire de Carlsberg, 1911, vol. 10, part I, p. 93. See Chapter I, footnote 19. 16 Arch, de Zool. Exp. et Gen., 1885, Ser. 2, vol. 3, p. XXXV; see also D'Arcy Thompson, Growth and Form, 1917, p. 127. 16 Compare D'Arcy Thompson, loo. cit., p. 127-130; Claude Bernard, Introd. a 1' etude de la me"decme exp., 1855, p. 110 as quoted on p. 17 (and footnote 20) of Chapter I. 17 The Fitness of the Environment, 1913, p. 187. 18 Loc. cit., 1902, p. 101-103, 204 ELEMENTS OF PHYSICAL BIOLOGY the sea undergoes double decomposition with the alkali earth chlorides, these latter being deposited as carbonates (limestone and dolomite) while the sodium remains in solution as salt. Thus sea water is rich in sodium chloride and poor in potassium, while on dry land the balance is essentially reversed.19 Plants and invertebrate animals, Bunge points out, contain little sodium, unless they live in a highly saline habitat, in or near the sea, or on salt steppes. Yet the land vertebrates are all remarkably rich (comparatively) in salt, in spite of the scanty supply around them. Is not the large amount of sodium chloride found in the present inhabitants of dry land another proof of the genealogical connection which we are forced to accept from morphological facts? There is no doubt that each of us in his individual development has come through a stage in which he still possessed the chorda dorsatis and the branchial arches of his sea-dwelling ancestors. Why may not the high average of salt in our tissues be also inherited from them? Support for the supposition thus suggested is seen by Bunge in the fact that the younger a vertebrate is in its individual development, the more salt does it contain. Furthermore, cartilage contains the highest percentage of sodium of all the tissues of our body, and is also the tissue of greatest antiquity. The human skeleton is originally composed of cartilage, which is replaced, for the most part, by bone as the individual matures. These are facts which lead most readily to the interpretation th? * the vertebrates living on dry land originally came from the sea, and aw still continuing to adapt themselves to their present surroundings, where they can get but little salt. We prolong this process of acclimation by taking advantage of the salt strata which have been left on the land by our primeval element, the salt flood. Chemical Correlation in Soil and in Organism. Our ancestral resemblance to the soil from which we spring is also exhibited by evidence converging from a different source. II. S. Washington, 19 This observation must be accepted with some caution. Compare Whitney, Science, 1922, vol. 56, p. 218. "Until we determine the actual loss, through chemical denudation, of silica, alumina, iron, potash and other electrolytes in the colloidal state, carried by rivers, we are in no position to even speculate as to whether erosion is a selective process which might change the chemical composition of the soil." STAGE OF THE LIFE DEAMA 205 in his studies on The Chemistry of the Earth's Crust, already cited, draws attention to the fact that in the rocks soda and iron tend to be associated together as a pair on the one hand, and potash and magnesia on the other. This is well brought out in the diagram figure 44, reproduced from Washington's memoir, in which it is seen that the points representing the analysis of a number of rock samples tend to group themselves about the diagonal of the square, indicating that FeO FlG. 44. COKBELATION IN THE OCCURRENCE OF Na, Fe AND ~K, Mg IN ROCKS A large number of analyses here plotted show a marked tendency to array themselves along the diagonal, showing that high percentage of Na is commonly associated with high percentage of Fe; K and Mg follow a similar relation. After H. S. Washington. high content of soda goes together with high content of iron, but with low potash and low magnesia; and vice versa. The point of special interest to us here in the present connection is that to which Dr. Washington draws attention in the words: Curiously enough, the same correlation between these two pairs of elements, soda and iron, and potassium and magnesium, seems to hold good in the organic world. This is apparently shown by the following facts: In 206 ELEMENTS OF PHYSICAL BIOLOGY autotrophic plant metabolism potash is an essential element, as is also magnesium, in that chlorophyll (which in the leaves acts as the carbon-transferring substance) is a magnesium salt of a complex organic acid, while sodium and iron are generally toxic toward (at least the higher, gymnospermous and angiospermous) plants. On the other hand, sodium, rather than potassium, is the alkali metal essential to the higher animals, salt being a very necessary article of diet (in part because of its chlorine, and in part because of its sodium, content), and sodium chloride is present in the blood plasma; and at the same time, hemoglobin and its derivatives (which act as oxygen carriers, and are analogous to chlorophyll in plants) are iron salts of organic acids closely related to that of chlorophyll; while, similarly potassium and magnesium are more toxic toward the higher animals than are the other pair. This singular parallel must not, of course, be looked upon as an instance of resemblance due to anything of the nature of inheritance of ancestral traits in the biological sense. Rather must it be connected in our minds with the fact that systems composed of the same fundamental substances, will display certain analogies through interplay, in them, of the same chemical affinities. Accessibility of Valuable Earth-Constituents. Such a comparison as has been made above of the relative abundance of the several elements in the living organism and in the environment from which it draws its supplies, would be misleading if attention were not drawn to another factor aside from abundance, which enters strongly into play in the quest for the necessities of life. More important than mere abundance is accessibility. For, a substance may be present in comparatively large quantities, and yet be difficult to lay hold of, either on account of its wide dispersal in dilute form, or for other reasons. On the contrary, a comparatively rare substance may be procurable with relative ease, if it occurs segregated in concentrated or otherwise readily accessible form. Perhaps the most telling illustrations of this are to be found in industry. The element copper for 2 example is found only to the extent of about -r per cent in the earth's crust. Yet it is one of the most important metals in the arts, and is not ordinarily thought of as particularly rare. This is because, in those regions where it does occur, it is found in concentrated form, either as native metal, or as rich ore. Other instances are readily cited. Tin, lead and zinc are all rarer than copper, and each rarer than its precursor, in the order named. Still rarer are silver, tungsten, gold, bromine and platinum, all of which find important use in STAGE OF THE LIFE DRAMA 207 ^ O r-l (-H r-t WrH M Si r-i CM CO 42803 22 19 iO CO t- 00 CJ 1SI n S 02 WO *z W ffl 02 o ,_, O CU -> J _O pa 5 R H -<1 ^ O p OM W fM 208 ELEMENTS OF PHYSICAL BIOLOGY the arts. But the mode of occurrence of these substances is such that they can be gathered or rained with comparative ease. It has been pointed out by H. S. Washington that the elements, as arranged in Mendeleeff's table, naturally fall into two groups divided by a zigzag line, as shown in figure 45. Above this line are the rock elements or petrogenic elements, that enter into the principal rock-forming minerals (and also, the gases of the atmosphere). Below the line are the ore elements or metallogenic elements, which commonly occur in concentrated form as ores and as native metal. Now man's industrial activities are merely a highly specialized and greatly developed form of the general biological struggle for existence ; and this same feature of accessibility and of concentration in segregated supplies (ores and the like), which is a prime condition for the very existence of some of our industries, is also involved, in closely analogous manner, in the more primitive life processes. Our fields demand fertilizers bringing ammonia, nitrates, potash, phosphates, etc., in suitably concentrated form, if they are to bear a harvest commensurate with the needs of a modern community. And this again is merely an accentuated example of the still more primitive needs of the unsophisticated flora and fauna of virgin nature. Of scattering, dissipating processes there are plenty. Rain and snow wash most of what is soluble, and much that is not, into the rivers and^ut to sea. Our own activities in modern intensive agriculture briiig each year to the land a highly concentrated diet of fertilizers, which in the very act of cultivation are scattered and diluted many thousand times. And our modern sewage system is deliberately wasteful of vital substances, which it discharges into streams and out TO sea. All this dissipation must in some way be balanced if the regime is to continue. Thus the circulation of matter in nature must no/fc only provide for the mere presence of certain substances on which ^che maintenance of life depends, but it must furnish them in suitable ' concentration and, generally, in available form. It must, therefore, in many cases include, as a definite step, a segregating or concentrating process 20 as well as simple motion through a cycle. We shall have occasion to note concrete illustrations of this in the separate consideration of the circulation of the several elements, to which we now proceed. 20 The significance of this from the point of view of energetics will engage our special consideration in a later section. CHAPTER XVI THE CIRCULATION OF THE ELEMENTS -THE WATEH CYCLE The great Sea-water finds its way Through long, long windings of the hills; And drinks up all the pretty rills And rivers large and strong: Then hurries back the road it came Returns on errand still the same; This did it when the earth was new; And this for evermore will do As long as earth shall last. Wordsworth. The ancients, totally blind as they were perforce to the fine details of material transformations revealed by the search light of modern chemistry, nevertheless recognized in its broad features the cycle of life, the circulation of the elements in nature. "Dust thou art, and unto dust shalt thou return," we read in an old book of wisdom. Heracleitus (536 to 470 B.C.), promulgator of the famous doctrine Tr&vra /Set has a more detailed, if not more accurate conception of the cycle of Nature, which he formulates in these terms: Earth S \ Fire Water Vapor (Air) The human mind was not yet schooled, then, to polish the facets of this rough gem, and bring out the sharp-edged truth as we see it today Solid \ Liquid Vapor 209 210 ELEMENTS OF PHYSICAL BIOLOGY But all honor to the minds that discerned through the mists of dawn the bold features of the landscape to be revealed in the sunlight of later day. Today we recognize not four elements, but over ninety, not counting those modern variants, the isotopes. And we follow in much detail not one cycle, but, as particularly pertinent to life, five major cycles the circulation of water, carbon, oxygen, nitrogen and phosphorus. This was noted already at the conclusion of Chapter XIV, but the discussion of the cycles was deferred to give space to a preliminary survey of the scene in which these cycles churn the planet's surface in their age-long duty. We are now prepared to take up the thread where we broke off; we turn our attention first to the water cycle. Water Requirements of Human Body. We do not ordinarily class water as a food, though we partake of it by the same channel .. | that gives entrance to the materials commonly so classed, and although the lack of water, if we are by any circumstance deprived of this substance, is felt even more acutely than an interruption in the adequate supply of food. The fundamental basis for this distinction, its origin in the unsophisticated mind, is undoubtedly the fact that we have a separate sense of thirst, distinct from the signals of hunger and appetite originating from nutritive demands of the body. And this naive, unsophisticated distinction is entirely in accord with the reasoned analysis of the respective functions of water and of food in the narrower sense. It is undoubtedly just because of this difference in function that thirst and hunger have been developed as separately recognized sensations. Water acts merely as a vehicle; unlike the food, which undergoes extensive and complicated reactions within the economy, water leaves the body essentially as it enters it, unchanged chemically, though charged (in part) with substances in solution. It would be a gross error, however, to suppose that water, because it functions thus in accessory capacity, and escapes the more intimate transmutations of metabolism, can be lightly regarded in making a survey of the participation of the several elements in the cycle of nature. It must be remembered that water constitutes as much as 60 per cent of the total mass of the human body, for example, and a still greater proportion of the substance of most of our food-stuffs, as shown in table 20. _ .,*f? WATER CYCLE 211 Thus an adult human being consumes per diem about 3 liters of water of which about 1 liter is contained in his solid food. In point of fact he consumes about 5 pounds of water for every pound of dry solid matter ingested. It is thus seen what an important item water is in the daily economy of the human organism. The excretion of water by the kidneys, lungs, intestine and skin is somewhat in excess of the intake. The excess of the outgo over the intake is formed in the body by the oxidation of hydrogen organically combined.1 Water Requirements of Plants. Rainfall as a Limiting Factor. In the economy of most plants the traffic of water is of even greater importance 2 than in man and land animals generally, and TABLE 20 Moisture content of some common foods indirectly the moisture needs of plants are, of course, of fundamental importance also to the animal population feeding on the vegetable growth of the soil, so that the water supply of a territory 1 L. J. Henderson (The Fitness of the Environment, p. 133) estimates that a man weighing 60-70 kgm. excretes daily: grams Water 2500-3500 Carbon dioxide 750- 900 All other substances 60- 125 and that water is, accordingly, three-fourths and carbon dioxide one-fifth of the total excreted. The proportion of water excreted from kidneys, skin, lungs and intestines, is given by Kirk (Physiology, p. 208) as 1:0.5:0.22:0.09, or 11.5:5.75:2.5:1. 2 L. J. Henderson, loc. cit., estimates that of the materials ingested by ordinary green plants, more than nine-tenths is water, and carbon dioxide at least five sixteenths of the remaining tenth. 212 ELEMENTS OF PHYSICAL BIOLOGY may function as the basic limiting factor of the total life which that territory is able to support. A study of these relations with particular reference to the human population of the United States, has been made by W. J. McGee, who remarks : 3 Hellriegel in Germany and King in this country have shown that crop plants require for their growth_a quantity of water, measured by transpiration, averaging from 300 to 600 (with a mean of about 450) times the weight of the plants after drying; and common field experience indicates that, in addition to the moisture passing through the plants, the soil requires an even larger quantity to maintain a texture suitable for crop growth much of which passes away through evaporation and seepage. On this basis "the agricultural duty of water" in this country has been formulated as the production of one-thousandth part of its weight in average plant crop. Reckoning human food and drink on this basis, and assuming that meats require (chiefly in the growth of plants used as feed for the animals) ten times the quantity of water represented in vegetal food, it appears that the adult who eats 200 pounds each of bread and beef in a year consumes something like 1 ton of water in drink and the equivalents of 400 tons in bread and 4000 tons in meat, or 4401 tons in all figures corresponding fairly with the results of intensive agriculture in arid districts. Accordingly, the "duty of water" considered in relation to human population may be stated roughly as the maintenance of a human life a year for each 5 acre-feet used effectively in agriculture. Now mainland United States (i.e., the chief body of our territory, exclusive of Alaska and the insular possessions) comprises something over 3,000,000 square miles, or somewhat less than 2,000,000,000 acres of land; yet the annual rainfall the sole original source of fresh water averages barely 2* feet (30 inches), or hardly 5,000,000,000 acre-feet. So while the land area, if peopled to the density of Belgium (over 640 per square mile,) would carry a population of 2,000,000,000, the water supply suffices for only 1,000,000,000. The conclusions of McGee may have to be modified in point of detail, and some of his figures may perhaps have to be revised; but the general principle underlying his reflections attract our attention. The moisture needs of the living population (all species included) are a large and fundamental item in biological economy; whether this item proves the ultimate limiting factor of population growth, as McGee suggests, is a question whose answer must be sought in 3 Science, 1911, vol. 34, p. 429; Yearbook of the Department of Agriculture, 1910, pp. 169-176; Bureau of Soils Bull. 71 (1911), pp. 7-14; World's Work, 1912, vol.. 23, p. 443. Compare also L. J. Briggs, The Water Requirements of Plants, U. S. Department of Agric., Bureau of Plant Ind Bulletins 284, 285. WATER CYCLE 213 terms of Liebig ? s Law of the Minimum; a dearth of other essentials may make itself felt before the limit of available moisture is reached. The Sources of Supply. Such, then, in broad outline, are the moisture needs of organic nature; as such they have existed, in greater or less degree, for millions of years, and have been satisfied, and will continue long to be satisfied, from a source essentially inexhaustible because constantly replenished by the return flow : The great reservoir is the ocean, with its 302 million cubic miles of water, and an evaporating surface of over 144 million square miles. Annually there rise from this into the atmosphere about 63,300 cubic miles of water, to which some 22,800 more are added by evaporation from the land, making a total of 86,100 cubic miles. This figure also represents the total precipitation in rain, snow, etc., but of the total about 56,700 fall back directly into the ocean, and only the balance, 29,400 is available for the needs of the land. It has been noted that the evaporation from the land is about 22,800 cubic miles. The difference between this and the precipitation on land, the balance of 6500 cubic miles, is the drainage from the land to the ocean by rivers. No attempt will be made to estimate what proportion of the precipitation on land is derived from evaporation over the sea, and what proportion comes from the land itself. Some idea of the relation, however, can be formed from a consideration of the difference or the ratio of the rainfall within the area drained by rivers and the amount actually discharged by them into the sea. John Murray 4 has collected information on this subject, with the result shown in table 21, which covers 33 of the world's principal rivers. It will be seen that the total rainfall in the area of these rivers is 10,186 cubic miles, the discharge to the sea is 2182 cubic miles, leaving a difference of 8004 cubic miles unaccounted for. A certain portion of this perhaps represents seepage, but the bulk must correspond to water reevaporated from the land and from inland waters. It will be observed that for the 33 rivers combined the proportion of the discharge to sea to the total rainfall is about one-fifth. For individual rivers the ratio varies widely, between the extreme of 0.58 (Rhone) and 0.027 (Nile). Naturally the climate very materially affects this figure. 4 Scottish Geographical Magazine, 1887, vol. 3, p. 76. 214 ELEMENTS OF PHYSICAL BIOLOGY There is also a circulation of waters of the sea in very large dimensions. According to L. J. Henderson5 the Gulf Stream in the Straits of Yucatan carries 200 million tons per second, 6 travelling TABLE 21 Showing the drainage area, annual rainfall, annual discharge, and ratio of discharge to rainfall, of S3 rivers in different parts of the world 5 The Fitness of the Environment, 1913, p. 182. 8 Across any cross-section of the stream, presumably; the statement is not clear on this point. WATER CYCLE 215 with, a mean velocity of about 80 miles per day. This circulation in the ocean has of course no direct part in the water cycle of the organic world, but indirectly is most important on account of its climatic effects. m\ r Oceo/% ///&./m. mill $f mi. figures \rifhout denomination afie cubic FIG. 46. CIRCULATION OP THE ELEMENTS IN NATURE. THE WATEE CTCLEI Water Cycle Diagram. The principal figures relating to the circulation of water on the globe are exhibited in diagrammatic form in figure 46, which tells the story more effectively than words. It may here be added in explanation that the 3000 cubic miles of 216 ELEMENTS OF PHYSICAL BIOLOGY moisture contained in the air are practically restricted to the lower 6 miles or so of the atmosphere. For the rest, this moisture is unevenly distributed, as everybody knows from personal weather observation. Water vapor and condensed water differs in this respect from the other permanently, gaseous constituents of the atmosphere. (See table 12 and figures 40, 41.) Fraction of Total Water Circulation Taking Part in Life Cycle. Only a fraction of the total circulation of water actually passes through the organic cycle. We may make an attempt as follows to obtain a rough idea of the order of magnitude of the fraction thus concerned. If the entire land surface were cultivated to produce crops at the rate adopted as standard by W. J. McGee, the growth produced (figured in dry weight) would be T^u~ff of the rainfall. Furthermore, this growth would evaporate, by transpiration, about 500 times its own weight of water, (this is assuming one crop per year). It would therefore evaporate just about one-half the annual rainfall. But the 22 800 total evaporation on the land is OQ'QQQ = tnrce fourths of the annual rainfall on land, the remaining fourth being drained to sea by rivers. Hence, of the water evaporated on land, one-half times four-thirds = two-thirds is evaporated by plants and thus takes direct part in the organic cycle. In comparison with the evaporation by plants, that from animals is undoubtedly negligible, especially in view of the coarseness of our data. If we put the evaporation on land as one-fourth of the total evaporation, we finally arrive at the value one-sixth as that fraction of the total water in circulation, which takes actual part in the organic circulation. Desert areas cannot materially alter this estimate, since they contribute but little to either side of the account, both evaporation and life being meagre or absent. In some measure this remark also applies to frigid wastes of the polar regions, where the low temperature makes for comparatively low evaporation (a factor counter-balanced, it is true, in some degree, by the extensive cover of ice and snow) . For temperate zones McGee's figure for cultivated fields is undoubtedly too high to apply as an average for the entire land. In the tropics, on the other hand, it is perhaps not excessive. On the whole the fraction one-sixth computed as above is probably too high, but perhaps it serves to give us an idea of the order of magnitude involved. WATER CYCLE 217 Another estimate leading to a materially lower result, is obtained as follows: If we accept Engler's estimate that one-fiftieth of the atmospheric carbon dioxide, that is to say, 4.4 X 1010 metric tons, takes part in the organic cycle; and we adopt the figure given by L. J. Henderson2 that the water taken up by plants, is about 11 times the C02 which they absorb, we obtain, as a very rough estimate of the water engaged in the organic cycle, an amount of 5 X 10U metric tons, or, in round numbers, 120 cubic miles. This, then, is about vfar of the total annual circulation of water, or about $%-$ of the total rainfall on land. CHAPTER XVII THE CARBON DIOXIDE CYCLE Behold how great a matter a little fire kindleth. St. James. If the lamp of life is a poetic symbol, it is an image essentially true to fact. Not only is life, in particular animal life, largely a combustion process: like the flame, life reaches out for fuel, and with the power gained, strains again for more. Like the flame it consumes, and it spreads. And as the fire sends out sparks, of which many die, but a few, falling upon favorable ground, flare up as a second generation, in reproduction of the parent flarne; so the living creature scatters its seed, some to die, but some also to live again the life of the parent. "But," someone perhaps will remark, "a fire may start without preexisting flame; whereas all life is itself begotten of life." Is this distinction really so fundamental? In nature undisturbed by man the starting of a fire spontaneously is a rare event; and that, after all, is the most that we can say positively regarding the origination of life from the non-living it is either so rare or so unobtrusive1 an event as to have escaped our observation. No doubt it took man many thousands of years to acquire the art of lighting a fire, may not in the lapse of time a second Prometheus arise to teach us also how to kindle the torch of life? Let us not delay his coming by closing our minds to the possibility. 2 1 Compare F. J. Allen's view, as presented by L. L. Woodruff in The Evolution of the Earth and its Inhabitants, 1919, p. 102: "Life at this stage was of the humblest kind, since there were no definite organisms, only diffuse substances trading in energy, and between this stage and the evolution of cellular organisms an immense period elapsed." If this picture of the beginning of life is true to fact, the process was unobtrusive ; probably, if we were shown a specimen of such elementary "living" matter, we should not recognize it as such. All this is in accord with what has been said in an earlier ^ chapter regarding the definition of life. If we continue to use the word life, this is merely a matter of convenience and does not imply any departure from the point of view set forth in the opening chapters. See also p. 19. 218 CARBON DIOXIDE CYCLE 219 Be that as it may, the fundamental fact remains that slow combustion, oxidation as the chemist calls it, is a dominant feature in the physiology of animal life, and that the leading roles in this action are played by the elements carbon and oxygen. In our method of securing our supply of these elements there is a certain dyssymmetry. Carbon we eat in our meals; oxygen we breathe in in respiration. But in function the two elements stand in essentially symmetrical relation; the two together and impartially furnish us with the requisite energy for our life activities. ^ Thus we must regard oxygen as food as much as carbon. This fact deserves a passing note, since it is sometimes stated that assimilation of inorganic food is a characteristic of plants, as distinguished from animals. The statement rests on an arbitrary and wholly gratuitous exclusion of oxygen from our list of foods. It just so happens that there is one item on the animal's menu, namely, oxygen that is gaseous and is spread broadcast; does not therefore have to be hunted and captured. Toward this the animal assumes the same attitude which, presumably, plants adopt toward all their foods: he takes it in unconsiously. This touch of plant nature which we recognize in ourselves should serve to give us a sympathetic insight into the "psychology" of plants. At the same time it reminds us once again of the esentially arbitrary character of the division of organisms into two classes, animals and plants. One and the same organism possesses both animal and plant characteristics, and this is true even of that most highly specialized of ^all animals, the human being. In view of the symmetry in function that exists between carbon and oxygen, and the inseparable relation 2 It is easy to strike a match, but this is merely a way of borrowing tho efforts of others, those who have made the match possible, and those who have manufactured it. How many city dwellers could, by their unaided efforts, start a fire where none was before? Anyone who, in an emergency, may have been forced to attempt the feat will appreciate how among tho ancients "the spark of fire was zealously guarded and soon invested with sacred attributes .... The chief function of the vestal virgins in Homo was to keep the perpetual fire; and in the Catholic church today with its never extinguished light we have the last survival of what was once a social custom " Another curious survival of this custom is quoted by E. A. Seligman (Principle of Economics, 1908, p. 69): "Whenever the location of gas works is changed the fire is transferred by a brand from tho old to the new building. Under no consideration would a new fire bo started." 220 ELEMENTS OP PHYSICAL BIOLOGY in which, they stand in the life processes of the organism, we shall consider jointly, in this chapter, the circulation of carbon on the one hand, and of oxygen on the other. The Carbon Cycle. A very particular interest attaches to the carbon cycle. Carbon is the organic element par excellence, whose absence from any chemical substance stamps this forthwith, by common if somewhat arbitrary consent, as inorganic: whose presence affords the soil ? ,, \ season for the growth of what might be termed the tropical jungle in the domain of chemistry. For in the compounds of carbon nature seems to have run riot, in a revel of creative versatility, as if vying to set a record unapproached elsewhere in all the realm of chemistry, for number, variety and complexity of her children. Other elements 'oxygen, nitrogen, phosphorus, sulphur, iron, indeed play a significant role in life processes; but the indispensable bond that ever links all other ingredients in organic unity is carbon. Furthermore, carbon is preeminently the energy carrier, the standard coin of the organic real, in which both the first cost of installation, of anabolic tissue building, and also the running cost of operation, of metabolism, is defrayed. Indescribably complex far beyond the understanding of the organic chemist of today as are the metamorphoses that carbon undergoes in the economy of the organism, its source and its gate of entry into the organic cycle are comparatively simple. Some two and a half million million tons (2.2 X 1015 kgm.) of carbon dioxide, in the air, and perhaps twenty to twenty-five times this amount contained in the waters of ocean, lakes and rivers, these constitute the store from which all life ultimately draws its supply. Of this vast store, according to an estimate made by C. Engler, 3 about one-thousandth part actually takes part in the cycle of life. The total carbon locked up in living organisms, which would be a measure, in a way, of the spread of life on our globe, is difficult to gage even roughly. One hardly knows how much or how little significance to attach to an estimate by A. G. Hogbom4 that the total quantity of carbon in all living matter is of about the same order as that contained in the atmosphere, namely, 6 X 1011 metric 3 Linck, Kreislaufvorgaxige in der Erdgescliichte, 1912, p. 6; Engler, tJber Zerfalls-prozesse in der Natur. 4 Clarke, Data of Geochemistry, 1920, p. 49. CAKBON DIOXIDE CYCLE 221 tons; an amount which, spread over the entire surface of the globe, would cover it with a film of carbon 1 mm. thick, or with a film of living matter about | inch thick. The organic carbon cycle, reduced to its simplest terms, is a closed chain of three links. Atmosphere / Green Animals* Plants Green plants, under the influence of sun light, absorb C02 from the atmosphere and convert it, with elimination of oxygen, into the many and complex compounds of the plant substance.5 Animals consume plants (directly or indirectly) as food, and in the course of the operations of their typically active lives (as compared with the typically passive, vegetative existence of the majority of plants) they reoxidize the carbon reduced in the photosynthetic plant processes, and return C02 to the atmosphere, thus completing the cycle. In actual fact this simple fundamental cycle is complicated by a number of influences. The decay of dead animals and plants adds a comparatively small item to the discharge of C02 into the atmosphere. Plants are somewhat mor-e resistant to complete decay than animals, and one result of this is the accumulation of notable 6 To discuss here the chemistry of photosynthesis in plants would lead us too far afield. Very important advances have been made recently in this field of biochemistry. It must suffice here to refer to the original literature of which the following articles may be mentioned: E. C. Baly, Photosynthesis, Nature, March 16, 1922, p. 344. Report of discussion on photosynthesis at the British Association Meeting, Nature, December 23, 1922, p. 856. I. M. Heilbron, The Photosynthesis of Plant Products, Nature, April 14, 1923, p. 502. 0. Baudisch, On the Formation of Organic Compounds from Inorganic by the Influence of Light, Science, April 20, 1923, p. 451. 0. Baudisch, The Influence of Light on Inorganic Matter and Life Processes, Jour. Industrial and Eng. Chemistry, May, 1923, p. 451. J. C. Bose, Effect of Infinitesimal Traces of Chemical Substances on Photosynthesis, Nature, July 21, 1922, p. 95. Baly, Heilbron and Parker, Photochemical Production of Formaldehyde, Nature, September 1, 1923, p. 323. J. H. Mathews, Trends in Photochemical Research, Jour. Ind. and Eng. Chem., September, 1923, p. 885. 222 ELEMENTS OF PHYSICAL BIOLOGY quantities of reduced carbon in the form of peat and coal. This process of fossilization is slow, and would not in itself, in any short period, materially affect the carbon cycle. It has, however, fur- /\ nished the occasion for a phenomenon which, judged in a cosmic , ' perspective, represents a purely ephemeral flare, such as must ultimately appear utterly insignificant in the geological calendar, if duration alone is considered; but which to us, the human race in the twentieth century is of altogether transcendent importance: The great industrial era is founded upon, and at the present day inexorably dependent upon, the exploitation of the fossil fuel accumulated in past geological ages. We have every reason to be optimistic; to believe that we shall be found, ultimately, to have taken at the flood this great tide in the affairs of men; and that we shall presently be carried on the crest of the wave into a safer harbor. There we shall view r\ with even mind the exhaustion of the fuel that took us into port, knowing that practically imperishable resources have in the meanwhile been unlocked, abundantly sufficient for all our journeys to the end of time. But whatever may be the ultimate course of events, the present is an eminently atypical epoch. Economically we are living on our capital; biologically we are changing radically the complexion of our share in the carbon cycle by throwing into the atmosphere, from coal fires and metallurgical furnaces, ten times as much carbon dioxide as in the natural biological process of breathing. How large a single item this represents will be realized when attention is drawn to the fact that these human agencies alone would, in the course of about five hundred years, double '-r the amount of carbon dioxide in the entire atmosphere, if no compensating influences entered into play. In point of fact the per- f centage of carbon dioxide in the atmosphere exhibits remarkable I constancy and there are several very large items, in addition to those already touched upon, both on the ingoing and outgoing side ' of the account. The case of man has been singled out for mention here merely because our knowledge of the human population and economy enables us to make a reasonably close estimate of his contributions. The quota supplied by the remaining animal species can hardly even be guessed at. But probably the greatest source of atmosphere C02 are volcanoes and mineral springs. Cotopaxi alone has been credited with an annual discharge of two million 4 tons of the gas. *- * [ CAEBON DIOXIDE CYCLE 223 On the debit side there is first of all the item of consumption by plants. E. H. Cook, 6 from very uncertain data, computes that leaf action alone more than compensates for the production of carbon dioxide, consuming about one-hundredth of the total atmospheric oxygen in a year. Yost7 computes that if the entire land area were planted with sun flowers, about 6.5 X 1011 tons of CO2 would be absorbed per annum. Forests would be considerably less efficient, and would take care of about 2.8 X 1010 tons per annum, or, say in round numbers one-hundredth of the atmospheric carbon dioxide. An older estimate, by Liebig, puts the annual output of the soil of Central Europe at 2.5 tons of dry organic matter per hectar, or, say 1 ton per acre. Allowing 40 per cent carbon in such organic matter we find for [the total annual production of carbon in plants 13,000 million (1.3 X 1010 ) tons. This is about ten times the world's annual coal consumption, and about one-fiftieth of the total carbon in atmospheric carbon dioxide. Arrhenius points out that if all this carbon fixed by plants were deposited in peat bogs, the atmosphere would be depleted in half a century. But, of course, only a small proportion of the bodies of plants are thus "horded" and removed from the organic life cycle. A figure of perhaps greater interest, because based upon observations of processes actually going on in a selected portion of the universe, is given by W. R. G. Atkins. From the observed change in the hydrogen ion concentration in the water of the English Channel, this author has calculated that 250 metric tons of organic carbon (figured as hexose) were produced per square kilometer between July and December. From similar observations made at Port Erin, Moore found a production of 300 metric tons per square kilometer during the six months that included the vernal maximum, of diatom production. 8 An important item among the withdrawals from the atmosphere is the absorption of carbon dioxide in the weathering of rocks, with replacement of silicates by carbonates. A. G. Hogborn reckons this item as about balancing the reproduction of carbon dioxide in the F. W. Clarke, loc. oit., p. 48; Phil. Mag., 5th ser., vol. 1882, p. 387. 7 Pflanzenphysiologie, 1913, p. 151. 8 Journal of Marine Biol. Assoc. October, 1922, vol. 12, no. 4, Nature, January 27, 1923, p. 132. 224 ELEMENTS OP PHYSICAL BIOLOGY combustion of coal. Its accumulated record is seen in the sedimentary rocks, which, according to F. W. Clarke, 9 contain 30,000 times as much as C02 as are today present in the atmosphere. 10 Sterry Hunt "illustrates the effect of weathering by the statement that the production from orthoclase of a layer of kaolin (china clay) 500 meters thick and completely enveloping the globe would consume 21 times the amount of C02 now present in the atmosphere." Chamberlin and others estimate that it would take about 10,000 years to consume the present amount of atmospheric C02 by the weathering of rocks. Loss of C02 by peat formation may be estimated at the same figure. The formation of COa by the burning of coal would, according to these estimates, cover the loss by weathering and peat formation combined, seven times over. Finally, there is the great reservoir of the ocea, in equilibrium with the atmosphere, and absorbing, under present conditions, some 18 to 25 times as much C02 as it leaves in the air above it. Thus the sea acts as a vast equalizer; of every ton of C02 thrown into the atmosphere by volcanoes, or by coal fires, for example, the ocean ultimately receives directly or indirectly, about 1900 pounds, only the balance of 100 pounds remaining in the atmosphere. It is thus seen that even extensive contributions from the lithosphore have but a slight effect upon the atmospheric store, and fluctuations are in this way ironed out and moderated. Arrhenius11 points out, moreover, that at the present time the carbon dioxide content of the air over the ocean is on an average 10 per cent lower than over land. From this, and the fact that generation of C02 by coal (and probably also from volcanoes) has in late years been increasing, he concludes that the air is, at the present epoch, becoming richer in this gas. 8 Loc. cit., p. 48. See also C. Shuchert, The Evolution of the Earth and its Inhabitants (Yale Press, 1919), p. 52. 10 Hogbom's figure, quoted by Arrhenius (Worlds in the Making, 1908, p. 54), is 25,000 for limestones and dolomites. Am. Jour. ScL, 3d ser, 1880, vol. 19, p. 349. Clarke, loc. cit, p. 48. 11 Loc. cit., p. 54. Arrhenius' figure differs somewhat from the one given above. He supposes that the sea takes up five-sixths of the COZ thrown into the air, i.e., 1 ton would yield up 1667 pounds to the ocean, leaving 333 pounds in the air. ft CARBON DIOXIDE CYCLE 225 As to which side of the account shows a net balance, in the carbon cycle, we have no certain knowledge. Arrhenius builds his conception of the future industrial development of our race on the expectation that the atmosphere is gaming in carbon dioxide, under the present regime of "evaporating" our coal mines, as it were into the air. On the other hand, if our atmospheric C02 is of volcanic origin, and the balance is maintained today with the aid of discharge from the lithosphere, then the ultimate extinction of the earth's plutonic fires would bring in its train the depletion of the atmosphere and secondarily the extinction of life. "The cessation of volcanism would signify the end of life on the globe." A similar position is taken by C. Schuchert, 12 who further remarks: We should add that if there were again as much life as there is at present, all the carbon of the atmosphere would be in the living plants and animals, and, if such a condition were possible death would come to them all .... Life and its abundance at any time are conditioned by the amount of this gas (COt) present in the atmosphere. This remark of Schuchert's is suggestive as illustrating in concrete manner the relative amounts of carbon concerned in the life balance. It is, perhaps, somewhat misleading in making no mention of the equalizing influence of the ocean which has been noted above. In point of fact, if all the C02 in the air were withdrawn, a nearly equal amount would rise from the ocean to take its place. A summary, in graphic form, of the principal relations in the carbon cycle noted in the preceding paragraphs, will be found in figure 47, which should aid in giving a comprehensive picture of the situation. < ; The Oxygen Cycle. The organic oxygen cycle is, of course,, directly related to the carbon cycle, although other features also enter into operation in regulating the oxygen balance of the atmosphere. The complementary relation between animals (essentially oxidizors of carbon) and plants (essentially reducers of carbon dioxide) is indeed a biological fact of fundamental importance at the present stage of evolution. But if we look back through the vista of ages, to the time before the advent of life, such as we^know it, our curiosity is aroused as to the origin of the atmospheric carbon i The Evolution of the Earth and its Inhabitants, 1919, p. 52. 226 ELEMENTS OP PHYSICAL BIOLOGY H O o NA B W w tJ W ft o o e ! t-3 P O M O (JABEON DIOXIDE CYCLE 227 dioxide and oxygen. Various views have been upheld on this subject. F. W. Clarke13 remarks: It is likely that carbon dioxide has been added to the atmosphere by volcanic agency, in some such manner as this: Primitive carbon, like the graphite found in meteorites, a,t temperature no greater than that of molten lava, reduced the magnetite of igneous rocks to metallic iron, such as is found in many basalts, and was itself thereby oxidized. Then, discharged into the atmosphere as dioxide,, it became subject to the familiar reactions which restored it to the lithowphere a,s coal or limestone. Arrhonius, 14 referring to Koehno's reflections on this subject, points out that the atmosphere contains about 1.2 X 101 ! 5 tons of oxygen, an amount which roughly* 6 corresponds with the mass of fossil coal in the sedimentary rocks. "The supposition appears natural, therefore, that all the oxygen of the air may have been formed at the expense of atmospheric carbon dioxide. Probably all the oxygen of the air owes its existence to plant life." F. W. Clarke resumes the views of a number of investigators as follows: 10 C. J. Koehne assumed that the primitive atmosphere contained no free oxygon, and he has boon followed by T. L. Plupson, 17 J. Lemberg, 18 J. Steven- son, 10 and Lord Kelvin." Lomberg and Kelvin, however, do not go to extremes, but admit that possibly Homo free oxygen was present even in the earliest times. Lemberg argued that the primeval atmosphere contained chiefly hydrogen, nitrogen, volatile chlorides, and carbon compounds; the oxygen which is now free, being Mum united with carbon and iron. The 13 F. W. Clarke, loc. oil., p. 55. "Worlds iu the Making, 1908, p. 58. 111 The correspondence is rather distant if we accept Engler's estimate of the world's coal reserves, namely, !J X 10 1S tons, containing 75 per cent carbon.. Hoc Lin ok, loo. oil;., p. 37, Kngler'H estimate is probably low. The World Altnanao, 1921, p. 201., given 7.5 X H) n! tons. This would correspond to 1.5 X 10 13 tons oxygon, as against 1.2 X ID 11' tons in the atmosphere. It is true that these ostinmteM of coal reserves cover only such coal as it would pay to mine. F. W. Clarke, loc. oil;., 1021, p. 50. 17 Chom. News, ISO.'J, vol. 07, p. i:?5. Also several notes in vols. 68, 69, and 70. For Koohno'n work wee PhipHou'n papers, 1893-1894. "Zeitsohr. Deutsoh, gool. (lenell, 1888, vol. 40, pp. 030-634. I'PhiloH. Mag., 1900, 5th ser., vol. 50, pp. 312-,'JOO; Oth ser., 1902, vol. 4; p. 435; 1905, vol. 9, p. MS; 1900, vol. 11, p. 220. * Ibid., 1899, 5th Her., vol. 47, pp. 85 89. 228 ELEMENTS OF PHYSICAL BIOLOGY liberation of oxygen began with the appearance of low forms of plant life, possibly reached a maximum in Carboniferous time, and has since diminished. Stevenson's argument is much more elaborate, and starts with an estimate of the uncombined carbon now existent in the sedimentary formations. In the deposition of that carbon, oxygen was liberated, and from data of this kind it is argued that the atmospheric supply of oxygen is steadily increasing, while that of carbon dioxide diminishes. The statement that no oxygen has been found in the gases extracted from rocks is also adduced in favor of the theory. First, an oxidized crust and no free oxygen in the air; then processes of reduction coming into play ; and at last the appearance of lower forms of plants, which prepared the atmosphere to sustain animal life. The arguments are ingenious, but to my mind they exemplify the result of attaching excessive importance to one set of phenomena alone. It is not clear that due account has been taken of the checks and balances which are actually observed. At present the known losses of oxygen seem to exceed the gains. For example, C. H. Smyth21 has estimated that the oxygen withdrawn from the air by the change of ferrous to ferric compounds, and so locked up in the sedimentary rocks, is equal to 68.8 per cent of the quantity now present in the atmosphere. G. Bunge 22 also supports the view that atmospheric oxygen is continually diminishing, becoming bound by the ferrous oxide resulting from the decomposition of silicates. Accumulation of carbon dioxide in the atmosphere, at any rate under present conditions, is also assumed by S. Arrhenius, as has already been remarked.23 21 Jour. Geology, 1905, vol. 13, p. 319. 22 Text book of Physiological and Pathological Chemistry, 1902, pp. 16-17. 23 See Jour. Franklin Inst., 1920. vol. 190, pp. 114-121. CHAPTER XVIII THE NITROGEN CYCLE If the denuuul becomes inHiHteut enouKh, wo cannot doubt that methods will be dovimul which mil Kiv us the desired results. To question that would bo to admit thai; man haw nearod the culmination of his evolutionary career and is preparing to bequeath the iwwtery of the earth to hia successor whoever that may be.' (7. W. Martin, ' Natural Demand and Supply. The proportion of nitrogen to carbon in the human body IB 1 :3, in the atmosphere it is 5,500: 1. A human adult contains in IUH body about 42 pounds of nitrogen, and over 50 pounds of curium. Over every square foot of the earth's surface rifles a column containing Homo- .1500 pounds of nitrogen, and only about. 1/4 pound of carbon. The demand and the supply of these two element appear, therefore, at first sight, to be altogether out of all proportion favorable to nitrogen. Yet, in point of fact, the practical problem of Heeuring an adequate supply for the substance and expansion of life w incomparably more complex in the case of nitrogen than in the cawo of carbon. The reason for this somewhat remarkable, inversion in to bo noon in the fact that nitrogen is readily aecoHsibio an food for living organisms only when it occurs in certain chemical combinations, and nitrogen thus combined is far from plentiful. It has I een estimated by T. II. Norton that this available or "nomadic." nitrogen -i.e., that which taken part in the migration through the organic, cycle -amounts to only about two one-millionths of the total nif.rogen of the atmosphere, or, way, to about 8 X 109 tons. In fact, njUrogon w today probably the chief of those limiting factors' which, in accordance with Liobig's law of the minimum, establish the bounds for the extreme expansion of living matter upon the earth. At the name time the circumstance of the chemical idiosyncrasies of the element nitrogen introduces a certain complexity into the nitrogen cycle, which strikes the eye at a glance in the charts, figures -18 and 40, exhibiting the essentials of the nitrogen 1 Compare ("}. Bunge, I'liymolotfioal and Pathological Chemistry, 1902, p, 17; Grinmsll Jharit\ , Nftrogan Nitrogenous Animal Compounds! Urea Ammonia KlWH in hrondor outline the main feature of the oycki, while figure -ID cx!nl)i(,,s in greater detail especially those stages in the eyde UuU. am muni, iudijuately aKsociated with life agencies. 2 '' For dcituilH (in UUH ])linH<> of the milijocfc the reader must be i-oferred to Mio Hpocutl liUu'iil.iinv A. good Hiinunary, fairly detailed and complete, yot coticiHO, will IHI found in [{ llubor, Zur Sfcickstoff-Frage, Born 1908 pp. 1-10. 232 ELEMENTS OF PHYSICAL BIOLOGY Gate of Entry into Nitrogen Cycle, The natural gateway for the entry of atmospheric, elementary nitrogen, into the organic cycle is a narrow one. So far as at present known, only a limited class of organisms possess the faculty of "fixing" this element, that is, taking it in its gaseous state from the atmosphere and converting it into the condensed (liquid or solid) form, in which only it has common acceptation as coin of the organic realm. The organisms known to take part in this natural process of nitrogen fixation are three, namely certain bacteria having their habitat in the soil; certain leguminous plants (peas, beans, clover, alfalfa), working in conjunction, in symbiosis, with nitrogen-fixing bacteria lodged in tubercles upon their roots; and, thirdly, the wheat plant has recently been shown to possess the independent faculty of assimilating nitrogen from the air. This recent demonstration, 3 of course, suggests the ready question whether after all, a number of other plants may not be similarly endowed. This remains as a matter for further investigation, but it is improbable that we shall have occasion to change materially our present impression, namely, that the natural avenues by which elementary nitrogen gains admission from the atmosphere into the cycle of life are rather narrowly restricted. As to other avenues opened up by the man, these will be considered presently. Leak of Nitrogen out of Circulation. While there is thus a narrowly restricted class of vegetable organism through which nitrogen trickles in a thin stream from the elementary supply in the atmosphere into the life cycle, the majority of plants derive the supply for their biological needs from ready formed nomadic nitrogen in the soil, that is to say nitrogen combined in the form of ammonium salts, nitrites and nitrates. These substances are subject to oxidation and reduction in the soil under the influence of various bacteria, as indicated in the chart figure 49. The result of these changes is that a certain fraction of the nomadic nitrogen is continually leaking out of the circulation and joins the general reservoir of free nitrogen in the atmosphere. This is only one of a number of items on the losing side of the balance sheet. Other items will be found in following up the details of the two charts already 3 C. B. Lipman and J. K". Taylor, Science, November 24, 1922, p. 605. These authors report that in their experiments wheat plants assimilated 13 to 21 per cent of their nitrogen content from the air. NITROGEN CYCLE 233 referred to. There is loss in the autumnal leaf fall of deciduous plants; in the decay of dead plants, or in their fossilization as peat, lignite and coal. Forest fires, and the burning of wood and coal; the distillation of coal for illuminating gas; the oxidation of coal in metallurgical furnaces, the coking of coal in ovens of the so-called beehive type; all these are operations in which a greater or less proportion of the combined nitrogen in the coal is liberated into the air in the free, unavailable form. In view of the great loss which this represents in the economy of our food resources, the highest importance attaches to the modern drift away from the beehive coke oven to the by-product oven, in which the major part of the nitrogen in the coal is recovered as ammonia. TABLE 22 Fraction, of total output of coke in the United States, produced in by-product ovens These by-product ovens were introduced in 1893. It is estimated that during the period from 1893 to 1910 alone, through the cont Limed use of the old beehive type coke oven, over 9,300,000 tons of ammonium sulphate were wasted, representing, at the prices then prevailing, a value of 553 million dollars. In addition to this must be reckoned a further loss in the resulting field crops. Had all the nitrogen wasted in the beehive ovens been spread as fertilizer on the field, this would have increased the crops some 20 per cent.4 An idea of the extent arid significance of the healthy modern drift towards replacement of the beehive by the recovery coke oven may be gathered from table 22, reproduced from an article by Grinnell Jones in the Quarterly Journal of Economics, 1920, vol. 34, p. 402. H. E. Fischer, writing in the Journal of the Franklin Institute, 1920, vol. 190, p. 191, remarks that if all the coal in the United States were used as coke, and the ammonia recovered in the process, this alone would 4 This and other data regarding nitrogen losses here set forth are drawn, largely, from an article by J. D. Pemiock in the Journal of Industrial and Engineering Chemistry, 1911. 234 ELEMENTS OF PHYSICAL BIOLOGY furnish one million tons of ammonia, which corresponds to about one-half the world's total production of nitrogen compounds. Returning to the chart (fig. 48) and continuing to trace the progress of nitrogen in the organic cycle, we note next that combined nitrogen is absorbed from plants by animals in their food. It is rejected from the animal economy in part as excretory matter (manure, etc.), in part in the bodies of dead animals, in so far as these are not themselves consumed as food. A large item here, in the economics of the human community, is the refuse from slaughter houses. Certain portions of this are recovered for various uses (glue, leather, etc.). Some is made into fertilizer. Much of it goes to waste, and thus gives opportunity for another leak of nitrogen out of the life cycle to the elementary form in the atmosphere. It is difficult to form any estimate of the extent of this loss, but there can be no doubt that it represents a waste of hundreds of tons of nitrogen daily. Much also is lost from the other item of animal waste materials, not a little of the loss being occasioned by modern methods of sewage disposal in large cities. Such methods represent, from the standpoint of agricultural economy, a luxury, which however, will be thought worth the price if the means are at hand to make good the loss from other sources. Those portions of animal refuse which are placed on the soil of crop-bearing fields and pastures return, at least in part, into the organic cycle. Accessory Sources of Combined Nitrogen. It is of course absolutely essential for the continuance of the life cycle that the losses of combined nitrogen which have been noted should in some way be compensated by equal or greater accessions to the total amount of nomadic nitrogen. One source of such compensating revenue has already been noted, namely the direct assimilation of elementary nitrogen from the atmosphere by a narrowly restricted class of plants. There are two other natural sources. Volcanoes and furnaroles belch notable quantities of ammonium chloride into the air; nitric acid is also formed by the action of lightning, while ammonia is produced by the passage of the silent electric discharge (aurora) through the atmosphere. Arrhenius5 estimates that the amount of nitrogen annually bound in this way amounts to about 1.4 X 109 B S. Arrhenius, Worlds in the Making, 1908, p. 144. See also Haber, Zeitschr. f. Angev. Chemie, 1910, p. 685. NITEOGEN CYCLE 235 metric tons, or one part in 3 millions of the total atmospheric nitrogen. The products are washetl into the soil by the descending rain, together with more or less of the same substances that have escaped into the atmosphere from the ground and are thus restored to the soil. Estimates which have been made of the quantities involved 3.6 I .8 O oo IB30 6O TO WOO /OSO 90 YEAR. FIG. 50. THE RISE OF THE SALTPETER INDUSTKY SO 30 are somewhat conflicting, but on the whole the gains of the soil in this way are held to exceed its losses.6 The stages and agencies so far reviewed may be collectively designated as those constituting the "natural nitrogen cycle," as distinguished from a group now to be considered, which are charac- 6 F. W. Clarke, loc. cit., 1920, p. 52; Linck, Kreislaufvorgange, 1912, pp. 6-7. It has also been put forward (Sch.dn.bcin) that a certain amount of nitric acid is formed in the evaporation of moisture from the earth (Bunge Physiological Chemistry, 1902, p. 11). But this is doubted by Ostwald. (Grundlinien der Anorganischen Chemie, 1912, p. 384.) 236 ELEMENTS OF PHYSICAL BIOLOGY terized by human interference with the course of nature. It Is hardly necessary to point out that such a distinction between natural and artificial agencies is merely a convenient use of brief terms; the fact must never be lost sight of that man himself is very essentially part of nature, and that his development, whether physiological, psychological, sociological, economic, or what not, is part of the great process of nature. Human Interference in Nitrogen Cycle. Man's earliest conscious, purposive intervention in the nitrogen cycle dates from antiquity, and primarily consisted merely in taking more or less pains, in an empirical way, that the nitrogenous waste material of animal economy be, as far as possible, restored to the soil. Perhaps the first recorded use of fertilizers not derived from current wastes of domestic animals is the exploitation of guano by the Incas, which dates from antiquity, and was brought to the notice of Europe by de la Vega in 1604. It seems to have aroused no interest until attention was again drawn to it two hundred years later by von Humboldt and by Justus Liebig, and large scale importations of guano into Europe began soon after this. A greater event in the history of agriculture was the opening up, in 1831, of the Chilean nitre beds. Without this source of saltpeter the modern development of intensive agriculture, and the consequent growth of population in all civilized countries, would have been at the least greatly hampered. The rapid rise of the saltpeter industry is clearly exhibited in table 23 and the corresponding graph figure 50. While our chief interest here is in the agricultural use of Chile saltpeter, its consumption in the industries is altogether too extensive to be passed by without mention. J. D. Pennock7 gives the figures shown in table 24 for the relative amounts of saltpeter consumed in different uses. It should be observed that Pennock's figures relate to peace time conditions. Even so, nearly one-half the consumption is taken up in the manufacture of explosives. Nitrogen thus employed is, of course, lost to the life cycle. A certain loss also concurs in the refining of the caliche (native saltpeter), and in the production of nitric acid and sulphuric acid8 therefrom. 7 J. D. Pennock, Jour. Industr. and Eng. Chem., 1911, p. 172. 8 When manufactured by the Chamber process. NITROGEN CYCLE 237 TABLE 23 Growth of the saltpeter industry (III) Nitrogon on basin of 15.05 por con I 17.5 3,498 40,230 156,339 233,334 287,207 410,095 478,230 424,900 302,850 502,370 519,570 496, 120 The figures in column I are the Chilean nitrate production, as given by Parsons and Petit, Brokers. The figures in oolxims 11 and III, from 1831 to 19 11 inclusive, represent the World's consumption of saltpeter according to C!(5ni Civil, vol. 62, p. 192. The figures from 1913 to 1918 in oolums II and II I ropi'eserit the total production of Chilean and Indian nitrate, according to Griunell Jones, Jour. Frankl. Inst., 1920, vol. 134, p. 398. The precipitous drop in the Chilean production in 1915 was due to a blockade established by the GermariH during the early stages of the, World War. See Fig. 50, in which circles indicate production, the drawn out curve consumption. TABLE 2t Distribution of Chili saltpeter consumption in the United States in 1010 among different uses In manufacture of fertilizer. In manufacture of dyestuffs. In general chemistry In glass In explosives In nitric acid In sulphuric acid Unaccounted for 13 12 10 4 41 9 100 238 ELEMENTS OF PHYSICAL BIOLOGY Origin of Nitre Beds. The origin of the nitre beds is uncertain. The presence of boron in the deposits, and the association of this element with ammonia in volcanic emanations, have been regarded by some as evidence that the saltpeter is of ultimately volcanic origin. Others have ascribed it to organic sources, such as altered guano deposits. But whatever be their origin, this is certain, that the saltpeter beds represent an accumulation of ages, and that the present rapid rate of consumption is out of all proportion with the rate of formation of the deposits. In other words, here, as in the case of coal, we are living on our capital, and must prepare ourselves for its impending exhaustion.9 It is true that our other sources of combined nitrogen notably ammonia from coke ovens supplement our drafts upon the nitre beds, and thus help to defer the day of scarcity. But coal itself is a limited stock, and other sources of combined nitrogen seem quite inadequate for the needs which we have developed under the stimulation of temporarily bountiful supplies. It is a peculiarity of living substance that in times of plenty it tends to grow beyond the bounds compatible with ultimate stability; it overshoots the mark so to speak; the curve along which it approaches its equilibrium is very apt to be humpbacked, or it may be oscil- latory. 10 The prospect of a period of actual diminution (not mere marking time) to follow upon a period of exuberant prosperity, is one that an organism gifted with foresight must look upon with disquietude. Such foresight may, then, lead an organism so gifted, to make efforts to provide for untoward future exigencies, either by laying by supplies, in times of plenty, for times of stress; or by devising means, if possible, to increase, by new measures, the supplies which, under the old regime, would presently fall short of requirements. Man has not always made a display of brilliant foresight, but in this instance, in making ready for the exhaustion of the nitrate supply, he has taken time by the forelock, and all indications are that long before the emergency arises he will have made himself _ 9 The probable date of this exhaustion has been variously estimated. Little value can be attached to positive statements. More significant, perhaps, is the negative report made in 1913 to the Chilean Government by the Inspector General of Nitrate Deposits: "There is no fear of the Chilean nitrate deposits being exhausted for two hundred years" (Grinncll Jones loc. cit., p. 401). ' "Compare what has been said on this subject in Chapter XI. NITROGEN CYCLE 239 ready to meet it. For the last decade has seen the development, to full industrial capacity, of several processes for the fixation of atmospheric nitrogen, its conversion into compounds directly or indirectly adapted to enter the cycle of nomadic nitrogen. For details regarding these modern industrial developments the reader must be referred to the technical literature. 11 It must suffice to indicate here very briefly the nature of the several processes. 1. The Birkeland and Eyde Process, is essentially man's imitation of the production of nitric acid by lightning. Air is passed through an electric arc fanned out into a broad disc by a magnetic field. The process is commercially viable only where very cheap power is available, and has been developed mainly in Scandinavia, with the use of water power. 2. The Cyanamide (Frank and Caro) Process effects the absorption of atmospheric nitrogen by calcium carbide in the electric furnace. The product can be employed directly as a fertilizer, or can be made to yield ammonia and other nitrogen compounds. 3. The Haber Process effects the synthesis of ammonia from nitrogen and hydrogen under pressure (100 to 200 atmospheres) in the presence of a catalyst. An allied process is that of Claude, which works at very high pressure (1000 atmospheres). ia 4. The Biicher Process, which has not yet passed beyond the experimental stage, yields cyanides; these can also, if the market warrants it, be made a source of ammonia. A highly significant development is the union of the Habcr ammonia process with the Solvay process, whereby the carbon dioxide obtained as a waste product in the manufacture of the hydrogen for ammonia synthesis, is utilized in the production of sodium carbonate; while, on the other hand, the formation of large quantities of the nearly worthless calcium chloride waste of the Solvay process, as ordinarily conducted, is avoided. Inasmuch us "soda ranks second only to sulphuric acid among all chemicals in magnitude of output (1,390,628 short tons in the United States in 1918) and fundamental importance, .... this (combination of the Haber and the Solvay processes) may well prove to be the most 11 Sec for example the articles by G. H. Fischer and Grinnell Jones already cited. 12 H. E. Fisher, Jour. Franklin lust., 1920, vol. 190, p. 201. 240 ELEMENTS OF PHYSICAL BIOLOGY 1,6 FIG. 51. THE RISE OF THE FIXED NITROGEN INDUSTRY NITROGEN CYCLE 241 significant development in industrial chemistry of the present decade."13 5. The Ostwald Process, A subsidiary process bridging the gap from the product (ammonia) of the processes of the Haber and Frank and Garo types, to the market requirements of nitric, acid (nitrate and nitrites), is the Ostwald process for the catalytic oxidation of ammonia. The Meteoric Rise of Nitrogen Fixation Industries. In the period during arid immediately following the World War the situation in the nitrogen industries was abnormal, production being temporarily activated to fever heat, inasmuch as nitrogen compounds are among the most indispensable of war materials. Tims it came about that the development of nitrogen fixation had for its immediate motive not so much the constructive spirit of the arts of peace, providing for the future needs of men, as the malice and forethought of the conspirators of war. The conflict left on our hands, upon the conclusion of the armistice, both completed and unfinished manufacturing plants in excess of immediate needs in times of peace. Legislative difficulties also hampered well-designed efforts to convert these plants to industrial use. These arc temporary conditions; although one may not be able to foresee exactly how, in detail, these industries will finally adjust themselves, there, can be little doubt that from now on synthetic nitrogen compounds will continue to be drawn in increasing amounts from the atmosphere into the life cycle. The phenomenal growth of this infant industry within the past ten or twelve years is forcibly brought out in the graph (fig. 51) and the corresponding table 25. It will bo observed that in 1909 only about 1 per cent of the world's needs in combined nitrogen were satisfied from the new-born industry. In .1.917 its contribution had swollen to 30 per cent, and by 1920 the capacity of existing plants was adequate to furnish 43 per cent of the world'n requirements. This extraordinary development is something much more than a fundamental new departure in industry. It represents nothing lens than the ushering in of a new ethnological era in the history of the human race, a new cosmic epoch. In the short span of a dozen years 'geologically speaking in an instant- man has initiated transformations literally comparable in magnitude with cosmic 13 Grinnell Jones, loc. cit., p. 414. 242 ELEMENTS OF PHYSICAL BIOLOGY NITEOGBN CYCLE 243 processes. Accepting Arrhenius' liberal estimate of the total quantity of combined nitrogen washed down to the soil in the annual rain fall over all continents of the globe, namely 400 million tons, it is seen that the new industry even now is capable of furnishing a supplementary supply equal to one six-hundredth of this prodigious quantity. 14 Economic and Energetic Significance of Concentration. We are, of course, greatly more interested in this six-hundredth which is under our control 'and of which a due proportion falls, in consequence, upon our fields in concentrated form 'than in the very much larger quantity that nature scatters with sublime indifference on stony places and good soil alike. This is just one of those cases to which reference has already been made in a general way. It is not so much the quantity of the material provided by nature that counts, as its accessibility; and accessibility here means, among other things, suitable concentration. This question did not so obviously project itself into the discussion of the carbon cycle, because the __ natural source of carbon is atmospheric carbon dioxide, which, being a gas, in the very nature of things spreads evenly, and presents itself unsought, by a spontaneous process, at the mouth of the hungry plant. But the combined forms of nitrogen are for the most part solids or solutions, occurring in definitely localized amounts of greatly varying concentration. The labors forced upon us in our efforts to satisfy the nitrogen needs of our fields are, to be precise, not primarily work of production, but virtually work of concentration; or to be more exact, work of bringing about concentration at the particular locality where it is wanted by transportation if need be. It is only because we find k easier, in some instances, to produce than to concentrate existing supplies, that we elect the former expedient; just as we may prefer to feed a boiler with a fresh supply of water, rather than to u For land and sea together Arrhenius estimates 1500 million tons of nitrogen in the rain fall. Note added in correcting 1 proof. Since the writing of this chapter there have become available Trade Information Bulletins No. 220 and 240 of the U. S. Department of Commerce, which give further and more recent data. In Bulletin 240 J. M. Braham estimates the capacity of the world's nitrogen fixation plants at 490,000 tons for 1923. The reader interested in this topic may also consult J. R. Partington, The Nitrogen Industry, publiBhcd by Constable, 1924. 244 ELEMENTS OF PHYSICAL BIOLOGY return to it the condensed exhaust from the engine. That the mere concentration of existing supplies should at all require the doing of physical work is a circumstance of particular interest, not only in its economic relations, 13 but also, and quite particularly, from the standpoint of energetics. This is a matter that will duly engage our attention in a later section, devoted to the energetics of the several processes that have here been considered in their purely material or stoiehiometi'ic aspect. Meanwhile it is interesting to observe that such localized sources of concentrated supplies as those presented in the Chilean nitre beds virtually function as centers of attraction toward which gravitates a stream of human beings 'Or their representatives in the form of ships and other conveyances arriving in search of cargo and going out laden with material. To an ultramundane observer who should survey the scene in suitable perspective, the activities around the nitre beds must appear very like the busy swarming of a colony of ants around the treasure trove of some silvan inhabitant departed this life; who, having completed his earthly career, is now yielding up, in the dissolution of death, such energies as still remain locked up in the carcass. Attractions such as this are, in a sense, merely apparent; they are the outward symptoms of a complicated chain of cause and effect10 characteristic of the behavior of living organisms. Yet they are often so consistent in their action that it would not be unreasonable to essay a systematic treatment of the movements in a world comprising such centers of attraction and such moving pawns, on the basis of brute tropisms unanalyaed into their ultimate component agencies. Here it must suffice to have pointed out that our highly complex industrial system, our far-flung intricate network of lines of traffic by land and sea, is but a sublimated copy, on a heroic scale, of the hustle and bustle that is going on all around us in nature, in response to attractions, tropisms, determinants of the 15 A striking illustration of this is cited by Haber (Zeitschr. f Angew Chemie, 1910, I, p. 685). If the gold in sea water were extracted and" apportioned evenly to all the human inhabitants of the globe, we should all be millionaires three times over; yet it does not pay to as much as begin this extraction. _ 15 Commonly accompanied by that anticipatory inversion of the sequencein time, of effect and cause, which is the earmark of purposive action. NITHOGEN CYCLE 245 moves of an army of checkers over the mosaic of the earth's topography. 17 Total Circulation Tends to Increase. The study of the nitrogen cycle furnishes us with a first occasion to take note of a phenomenon the full significance of which will become apparent in dealing with the dynamics of evolving systems. It is to be observed that the general trend of man's effort, especially in this new epoch of nitrogen fixation, has been towards drawing into the organic circulation a greater amount of matter, enlarging the wheel of the mill of life, so to speak. There can be little doubt that this trend will continue and increase in the future, and that it is the expression of one aspect of a general law; 18 the other aspect of this law, and its full significance, must be reserved for later discussion, as already intimated. 17 For a discussion of the natural concentrating processes the reader may be referred to the following articles: A. C. Lane, Nature's Coneentraiors, Engineering and Mining Journal, 1897, vol. 03, p. 54-2. ,1. C. Russell, Concentration as a Geological Principle, Bulletin Ccol. 8oc. An., 1907, vol. IS, pp. 1-28. E. Blackweldcr, The Geologic Role of Phosphorus, Aia. Jour. Sci., 1910, vol. 62, p. 285. W. Lindgren, Concentration and Circulation of the Elements from the Standpoint of Economic Geology, Economic Geology, 1923, vol. IS, pp. 419-44.2. 18 The phenomenon is, of course, closely related to that In which R. Luscaux refers as "unc propriete particuliere do la vie: cclle do rextentiion" (La Production ct la Population 1921, p. 37). ftcc also A. J. Lotka, I'roc. Nat 'I Acad. Sci., 1922, p. 47. CHAPTER XIX THE PHOSPHORUS CYCLE There is no coming into being of aught that perishes, nor any end for it .... but only mingling, and separation of what has been mingled. Empedocles. Immobile Elements. The circulation of water, carbon dioxide and oxygen in nature is greatly assisted by the freely occurring processes of evaporation, condensation (rainfall) and diffusion. In the case of nitrogen these processes still give some aid, as in the distribution broadcast of atmospheric nitrogen, and in the formation j. and precipitation of nitrogen "fixed" by lightning, etc. In phosphorus we have, on the contrary, a typical example of the inherently immobile elements needful to the living organism to adopt Liebig's phrase (fur sich nicht beweglicli) . The successive steps in the concentration, diffusion, and reconcentration of this element, as available for the substance of the organism, accordingly display a characteristic complexity. Some of the principal items and steps in the phosphorus cycle are set forth in diagrammatic form in figure 52. Natural Phosphorus Supply of Soils. The virgin soil contains, in general, a certain natural supply of phosphates. So, for example, Van Hise1 reports that the virgin soil of Ohio, Illinois and Wisconsin contained, to a depth of 8 inches, 2077 pounds of PaOg per acre. / After fifty-five years of cultivation this figure had sunk to 1813 pounds per acre, a loss of 36 per cent. These figures show the extreme importance of a conservation of our resources of phosphorus. The loss probably occurs partly through erosion by rain water charged with carbonic acid, which dissolves phosphates in the soil and in rocks, and ultimately "washes a certain proportion out to sea. To this unavoidable loss, however, is added a large item of preventable loss through our failure to ensure that the phosphorus of animal wastes be returned to the soil. So, for example, farmyard manure contains over three-fourths of the phosphorus in the feed and bedding supplied to the animals. It is therefore very essential that this be returned 1 Ann. Acad. Polit. Soc. Sci., 1909, vol. 33. . , 246 PHOSPHORUS CYCLE 247 o o W FM 248 ELEMENTS OF PHYSICAL BIOLOGY to the soil as completely as possible. Of the one-fourth of the phosphorus fed to the animals, and not accounted for in the manure, a considerable fraction appears in the bodies of these animals, especially i in the bones. These, then, also should find their way back to the * soil, as they do to some extent through the practice of using bone meal, either as such, or after conversion into superphosphate, 2 as fertilizer. This practice is materially assisted by the modern methods of meat production on a large scale, with very complete utilization of by-products. Leakage of Phosphorus from Circulation. The human cadaver is in the great majority of cases returned to the soil in the regular course of events, although under conditions which, obviously do not render it very readily available for crop production. An adult contains about 1| pounds of phosphorus, or 3.4 pounds IW If we allow one-half of this for a "unit of population," i.e., 1.7 pounds 4 P2 6 , with a death rate of 1.3 per cent per annum, we find that the ^ amount of P2 5 annually committed to the cemeteries of the United States is about 1105 tons. This is about the equivalent of 3300 tons of phosphate rock, or about one-thousandth of the annual production of that material in the United States. But a very much larger amount of waste is occasioned from the human population by the practice of running the sewage from cities into rivers and thus to sea. Van Hise estimates that annually 400,000 tons P2 5 or the equivalent of 1,200,000 tons of phosphate rock are thus ran to waste. He remarks: "The wide dispersal of the vast quantities of phosphorus which it took the process of nature an indefinite period to segregate, must cease. The loss is irrop- Jj arable." Much has been done in recent years to comply with this demand. Phosphate Rock and the Migration of Phosphorus. In the meantime, in our phosphorus economy also, as in the case of the combined nitrogen of the Chilean nitre beds, we are living on our capital. For, as our fields tend to become depleted of phosphorus under intensive agriculture, we restore some of the rarefied clement to the tired soil by drawing upon the accumulations of ages, in the form of phosphate rock. As a matter of fact, in this we are welding 2 By treatment with sulphuric acid, which renders the phosphorus more readily available to plants. These are technical details that cannot be ontered into here. The reader must be referred to the pertinent agricultural A-and technological literature. PHOSPHOEUS CYCLE 249 the closing link in a very remarkable endless chain of nature. For the phosphates washed by the rivers3 into the sea serve as food to the marine vegetation and indirectly to the fishes and other aquatic species. 4 These act in this case as concentrating agents, the bones and teeth of fish, and some shells of Crustacea and molluscs, being comparatively rich in phosphorus. 5 In its further migration the 3 For details the reader may be referred to an article by E. Blackwclder in the Am. Jour. Sci., 1916, vol. 62, p. 285, from which the following particularly pertinent passage may here be noted: "Of the vast quantity of dissolved mineral matter annually delivered to the sea by the run-off, it is estimated that about 0.45 per cent consists of phosphorus pentoxide. Using the best available figures for the amount of water thus brought to the ocean annually, it is calculated that if the phosphatic material in the form of solid tri-calcium phosphate were loaded into standard railroad cars it would fill a train stretching continuously from Boston to Seattle and would be 7 to 12 times as great as the world's total production of phosphate rock in 1911. Nevertheless, so great is the volume of the oceans, and so vast the area of their floors, that if all this material were deposited in solid form uniformly over the bottom of the sea, it would build annually a layer less than 0.2 mm. thick. Of the phosphorus poured into the sea, so large a proportion is utilized by living beings that the net working balance dissolved in oceanic water constantly averages less than 0.005 per cent, expressed as PzOs, or, in other words about 0.18 per cent of the dissolved salts. In this solution, phosphorus seems to have reached the most dilute state in which it exists during the course of its complex migrations. Its subsequent transformations generally tend to ever greater concentration, almost until the cycle is closed upon itself. 4 Compare also W. Lindgren, Concentration and Circulation of the Elements from the Standpoint of Economic Geology: "In the sea water the bluegreen algae concentrate phosphorus, certain molluslcs or crustaceans feed on the algae, and other meat-eating mollusks devour the vegetarians. Small fishes eat the molluslcs, large fishes eat the small, finally seals and birds swallow the fishes, and so in about six transformations the phosphorus originally contained in the sea-water may come to rest in deposits of guano on desert islands or in accumulations of bones of vertebrate denizens of the sea" (Economic Geology, 1923, vol. 18, p. 431). 6 In this connection may be noted again a passage from Blackwelder's article, p. 289 (see footnote 3): "As phosphorus ascends in the evolutionary scale of animals, its concentration tends to increase, although irregularly. The protozoan, air dried, contains less than 0.6 per cent PaOc. According to Juday quantities of minute crustaceans from Lake Mendota contain in the air-dried condition 1.8 to 2.4 per cent of PaGc, or several times that of the protozoans. A Russian biochemist, Sempelovski, found in entire fresh specimens of a cartilaginous fish (the common skate) 0.91 per cent PaOs, whereas the average for eight Teleostean fishes with well-developed bones was about 1.5 per cent. Certain brachiopods, such as those of the family Lingulidae form shells of fibro-crystalline tricalcium phosphate probably either the mineral dahllite or staffelite." 250 ELEMENTS OF PHYSICAL BIOLOGY phosphorus here splits into two streams. On the one hand the hard parts of dead fish and other sea animals fall to the bottom and form a phosphatic deposit. So, for example, it is reported that in certain localities a single draft of the dredge has brought up 1500 shark's teeth from the sea bottom. These deposits become further enriched through the replacement of their calcium carbonate by calcium phosphate under the action of the sea water.6 Subsequently some of the deposits so formed have been raised, in a crust upheaval, above the sea level, so as to form sedimentary strata from which we now derive some of our supplies of phosphate rock. The other division of the stream in the flow of phosphorus is perhaps one of the most remarkable examples of a cycle in the economy of nature. The fish of the sea are eaten by birds, who flock in great hordes and have their nesting places upon rocky islands and shores.7 There an accumulation of immense amounts of guano has taken place in the course of centuries and ages. Of this guano some has been returned directly to the land by the agency of man. Other portions, of more ancient origin,, have undergone transformation, and have passed into fossil form by reaction with the rock base on which they were in the first instance deposited. This is the origin of a second class of (metamorphic) phosphate rock, which also wo mine and spread on our field, so that this loop in the chtiin also is closed. Soil Losses of Phosphorus. From this sketch of the migration of phosphorus in nature it is seen that qualitatively the path of tho element is a closed circulation. Unfortunately the cycle is quantitatively quite incomplete. Van Hise, quoting Whitson's invest! gations, shows that, on a very conservative estimate, tho soil of the United States loses annually some 2 million tons of P2 G , the equivalent of 6 million tons of phosphate rock. This is about double the total output of our phosphate quarries, and about four times our domestic consumption of that output. It is thus scon that tho situation with regard to our supply of phosphatic fertilizers is an exceedingly serious one it would perhaps not be out of place to say For a detailed discussion of some of these concentrating processes and related matters the reader is referred to F. W. Clarke, loc. cit., 1921, pp. 132 495, 502. See also Chapter XVIII, footnote 17. ^ 7 For an excellent illustrated account of the part played by the Guanay bird in this cycle see R. C. Murphy, Natl. Gcogr. Mag. Sept. 4, 1924, p. 279. PHOSPHORUS CYCLE 251 ao alarming one. For here we have no reserve which we may hope to find means of tapping in the future, such as is presented to us, in the case of nitrogen, by the inexhaustible supply in the atmosphere. Phosphorus is at best a comparatively rare element, constituting only about 0.14 per cent of the earth's crust (see table 16, Chapter XV). The general and alarming decrease in the crop yield per acre in various states so well described by Mr. James J. Hill, 8 is largely due to the depletion of the soil in phosphorus The work (at the Ohio Agricultural Experiment Station9 ) upon different fertilizers shows that for the soils tested in their experiments phosphorus was the controlling element in producing an increase in the cereal crops. 10 And elsewhere11 Van Ilise remarks : The average rock contains twenty times as much potassium as phosphorus. Therefore, looking toward the distant future, if we consider ratios, we may unhesitatingly assert that the problem of maintaining the fertility of the soil in phosphorus will be twenty times as difficult as for potassium; but this ratio by no means measures the real difference, for when a deposit contains a moderate percentage of a substance it may be possible to utilize it commercially, whereas, if the percentage falls below this amount it is without value. Phospbtatic Slag as Fertilizer. To the consideration of the migration of the element potassium thus referred to by Van Hise, we shall presently turn our attention. Before leaving the subject of the migration of phosphorus, one secondaiy source of phosphate fertilizer remains to be noted here, namely, the by-product (slag) obtained in certain processes of steel manufacture, in which the phosphorus contained in the ore (and very objectionable as a constituent in steel) becomes segregated, and is thus eliminated, in the slag. This latter, by suitable processes, is converted into a very serviceable fertilizer.12 8 The Natural Wealth of the Land, and its Conservation. Paper given at the White House Conservation Conference, May 13, 1908. 9 Ohio State Agr. Coll. Bull. 141, 182. 10 Van Hise, loc. cit., p. 704. 11 Idem, loc. cit., p. 701. 12 For details regarding the use of phosphatic slags as fertilizer the reader may be referred to G. S. Eobertson, Basic Slag and Rock Phosphates, Cambridge University Press, 1922. CHAPTER XX CYCLES: CONCLUSION AND SUMMARY The saltness of the sea is due to the numerous springs of water, which in penetrating the earth, find salt mines, and dissolving parts of these carry them away with them to the ocean and to the other seas, from whence they are never lifted by the clouds that produce the rivers. Leonardo da Vinci. The Circulation of Chlorine and the Alkalis. It will be convenient to consider jointly the migration of the elements chlorine, sodium, and potassium in nature, inasmuch as they are closely connected. There is a piece of laboratory apparatus known as the Soxhlet Extractor, of which the chemist makes use when he wants to prepare a solution, an extract, of one of the constituents of a mixture of substances. This apparatus, as represented in figure 53, operates on a simple principle. The solvent (water, ether, petroleum spirit, etc.) is placed in the flask A heated by a bimsen flame B, so as to drive vapors of the solvent up through the tube C to the top of a tubular vessel D containing the material M to be extracted. The whole apparatus is open at the top, but escape of vapor is prevented by a condenser tube E cooled by a water jacket F. The Vapor condensing in E drips down upon the material M, and dissolves out the substance to be extracted. The condensate accumulates in the vessel D and rises in the syphon tube I until it reaches the top of the syphon, whereupon it drains back into the flask A and is reevaporated, this cycle being repeated indefinitely as long as desired. Since the vapor of a liquid containing a non-volatile substance in solution is pure solvent, the action continues until practically all the soluble substance has been extracted. It is almost literally true that we pass our lives in the midst of a gigantic Soxhlet apparatus. The flask is the sea basin; the solvent is the water of the ocean, the rain, and our rivers and lakes. The material extracted is the earth's crust (rocks, soil, etc.). The place of the Bunsen burner is taken by the sun which raises water vapor from the ocean's surface, into clouds which drift over the land. 252 CYCLES: CONCLUSION AND SUMMARY 253 FIG. 53. THE SOXHLET EXTRACTION APPARATUS The action of this apparatus is closely analogous to the natural extraction of soluble constituents from the earth's crust by the water in circulation through clouds, rain, rivers and the sea, under the influence of the sun's heat. 254 ELEMENTS OF PHYSICAL BIOLOGY CYCLES: CONCLUSION AND SXJMMAEY 255 The cold upper atmosphere acts as a condenser (see fig. 54), beyond which no clouds can pass out above. Presently the moisture of the clouds is precipitated as rain over the face of the earth. It drains into rivers and lakes back into the sea, charged now with the soluble constituents of rock and soil. This operation has been going on over and over for ages, with the result that the greater part of the more soluble constituents of the rocks is by this time collected in the ocean, imparting to its water its characteristic salt taste. It is worthy of more than passing note that these relations, in all essentials, were recognized by that universal genius, Leonardo da Vinci, whose remarks on this subject appear at the head of this chapter. The principal soluble constituents of the earth's crust are the carbonates and chlorides of the alkali metals, sodium and potassium. These, then, mainly take part in the extraction process described. There is, however, an important difference in the behavior of sodium and potassium in this process. In the igneous rocks sodium and potassium are present in very nearly equal proportions (see table 16). Yet the ocean is very much richer in sodium than in potassium (see table 14). What becomes of the potassium? 1 It is a circumstance highly significant for terrestrial life that potassium salts seem to be largely absorbed from their solutions on their passage through soil and clay. Thus the soil would retain a supply of the element so essential for plant growth, while the less vitally important sodium 'in other respects so similar to its next kin potassium has in large part passed on into the ocean. 2 Nevertheless, potassium is not present in most soils in profusion; under intensive agriculture the soil becomes impoverished in this constituent also, and recourse must be had to sources of potassium salts in concentrated form, the deposits left by the drying up of ancient seas, to make up the deficiency. In this field, also, the World War has materially affected the complexion of agricultural economics. Its influence has been twofold. In the first place, since 1 In this connection, and for details regarding the circulation of Na, K,Cl, and the related question of the age of the ocean, the reader may be referred to F. W. Clarke, Data of Geochemistry, pp. 136, 137, 145, et seq. 2 These suppositions must be viewed with a certain caution, as has already been pointed out; see p. 204, footnote 19. 256 ELEMENTS OF PHYSICAL BIOLOGY the only areas highly productive of potassium salts were contained within the domains controlled at that time by Germany, it became necessary for the Allies to find other sources of the needed element. One outcome of this was a temporary development of potash recovery from the waste of cement works and other materials. Unfortunately much of the commerce thus started had to be abandoned again when the customary sources of potash became once more available after the close of the war. The second effect of the war upon the potash situation arises from the political changes which it brought about. The Alsatian potash deposits, formerly controlled by the same monopoly as the German Stassfurt deposits, are now in French domains, and the monopoly is broken.3 Some of the quantitative aspects of the migration of chlorine and sodium are shown in figure 54. The Circulation of Sulphur. Sulphur occurs in abundance in inorganic nature in the form of the sulphates of the alkalies and alkaline earths. Plants assimilate these compounds directly and then form proteids containing about 0.3 to 2 per cent of sulphur. In this form it is assimilated by animals, who excrete the element chiefly in the form of sulphates. These, returned to the soil, complete the cycle. Tlie Circulation of Iron. The importance of iron in the economy of the living organism is out of proportion to the comparatively small amount of this element actually present in the body. Thus the body of a human adult holds only about 4.5 grams of iron, contained, for the most part, in the red blood corpuscles. The importance of this comparatively small amount of the metal arises out of the fact that it fulfills the essential function of an oxygen carrier, a catalyst as it were, mediating the transfer of oxygen from the air in the lungs to the tissues of the body through the blood stream. Similarly, in plants, the iron is contained chiefly in the chlorophyll, whose catalytic action is a fundamental condition for the assimilation of carbon dioxide from the air. This catalytic action of iron is attributable to the ease with which it passes from ferrous to the ferric condition and vice versa, and plays a significant 3 G. Jones, Q. Jour. Econ., 1920, vol. 34, p. 392, CYCLES: CONCLUSION AND SUMMARY 257 idle not only within the body of the organism, but also In the soil, where it hastens the oxidation of carbonaceous matter, thus rendering carbon once more available for the organic cycle. 4 Summary of Cycles. In conclusion of this chapter a few remarks and tables regarding the circulation of the elements in general may be offered. In retrospect we may observe that alcharacteristic stamp is placed on certain of the elementary cycles by the form in which TABLE 26 Supply of plant foods in soil Number of years the supply of several elements would last, utilizing soil to a depth of 7 inches, and producing annually a crop of 100 bushels of com. Average compositon of soil assumed equal to that of 2110 samples of common rocks in the United States. (C. G. Hopkins, Annual Acad. Sci. 1909, vol. 33, p. 638). * Assuming stalks returned to the land. each element occurs or takes part in the circulation. Thus, the gases oxygen and carbon dioxide occur in nearly uniform distribution, so that their migration is free from certain complications that arise in the case of the other elements. Water occupies a position intermediate between the gaseous 'elementsjand^those which like phosphorus, potash, etc., as solids, are subject to local segregation, and thus introduce problems of transportation in one form or another. As vapor, water drifts with air currents. But owing tn the phenomenon of precipitation, water, unlike the permanent gases, is very unevenly distributed, the supply available for life processes being strictly a matter of climatic conditions. Thus, in desert regions water functions as the limiting factor of life. Nitrogen, although 4 G. Bunge, Physiological and Pathological Chemistry, 1902, p. 21. 258 ELEMENTS OF PHYSICAL BIOLOGY gaseous in the elementary state, is chiefly operative in combined forms, so that its distribution in available form, is also a locally varied phenomenon. All these facts have their influence not only on the primitive flora and fauna as a function of geographic site, but play also an important role in those secondary life phenomena which we commonly describe as commerce and trade:. Two tables 26, and 27, are, finally appended, the one giving certain data of interest regarding the Supply of Plant Foods in the TABLE 27 Rate of participation of the elements in cycles of nature * Authorities : A. = Arrhenius, Worlds in the Making, 1908 ; C. = Clarke, Data of Geochemistry, 1921; L = Linck, Kreislaufvorgange, 1912; M. = McGee, Science, 1911, vol. 134. The numbers in the column "Authority" refer to pages of the works cited. Soil, according to C. G. Hopkins; the other giving estimates of the Rate of Participation of the Elements in the Cycle of Nature. It seems hardly necessary to point out that the quantitative estimates cited in these chapters on the circulation of the elements in nature represent only very rough approximations, the best perhaps that can be attained in the present state of our knowledge. As F. W. Clarke3 remarks, "Such estimates may have slight numerical value, but they serve to show how vast and how important the processes under consideration are." Rough as the data are, they give us, presumably, at least an idea of the order of magnitudes involved. The least that can be claimed for them is, in the words of Clarke5 once more: "In calculations of this sort there is a certain fascination, but their chief merit seems to lie in their suggestiveness." 6 F. W. Clarke, Data of Geochemistry, 1920, p. 48. CHAPTER XXI MOVING EQUILIBRIA Aus dieser Untersuchung wird kein Dualismua hervorgehen, sondern eine Wissenschaft, welche Organisches und Anorganisches umfasst, und die den beiden Gebieten gemeinsamen Thatsachen darstellt. E. Mack. In preceding pages we have considered as examples of biological "equilibria," states that quite obviously can be regarded only as rough approximations to equilibria or steady states; and we have not, so far, examined critically the justification for this attitude. It is desirable to give at least brief consideration to this matter. It is common custom, in dealing with the relatively simple systems studied in physical chemistry, to assume that a sufficiently slow change in one parameter (e.g., volume) defining the state of the system, brings in its train a succession of states each of which is essentially equilibrium. So, for example, if we slowly raise the piston in a gas-tight cylinder containing X grams of water and Y grams of water vapor at a temperature 6, it is commonly assumed that at every instant the quantities X, Y are such as correspond to equilibrium at the temperature 8. The Principle of Continuity. The basis of the assumption referred to in the preceding paragraph is rarely if ever discussed. Obviously it is to be sought in the principle of continuity. If the parameter P is constant, at the value P , the variables X, Y, . . . defining the state of the system have certain values X , YQ, . . . We tacitly assume that if the parameter PO is nearly constant at the value P (that is to say, passes through P in very slow change) then the variables X, Y will have nearly the value of Xo, Y , . . Or, in the notation of an earlier section, if ^-i^tt:,,*,, . . .P) (i) at and if, with P = P = constant ^ = pz = . . = pi = . . . = o (2) 260 ELEMENTS OF PHYSICAL BIOLOGY gives Xi = (?i = constant (3) then we assume that with P = P() (4) where P(t) is a slowly changing function of t, we shall have Xi = d(t) (5) where Ci(t") is a root of the system of equations Fi(i) = Fz (ti = . . . = Fi(t) . . . = (6) (for all values of It should be noted that, strictly speaking, this involves a contradiction. For if the velocities F are zero, the variable X cannot be changing. And, in point of fact, the result (5) represents a first approximation which is not in all cases free from significant error. Higher Approximation. It is possible, in certain cases, to proceed to second, third and higher approximations by successive steps, or, as will be shown, by a single formula. So, for example, for a system in two variables X, Y, we may write, first of all d -j = F^X, Y, i) (7) ^ = F(X, Y, t) (8) 'The first approximation here is F! = Fz = (9) X = X1 (t) (10) Y = Fi(<) (11) The second approximation we obtain by differentiating (10), (11), so as to obtain the derivatives Xi, YI, which, although not zero, are nevertheless small, according to our supposition of a slow change. Substituting these in (7), (8) we find Fi - Xi'(t) (12) F, = F,'(0 , (13) MOVING BQUILIBEIA 261 Hence X = Xt(t) (14) F = F2 (*) (15) And so on, for successive higher approximations. But this process can be contracted into a compact expression. We have ^J = ?f1 , ^Oj d JE *>1}*Y dt ~ di" bX dt bY dt ' ^! = 5f> _)_ ^J^I L ^.2 ^I d d* d,Y di + dF d< ( If we substitute in (16) (17) f-X/> (18) dF Tt = YS0 (19) the right hand member must vanish, in view of (9), (10), (11) and we have +*'+*from^which it is seen that X2 (t), F2 (0 can be expressed directly as the solution of the system of equations Similarly the (n + i) th approximation is found by writing _' = _ = o (24) Special Case. Returning to the general case of n variables, suppose that for all values of Xl Xz . . . differing appreciably from 262 ELEMENTS OF PHYSICAL BIOLOGY the equilibrium values, the velocities ] ... are negligible (Z6 QJ(I dXr as compared with some one of them, say -j-. Then we can write, at practically Xt, . . . Xn) = (25) Fn (Xi, Xz, . , . Xr, . . . Xa) where ^r is excluded from the system (25) . This defines X2 = Cz (Xr) (26) etc. In addition to this we then have the equation TTLT * = Ft (Ci, C*, . . . Xt, . . . Cn ) (27) at = Fr (Xr) (28) Hence which is directly integrable ? ,v x (30) In such case as this, then, that particular change which is much slower than all the others, sets the pace and controls the whole process. It acts as a brake, as a limiting factor. RADIOACTIVE EQUILIBRIUM Moving equilibria play an important role in evolutionary processes of the most varied type, as emphasized almost ad nauseam by Herbert Spencer, 1 though some of the most typical and at the same time most fundamental examples were unknown to him. For, the most exact, quantitatively precise illustrations of moving equilibria are to be seen in the evolution of chemical elements by successive steps 1 First Principles, Chapter XXII. MOVING EQUILIBRIA 263 ggsiggaga^^ FIG. 55. URANIUM AND ITS PRODUCTS OF RADIOACTIVE DISINTEGRATION (U = uranium; To = ionium; Ra = radium; Rn = radon == radium emanation; Po = polonium; Pb = lead.) Each element in the chain is produced from its predecessor either by the emission of an alpha particle, i.e., a doubly charged helium atom, in which case the atomic number is decreased by two units; or by the emission of a beta particle, i.e., an electron, in which case the atomic number increases by one unit. 264 ELEMENTS OF PHYSICAL BIOLOGY of atomic disintegration, accompanied, in most cases known to us, by radioactive manifestations. It is not within the plan or compass of this work, to give a detailed account of what has by this time grown into an extensive special field of physical science. It must suffice to refer to the chart (fig. 55) of one of the typical series of radioactive transformation chains, and to state briefly the simple law of transformation of such elements by spontaneous atomic disintegration : The amount of a substance transformed per unit of time is directly proportional to the amount of that substance present, so that if Si is the ith substance in a transformation chain and if we denote by Xt the mass of Si, then we have a system of equation "V T7" "\ T7" /fjrO -Ai-^-x-AA (32) where the coefficients X are constants, invariable under all conditions to which observation to the present date has extended. It will be seen that the system of equations (32) is a simple special case of the general form discussed in Chapter VI. Its solution2 is of the form there indicated, but the simplicity of the differential equations is reflected in the integrals, which here appear as finite series, the expression for the mass of z th substance, being Xt = a,-,ie~ Xlt + ai,2e~ X4t 4- . . . + ai,t * (35) am - if i < k (36) 2 For a somewhat remarkable method of integration (by a multiple integral), see A. Debierne, Les ide"es modernes de la Matiere, 1913, p. 328. 8 See, for example, E. Rutherford, Radioactive Substances, 1913, pp. 422, 423. MOVING EQUILIBEIA 265 Thus, after a sufficient lapse of time, the substances Si, S2 , . . . Sk are always present together in constant proportion, so that we have a moving equilibrium of a veiy simple type, illustrated graphically in figure 56, in accordance with some of the constants given in tables 28 and 29. The most slowly decaying substance here acts as TABLE 28 Radioactive equilibrium of radium in contact with its disintegration products on the basis oj data in Jour. Am. Chem. Soc., 1923, vol. 45, pp. 872-873 *Half-decay period = = 190 years. fPolonium. the controlling, slowly variable parameter, and sets the pace with which all the subsequent members in the transformation chain keep step, so that the polygons representing the system in its successive stages are geometrically similar. (Compare fig. 58 on p. 277.) The second of the two expressions for the ratio aifi: /akk calls for brief comment. If i < /c, that is to say if the substance Si precedes, in the transformation chain, the substance Sk which has its lowest disintegration rate, then Si does not appear at all in the equilibrium. Hence when an aggregation of substances in radioactive equilibrium is found in nature, the substance at the head of the chain (the "parent substance") is always the one of slowest disintegration rate. But, obviously we cannot from this draw any conclusion as to whether or not it is itself a product of disintegration of a pre-parent of more rapid Oi-% A decay .ate. Aay such pre-parei* OP PHYSICAL BIOLOGY as it were, have been CONTACT WITH ITS DISINM davs (half-decay period) torn a geometric series Tte different equations transformation "dily to deterge the . H. Mitchell, PhU. Mag., 23, p. 353. . , ^rairw of radioactive f^ation> and there is rf OTCCessive approxima. However, the first , P- ' A' MOVING EQUILIBBIA 267 approximation is so simple, that it is commonly applied. Equating the right hand member of (32) to zero we find immediately -j = *LI (37) and by an obvious extension - ~* (38) Afc Xi It is easily shown that Li} the reciprocal of X;, is the "mean length of life" of an atom of the substance $,> We may write (38) ~ - ~ (39) which expresses the fact that, in first approximation, the amounts of several substances present together in radioactive equilibrium arc in the ratio of the respective mean lengths of life. 5 This result can also be read out of (35) if \\h \, the least of the |X|'s, is negligible in comparison with all the other |X|'s, so that the denominator reduces to the product It is thus seen that the closeness of the first" approximation depends on the relative magnitude of X& and the remaining X's. In many chains of radioactive transformation the parent substance is very slow in its disintegration, and the first approximation (giving what Rutherford has termed the secular equilibrium) is exact within the limits of experimental error. But if one of the more rapidly decaying members is isolated and is then allowed to come into equilibrium with 5 This is a special case of a general law that if all the exponents \ arc real and negative, the final stages of the process of evolution are characterized by constancy in the ratios of the Variables .T. Compare p. 261, Special <7a.svj; also, Lotka, A. J., Proc. Am. Acad. Sci., vol. 55, 1920. Ifc should be noted, however, that in the general case, xt denotes not mass of Si, but CXCGHB of that mass over the equilibrium mass of Si. In the radioactive equilibrium there is no distinction between X and x, since the ultimate value of both is zero. For the second and higher approximation, applied to the radioactive equilibrium, the reader may be referred to A. J. Lotka, Proceedings Natl. Acad. Sci., 1921, vol. 7, p. 170. 268 ELEMENTS OF PHYSICAL BIOLOGY its own products of disintegration, the error of the first approximation may become appreciable. 7 This is shown, for example in table 29, which exhibits the amounts of radon gas (radium emanation) and its several products of disintegration in radioactive equilibrium. It will be observed that in the case of radium C there is a discrepancy of about 1 per cent between the amount computed by first approximation and the true amount. Radioactive Chains as Cosmic Clocks. It must be noted that all that has been said above regarding the amounts of the substances present in radioactive equilibrium does not apply to the last link in the chain, the end product. This does not, of course, take part in the equilibrium, but accumulates, if non-volatile, as in the case of lead, or, it may in part escape and be lost to observation, as in the case of helium. TABLE 29 Radioactive equilibrium of radon (radium emanation) in contact with its disintegration -products, on basis of data in Jour. Am. Chem. Soc., 1923, vol. 45, pp. 872-873 *Half~decay period = 0.69315 L = 3.85 days. If the amounts of parent substance and end product are large as compared with the amount of intermediates, the amount of any one end product formed is evidently simply proportional to the amount of parent substance lost by disintegration in a given time. The chain of substances in transformation behaves, in fact, much like a sandglass clock having a number of bulbs and from the accumulation in the end bulb we can obtain an indication of the age of the system, on the assumption that originally all was in the top bulb, that initially only the parent substance was present. The application of this principle to radioactive mineral deposits has given us a quantitative time scale in historical geology where before we had to 7 Compare E. Rutherford, Radioactive Substances, 1913, p. 430. MOVING EQUILIBRIA 269 rest satisfied with a crude chronology recognizing only order of precedence, or at best dealing in exceedingly uncertain jjestimates of lapse of time. Thus the investigation of radioactivity, remote as it seems from the field of life phenomena, has nevertheless contributed to biology essential information regarding the time that has been available for the evolution of the earth and its inhabitants. The estimate reached upon this basis is that the age of the radium-bearing rocks (uranium ore) examined is at least eight million years, and at most seventeen hundred million years old. For a resume" of various estimates of the age of the earth the reader may be referred to G. TABLE 30 Geologic time table After Sclmchert Schuehert, The Evolution of the Earth and its Inhabitants, 1919' pp. 56 et seq.; 80; and to the Proceedings of the American Philosophical Society, 1922, vol. 61, pp. 247-288. See also E. Rutherford, Radioactive Substances, 1913. Schuchert's estimate is that "geologic time endured about eight hundred million years," distributed among the several geological eras as indicated in table 30. The Origin of the Elements and the Ultimate Genesis of the Organism. The case of radioactive equilibrium has here been introduced primarily by the way of illustration, as probably the most typical example in nature of a moving equilibrium in a system in the course of evolution. But the matter is also of more material interest to us in our survey of the evolution of the earth as the abode of life. For, as has already been emphasized, we are not only on the earth but of it; we have thus a two-fold interest in the evolution of its substance first, as providing the stage upon which our life drama is set; and second, as furnishing the material of our bodies. Of these same ele- 270 ELEMENTS OF PHYSICAL BIOLOGY ments that make up the earth's crust we also are composed: their genesis is therefore also the first, remote chapter in the genesis of our own bodies. Through the discovery of radioactive chains of elements we hold a clue regarding the fundamental influences that have determined the quantitative chemical composition of our world, and have thus appointed the measure of the supplies available for our needs. Those elements whose genesis is known to us came into being in perfectly definite proportions. Presumably the same is true also of those whose precise mode origin is still unknown. There is good evidence to support this view. We have at present no detailed quantitative knowledge of the laws which determine the value of the decay coefficients X of the radioactive elements, and which thus ultimately fix their relative abundance in equilibrium. But a significant qualitative relation has been pointed out by W. D. Harkins. 8 When the elements in a radioactive chain are arranged in order of their atomic numbers, 9 and are separated into two groups, those of odd and those of even number, it is found that each even-numbered element is more abundant than the adjacent odd-numbered elements. And, what is of particular significance, the law of relative abundance of odd and even-numbered elements extends also to those elements, regarding whose precise mode of origin we have not, as yet, that sure knowledge which is gained by direct observation within the four walls of the physical laboratory. (See fig. 57.) 8 Jour. Am. Chem. Soc., 1916, vol. 38, pp. 863, 869; 1923, vol. 45, pp. 1420- 1433. Compare also F. W. Aston, Nature, March 15, 1924, p. 394. For other regularities observed in the length of life of radioactive elements see K. Fajans, Radioaktivitat (Sainmlung Vieweg Heft 45) 1921. 9 The chemical elements, arranged in ascending order of atomic weights, beginning at hydrogen = 1, may be given ordinal numbers 1, 2, 3, etc., indicating their position in the series. These ordinal numbers have been found to have important relation to the atomic architecture. They have been termed the atomic numbers. The definition here given is not quite exact; in certain places allowance must be made, gaps left for unknown elements, and the several isotopes of one element receive the same atomic number, though differing in their atomic weights. A more precise definition is the following: The atomic number of an element represents the excess of positive over negative charges in the constitution of the atomic nucleus. Each atomic number also represents the place occupied by the element in Mendeleef's table (Jour. Am. Chem. Soc., 1923, vol. 45, p. 868). For further information the reader must be referred to the special literature; of comprehensive works the following may be mentioned: Bragg, X-rays and Crystals; F. W. Aston, Isotopes. FIG. 57. RELATIVE ABUNDANCE OF THE ELEMENTS Each element of even atomic number is more plentiful than the adjacent elements of odd stomic numbers. Diagram according to W. D. Harking, based on analysis of meteorites. (Jour. Am. Chem. Soc., 1916, p. 863.) 271 272 ELEMENTS OF PHYSICAL BIOLOGY But the laboratory is not a prison, and the eye of the physicist is free to sweep the sky, where nature's great smelteries gleam at night. With the aid of the spectroscope he has studied the multitudes of the stars, and has recognized in them a number of distinct stages of evolution. Life's day is far too short to give the observer any opportunity to study directly the evolutionary changes in any one star. But by piecing together the observations made upon the mixed population of stars of different ages, it has been possible to construct with considerable certainty the main stages in stellar evolution, just as the stages of human life could be gathered from a single observation of a mixed population comprising persons of all ages. The evidence points clearly that the elements, such as we know them, are the product of "the general brewing of material which occurs under the intense heat in the interior of the stars." Out of such foundry came our own abode, if we accept the well-considered views of Eddingtor.. '" "I do not say that the earth was a gaseous body when it first became recognizable as an independent planet, but I am convinced that its material was at one time merged in a completely gaseous sun/' And since we are of earth, ours also is the same origin. The hand that writes these words and the eye that reads them alike are composed of the selfsame atoms that came into being, ages and ages ago, in the young sun. Far, far more wonderful than any dream of old 10 A. S. Eddington, The Borderland of Astronomy and Geology, Nature, 1923, p. 18, also, The Interior of a Star, Supplt. to Nature, May 12, 1923. The Tder who wishes to acquaint himself in greater detail on this subject may refer to Eddingtons's -work Stellar Evolution. In the interest of unbiassed presentation it must be noted here that T. C. Chamberlin (The Origin of the Earth, 1916) has put forward a theory of the origin of the earth and the planets which is at variance with that sustained by Eddington. On the other hand it is also proper to mention a fundamental objection to theories of cosmogony of the type of that of Chamberlin and Moulton, which is based on the supposition that the luminous stars are formed by the collision of dead suns. "The distances separating the stars are enormous compared with their own dimensions. Sir Frank Dyson once used the illustration of twenty tennis balls distributed at random throughout the whole interior of the earth, to give a model of the density of distribution of the stars Taking a very liberal view of the kind of approach that can be held to constitute a collision, it is estimated that a star would suffer a collision about once in a hundred million million years" (Eddington). For a survey of the modern views on this subject see J. Barrell, The Evolution of the Earth (Yale University Press, 1919). MOVING EQUILIBBIA 273 mythology is the story of our creation. Thus was the birth of man prepared in the grey dawn of time ; thus the metal of his frame compounded in the flaming furnace of a star. .... TERMINAL STAGES OF THE EARTH'S EVOLUTION Geophysics and Geochemistry. For the last stages in the evolution of the elements and their chemical combinations we do not look to the stars. We can study them at close quarters in the field and in the laboratory. In this way, with the application of physics and chemistry to general problems of geology, have grown up the sciences of geophysics and geochemisty. Indeed, it naturally might be supposed that on the terrestrial phases of inorganic evolution we should be altogether better informed than on those prior stages, far remote in time and space, which run their course in distant suns. But this is true, at best, only in restricted measure. It is a singular circumstance that, in some ways, we are better informed regarding the physics and chemistry of the stars, of which the nearest, outside the solar system, is twenty-five million million miles distant, than regarding that of our own planet. To say that the earth's surface layers accessible to our direct observation are comparable, scale for scale, to the shell of an egg, is to err on the side of liberality. The deepest burrow into the earth made by human agency, the mine shaft at Morro Velho, Brazil, 11 is 1-|- miles (6400 feet) deep or only about frsT of the earth's diameter. Direct observation can therefore give us at best only the most uncertain information regarding theconditions at even moderate depths. Where the crust has been creased and thrown into folds, subsequent denundation may have exposed layers of some 50 or 60 miles aggregated thickness.12 But, though this gives us an invaluable record of some of the most significant chapters in the earth's history, it adds little or nothing to our knowledge of conditions of temperature and pressure even at comparatively trivial depths, and regarding chemical composition also it gives us, after all mere surface indications. Indeed, our information on all these points is very largely of a negative character. We know from the earth's average density that the composition of the core must be very different from that of the shell. We know that the temperature u Sir Charles Parsons, Nature, February 19, 1920, p. 677. 12 G. Schuchert, The Evolution of the Earth, Yale University Press, 1919, p. 67. 274 ELEMENTS OF PHYSICAL BIOLOGY gradient observed in boreholes near the surface averages an increase of about 1F. for every 60 feet (1C. for every 35 meters) descent, but of the further course of temperature at greater depths we know with reasonable certainty only that it cannot continue at this gradient, which would give a phantastic temperature of 300,000F. (1 80,000C.) at the center. Lord Kelvin's calculations, based on the rate of cooling of the earth, and the more recent figures of the same character given by Van Orstrand, are rendered uncertain in their application owing to the presence of radium, in unknown amounts, evolving heat in its distiiitegration. Strutt has made the tentative estimate that the temperature rises uniformly to a depth of about 30 miles, and after that remains sensibly constant at 2700F. A little more definite is our information regarding the pressure in the earth's interior. A first approximation of its value is found by considering the earth as a fluid. It is thus found13 that the pressure at the center would be three million atmospheres. In any case there can be no doubt whatever that the pressures reached vastly exceed anything at our command in the laboratory, where a pressure of twenty-four thousand atmospheres, employed by P. W. Bridgman in his researches, stands out as a record achievement, though it coiv responds to a depth of rock of only 56 miles.14 It must be clear from what has been said above, that all conjectures as to the physical, chemical and subatomic transformations going on in the earth's interior are subject to a very large margin of uncertainty. In this connection it is well to recall the words of F. W. Clarke:15 The chemistry of great pressures and concurrently high temperatures is entirely unknown, and its problems are not likely to be unravelled by any experiments within the range of our resources. The temperatures we can command, but the pressures are beyond our reach We may devise mathematical formulae to fit determinable conditions; but the moment we seek to apply them to the phenomena displayed at great depths, we are forced to employ the dangerous method of extrapolation, and our conclusions are not verified. 13 This supposition, in calculating pressures, probably does not err far from the truth. The researches of P. D. Adams (Journal of Geology, February, 1912), P. W. Bridgeman and others have shown that at depths of some 30 miles rocks probably give way like butter to the pressure of the layers above them. " W. D. Lambert, Jour. Washington Acad. Soi., 1920, p. 126. Sir Charles Parsons, loc. cit. 15 Data of Geochemistry, p. 271. MOVING EQUILIBRIA 275 In these circumstances we can feel but little confidence in inferences based upon our laboratory observations, relating to radioactive ami other possible atomic transformations going on at greater depths within the earth. If the degree arid character of radioactivity which we observe in the accessible surface layers were to continue throughout the mass of the earth, the amount of heat developed would be much in excess of the observed losses by radiation.10 Unless therefore, we are to draw the highly improbable inference that the temperature of the earth's mass is steadily rising, we are forced to one of two assumptions. Either the radioactive elements arc segregated chiefly in the earth's crust; or, the present rate of heat loss by radiation from the earth does not represent its average rate. This latter is the alternative elected by J. Joly 17 in an original conception. According to this there are alternate periods of accumulation of heat in the solid rocks, followed by periods in which these rocks, having finally become melted, well to the surface in a death-dealing flood of fire. Thus, by convection, a process far speedier than conduction, through the solid rock mass, heat is dissipated until, after sufficient cooling, a second period of quiescence, with a solid earth's crust, is ushered hi. And so, in long waves of perhaps some thirty million years duration, the planet alternates between periods of hospitable clemency and periods intolerant of life. There is, for us living inhabitants of this globe, a certain wildly romantic element, a feature of calamitous tragedy, in the hypothetical picture of the world's history thus summoned up before our imagination. In its biological aspect how great and wonderful it all is I The living being working out his destiny on this poor raft, unknowing of the fiery ocean upon which this world is floating: unknowing of the inevitable sinking and uplifting which in truth largely controls the destinies of his race. .Deathdealing forces all around, and yet the light of life shining age after age upon the earth. 16 Compare V. Moritz, Dor Stoffwechsel der Erde, Zeitschr. f. Eloldrochemie, 1922, p. 421. 17 J. Joly, Movements of the Earth's Crust; lecture under the auwpicoH of the Royal Dublin Society, published in Nature, 1923, p. 003. A third possibility is that under the extreme conditions of temperature and pressure prevailing in the earth's interior reversal of the familiar radioactive disintegrations, or similar endothermie processes may go on. (Jour Natl Acad. Sci., 1924, p. 89. 276 ELEMENTS OF PHYSICAL BIOLOGY Such conceptions as this, stimulating as they are to the imagination in reconstructing for us an image of the remote past and distant future, must be entertained with reserve, remembering the words of caution quoted above from Clarke's classic work. We must be prepared to consider the possibility that under the extreme conditions of temperature and pressure prevailing at great depths other subatomic transformations than those known to us in the laboratory may occur. Perhaps some evidence of this is seen in the evolution of helium as a component of natural gas, in amounts (up to 1.5 per cent18 ) in excess of anything readily accounted for on the basis of the observed radioactivity of the rocks. And, while the subatomic transformations known to us are exothermic, accompanied by liberation of heat, others undoubtedly are endothermic, associated with absorption of heat. We seem to have carte blanche, in the present state of knowledge, in our speculations regarding the net heat balance of the elemental transformations that may be going on under our feet. On surer ground rest our conceptions regarding the organization of matter, especially in the more superficial layers of the earth, under the action of ordinary physical and chemical influences. That the prime factor effecting the first and fundamental segregation of the lighter elements is flotation under gravity can hardly be doubted; this statement would in fact, be little more than a platitude if we were assured that the elements themselves remain unchanged under the extreme conditions of temperature and pressure prevailing in the earth's interior. Beyond this prime factor the study of mineral and rock formation becomes a complex chapter in applied physical chemistry, the consideration of which is not within the plan of this work. The reader who wishes to follow out further this phase of the subject will find a comprehensive survey of the field in an article Dcr Stoffwechsal der Erde, by V. Moritz, in the Zeitschrift fur Elektrochemic, 1922, pp. 411-421; and in the memoir The Chemistry of the Earth's Crust by H. C. Washington, which has already been quoted. Organic Moving Equilibria. Of moving equilibria in the organic world, data are most readily available for the system comprising man and his domestic animals. Here the human race acts as the controlling factor, drawing its dependents after it in its growth. The equi- 18 R. B. Moore, Nature, 1923, p. 91; Cady and McFarland have reported one instance of 1.84 per cent. J, Joly, Radioactivity and Geology, 1909, p. 218. MOVING EQUILIBEIA 277 librium polygon for the principal items of animal husbandly in the United States is shown in figure 58. The geometric similarity of successive polygons is in this case only approximate, the proportion of the several components varies somewhat; except in the case of the sheep population, however, the variation is moderate over the halfcentury from 1871 to 1921. (Compare fig. 56 on p. 265.) Aside from the features for the express illustration of which the diagram figure 58 was drawn, it also serves to point once more to the -70 FIG. 58. EouiLiBEitnvi POLYGON .FOE THE HUMAN SPECIES AND SOME OF THE SPECIES ON WHICH IT DEPENDS FOU ITS FOOD SUPPLY. SCALES READ IN MILLIONS fact already emphasized, that the concept of evolution, to serve us in its full utility, must be applied, not to an individual species, but to groups of species which evolve in mutual interdependence; and further, to the system as a whole, of which such groups form inseparable part. It would be conveying a false impression in a very essential respect, to exhibit the example illustrated in figure 58, without a comment in emphatic reservation. Although, in a roughly approximateway, it is true, as shown by the polygon diagram, that in its relation 278 ELEMENTS OF PHYSICAL BIOLOGY \? ^ MOVING EQUILIBRIA 270 to certain staples of agricultural production, our population lias advanced in a succession of moving equilibria; yet, tbo progress of modern industrial civilization on the whole is essentially the very antithesis of a moving equilibrium conditioned by and following upon the changes of a slowly varying parameter. Quito on the contrary, the development of this age is rather of the nature of a rocket-like ascent with a speed altogether unparalleled in all previous history of organic evolution, and at the cost of rapid depletion of capital resources. Certain aspects of this phenomenon are reserved for consideration in a later chapter. Here it will bo sudiciently to the point to draw attention to table 31, reproduced from H. Pearl's essay on The Population Problem, which shows the altogether disproportionate increase in the growth of our material accessories iu recent years, as compared with that of the population itself. The human species, considered in broad perspective, a,s auui, t inc.liK ling its economic and industrial accessories, has swiftly and radically changed its character during the epoch in which, our life has been laid. In this sense we are far removed from equilibrium ...... a fact which is of the highest practical significance, since it implies that a period of adjustment to equilibrium conditions lies before us, and ho would be an extreme optimist who should expect that such adjustment can be reached without labor and travail. We can only hope that our race may be spared a decline as precipitous as is the upward slope; along which we have been carried, heedless, for the most part, both of our privileges and of the threatened privation ahead. While such sudden decline might, from a detached standpoint, appear as in accord with the eternal equities, since previous gains would in cold terms balance the losses, yet it would be felt as a superlative catastrophy. Our descendants, if such as this should be their fate, will see poor compensation for their ills in the fact that we did live in abundance and . Pearl, Geographical lioviow, 1922, vol. 12, p. 038, MOVING EQUILIimrA < 1 J to certain staples of agricultural production, our population advanced in a succession of moving equilibria; yet the p roarer modern industrial civilization on the whole is essentially tinantithesis of a moving equilibrium conditioned by and follmvim'; upo the changes of a slowly varying parameter. Quite on the cmtinin , the development of this age is rather of the nature of a rurkef -Hie ascent with a speed altogether unparalleled in all previous hi:>f urv nt" organic evolution, and at the cost of rapid depletion of capital resources. Certain aspects of tins phonomo.ii.on are reserved l E" Picard> Tra^ d'Analyse, vol. 3, 1908, pp. 187, 188, 194, 197; E. Goursat, Cours d'Analyse, vol. 2, 1918, pp. 482, 498. 280 DISPLACEMENT OF EQUILIBRIUM 281 final values of the parameters whose modification provokes or is associated with the change. So, in physico-chemical transformations ("changes of state") the principle of Le Chatelier enables us to predicate, within certain limits, the sign of the displacement of equilibrium conditioned by a change in certain of the parameters upon whichjthe equilibrium depends. THE PRINCIPLE OF LE CHATELIER The principle of Le Chatelier is best illustrated by a simple example. Consider the simple chemical reaction 2H2 + Oa =2HaO + 58.3 oal. At high temperatures this reaction is reversible; that is to say, it takes place to some extent in the direction of the upper arrow, but also to some extent in the direction of the lower arrow, and an equilibrium is finally established between these two opposing reactions. Now this is what the Le Chatelier principle tells us: If we add either H alone or alone to the system, the equilibrium is shifted in the direction of the upper arrow, that is to say, in such direction as to absorb some of the added constituent. Similarly, if we heat the system, the equilibrium is shifted in the direction of the lower arrow, that is to say, in the direction of the reaction which absorbs heat. The principle, as enunciated by Le Chatelierz himself, is: Every system in chemical equilibrium, under the influence of a change of any single one of the factors of equilibrium, 3 undergoes a transformation in such direction that, if this transformation took place alone, it would produce a change in the opposite direction of the factor in question. The factors of equilibrium are temperature, pressure, and electromotive force, corresponding to three forms of energy heat, electricity and mechanical energy. The second paragraph of the principle as quoted above, requires special emphasis. It is often omitted, even by authors of the highest 2 Recherches sur les Bquilibres Chimique, 1888, pp. 48, 210; Comptes Rendus, 1884, vol. 99, p. 786; Mellor, Chemical Statics and Dynamics, 1904, pp. 435H136. 8 It appears that some French writers employ the term "facteur d'e'quilibre" as synonymous with "intensity factor of an energy." (Cf. F. Michaud, Ann. de Phys., vol. 16, 1921, p. 132.) 282 ELEMENTS OP PHYSICAL BIOLOGY repute/ with the result that a vagueness is introduced for which Le Chatelier himself cannot justly be made responsible. This vagueness is then often rendered still worse by departures from, the original wording, aimed at an extension of the scope of the hiw to all conceivable systems and "factors," an extension which is gained with a total sacrifice of all validity of the principle. So, for example, if we seek to apply the principle as quoted above, but omitting the restriction of the second paragraph, to the water equilibrium already mentioned, and if we select as "factor" of equilibrium not pressure but volume, the principle would lead us to reason as follows: On diminishing the volume of the system, that transformation will take place which, did it take place alone (i.e., at constant pressure), would be accompanied by increase in volume; a conclusion which is false. As has been shown by Ehrcnfest/ 1 the error arises through failure to discriminate, in the application of the principle, between the intensity factor (e.g., pressure) and the capacity factor (e.g., volume) of an energy. It must appear singular that so obvious a defect of the principle, as commonly quoted, should so generally have escaped attention, and should for example, have passed unnoted through seven cditionw of so excellent a work as Nernst's Theoretische Chemie. Khronfost points out that the explanation lies in the very vagueness of the principles, which permits it to be construed in each case to suit circumstances. The principle is commonly applied fix post facto, and its competence to predict thus escapes any serious test. This, however, is only a partial explanation. After all, the fundamental reason for the tardy recognition, and the still more tardy admission in the general literature, of the weakness of tho principle, an commonly quoted, must be sought in an inherent weakness of the human mind: by a curious inversion of what might be expected in logical sequence, the last things to receive critical scrutiny are always the fundamental premises of our arguments. This 'is true both as regards the judgment of the average individual, of the people ut large, and often even of the man of very superior intellect. One recalls, in this connection, MacAuley's remarks regarding Dr. Johnson: "How it chancedJhat a man who reasoned upon his 4 See, for example, W. Nernst, Theoretische Chemie, 1913, p 60S ' f' Sf ! iem" 19U' V L 77) P' 735 ' Cf' also e, 1911, vol. 1, p. 467. DISPLACEMENT OF EQUILIBRIUM 283 premises so ably should assume his premises so foolishly is one of the great mysteries of human nature." If such an outwardly slight departure from Le Chatelier's original enunciation as the omission of his second ' 'explanatory" paragraph, thus completely destroys the validity of his principle, what is to be said of such sweepingly vague settings as in the followingexamples : The broadest definition of the principle of Le Ghaielier is that a system tends to change so as to minimize an external disturbance (W. D. Bancroft, Journal of the American Chemical Society, 1911, p. 92). Every external action produces in, a body or system changes in such direction, that in consequence of this change the resistance of the body or system against the external action is increased. If we regard the faculty of adaptation of animals and plants from the point of view that the organisms undergo, under the influence of external actions, changes which render them more resistant to those actions, then the property of non-living matter which is expressed by the principle of Le Chatelier-Braun may be regarded as a sort of adaptation of such non-living matter (Chwolson, Trait6 de Physique, 1909, vol. 3, p. 547). If the equilibrium of a natural complex (system of masses, organism, system of ideas') is disturbed, it adapts itself to the stimulus (Reiz] which causes the disturbance, in such manner that the said stimulus continually diminishes until finally the original or a new equilibrium is again established (J. Lowy, Jvosmos, 1911, p. 331). The last two examples are of particular interest to us here as suggesting application of the principle to biological systems. As a matter of fact, such application of the vaguely formulated principle (in a form in which it would be injustice to link it with the name of Le Chatelier) antedates by many years its enunciation by the French physicist. The following passages in Herbert Spencer's First Principles a're pertinent : Among the involved rhythmical changes constituting organic life, any disturbing force that works an excess of change in some direction is gradually diminished and finally neutralized by antagonistic forces, which thereupon work a compensating change in the opposite direction, and so, after more or less of oscillation, restore the medium condition. And this process it is which constitutes what physicians call the vis mcdicatrix naturae, This is a conclusion which we may safely draw without knowing the special re-arrangements that effect the equilibration: If we see that a different mode of life is followed after a period of functional derangement by some altered condition of the system if we see that this altered condition, becoming by 284 ELEMENTS OF PHYSICAL BIOLOGY and by established, continues without, further change, wo havo no altornafcivo but to say that the now forces brought to boar on the wyHtom have boon compensated by the opposing forces they Imvo evoked (I . >= according as pi =; p6 . 3. It can be shown that, given (1) and (2), stability demands that the curves representing the relative between p (ordinates) and v (abscissae) must slope from left to right downwards. For if such a curve slopes in the opposite direction, then the slightest displacement from equilibrium will immediately cause the system to travel with cumulative effect, avalanche-like, along the pv curve further and further away from the starting point. 10 9 For justification of this and other statements made in those paragraphs the reader is referred to the author's paper already cited. It may be remarked that Ehrenfest (loc. cit.) expresses the belief that such broader scope belongs to the principle, but he does not support his impression with proof. 10 It is interesting to note that an upward slope, from left to right,, occurs in the middle limb of the van der Waals' pv curve of a gas. But this limb represents an unstable state which is never realized, the gas, instead of following this part of the curve, partially condenses and traces a horizontal straight line for the pv relation. 288 ELEMENTS OF PHYSICAL BIOLOGY Now these fundamental properties (1), (2) and (3), of a capacity and an intensity factor of an energy 11 are shared by certain parameters that have no direct or simple relation to energy whatsoever; and since the applicability of the principle depends upon these properties, it will extend to such other parameters possessing them. As an example may be mentioned the relation between area a occupied by a population, and the rent per unit area RI that an (average) individual is willing to pay. If .Ri is greater than Re , the rent at market rate, the individual will move into a more spacious apartment, and a will increase, and vice versa; so that == according as Ri = RB at ~^~ <~On the other hand the curves representing, in rectangular coordinates, the relation between rent and area available per head, necessarily slope from left to right downward. If it were true, as sometimes stated, that the more a man has, the more he wants, economic equilibrium would be an unstable condition. This example is presented here with reservation. There may be various complications in practice that may form obstacles to the simple application of the principle indicated. But it will serve to show how a perfectly rigorous justification may exist for the application of the principle of Le Chatelier outside the field of plain energetics and thermodynamics. Where, and only where such justification can be clearly shown to exist, there it will be permissible and useful to apply the principle. Applications made broadcast, without prior examination of the parameters involved, perhaps without any thought at all of reasonable parameters, are of little if any worth. One other word of caution must be said, for which the example of area and rent will furnish a suitable illustration. Before we apply 11 Owing to the custom of counting heat absorbed by a system as positive, but work done upon it as negative, the relation analogous to that of (2) takes the form, in the case of heat energy, dQ <- n ,. < ^ according as 9 j =0,Ql ^ where Q is the quantity of heat absorbed by the system at a temperature from a source at the temperature 0. Here the Qd curves slope upward from left to right. Cf. A. J. Lotka, loc. cit., p. 36. DISPLACEMENT OF EQUILIBBIUM 289 the principle to any particular parameter, we must be sure that the contemplated change will modify this parameter alone, and not also at the same time others that are in principle, if not in physical fact, to be regarded as independent. So, for example, one reason why the example of area and rent was presented above with express reservation is that, ordinarily at any rate, it may be difficult or impossible to modify the area of a population without modifying at the same time certain other features, such as the supply of nutriments furnished in the soil, etc. On the whole, so far, it must be said that the result of a careful analysis of the principle of Le Chatelier yields negative results, so far as practical application to biological systems is concerned. The chief conclusion is that great caution must be exercised in employing the principle. This result may be somewhat disappointing, but it is for that none the less important. Facts are stubborn things; it seems a pity to demolish the idol of a pretty generalization, but in such things we cannot permit the wish to be father to the thought. And the idol is not wholly demolished in fact his hitherto doubtful title to certain domains has been established on a clear basis. But his province must be recognized as very definitely bounded. DISCUSSION OF DISPLACEMENT OF EQUILIBRIUM INDEPENDENTLY OF LE CHATELIER'S PRINCIPLE In view of the limitations in the field of strict applicability of the principle of Le Chatelier, we are in general forced to consider separately each particular case of displacement of equilibrium. How such cases may be treated may be exemplified by the following two instances. Case 1. Displacement of Equilibrium between Food and Feeding Species. Consider a species $2 of mass Xz , which requires for its (equilibrium) sustenance of a mass k2Xz of food. Let this food be derived exclusively from the slain bodies, of total mass di XT,, of a species /Si. Let a fraction e of all the deaths in Si be those caused by S2 feeding upon Si. Then k2X2 = ediXi (1) -- 290 ELEMENTS OF PHYSICAL BIOLOGY It is generally in the interest of the species $2 to reduce this ratio to a minimum, especially in such a case as that of a domestic species Si, kept by man ($2) to provide him with flesh food. For the species Si itself consumes food, and is thus directly or indirectly a tax upon the system. In fact, the species Si is merely a sort of food factory for S2 , and the less of Si is required to produce the requisite amount of food kzX2 , the more efficient is *Si as a food factory. We may therefore enquire what the formula (2) tells us regarding the efficiency of Si as a food producer. Xi h It will be observed that the ratio a = = may be reduced Jiz etti in two ways by operating upon the species Si (operating on S2 , it might be reduced by diminishing 7e2 ; but we will exclude this from consideration) ; an increase in either e or in di will bring about this result of reducing a. Now e would be increased if the species $2 helped to protect S\ from its other enemies. This, of course, is one of the obvious expedients employed by man toward his domesticated sources of sustenance. XBut the species $2 may also operate to reduce the ratio a. = As A* by increasing di, and it may do this in several ways, etti We may write (3) (4) where Ni is the number of the population of Si} mi the mass per head of this living population, TO/ the mass per head of the individuals slain by SZ) and j is a factor, namely -, Evidently dij is the TTt/]^ death rate per head in the population Si; to simplify matters we may assume that j is (nearly) unity, so that d\ represents directly the death rate per head in Si. It is evidently possible to increase di} the death rate per head in Si, without disturbing the equilibrium, provided that the birth rate 61 is increased in equal amount. There are several ways of accomplishing this. The most obvious is systematic breeding. We may briefly consider the analysis of an ideally simple case in point. DISPLACEMENT OF EQUILIBRIUM 291 Let bi be the natural birth rate per head and di the death rate per head, in a population of NI individuals of a food species Si. Of the total deaths, let pNi occur through various other causes, while qNiN2 are clue to the destruction of Si by the species S2 that feeds upon Si. In equilibrium, then, we have &i - di = bi - qN'2 - p = (5) N2 = b ^2 (6) 9 Furthermore, let the species $2 , when in equilibrium, consume fNz individuals of species NI, so that #2 = qNiNz (7) Ni = ^ (8) Now let $2 "cultivate" the species $1, so that the birth rate of the latter is raised from bi to bi + aN2 . The conditions for equilibrium now are &i + ffNt ' - qNa' -p = (9) Nz ' = ^ (10) q-aNI = ' as before (llj The effect of this cultivation, then has been, in this case, to leave the population of Si, the food species, unchanged. But the feeding species S2 has increased in the ratio q-aThis result could hardly have been foreseen by the aid of the principle of Le Chatelier. In this argument it has been supposed, as a first approximation, that q is a constant. In point of fact q will no doubt be somewhat modified when the species Si is "cultivated" by Sa. The effect of such modification of q would then be superimposed upon the effect derived in the argument set forth above. 292 ELEMENTS OF PHYSICAL BIOLOGY Case 2. Change of Circulation through Moving Cycles. Among the moving equilibria in nature an important class are those which arise in systems traversed by matter in cyclic transformations. Consider a very simple example of a cyclic transformation chain, such as that in which, of three components Si, Sz , S3 , the first becomes converted into the second, the second into the third and the third returns to the first, after the pattern: 7 \$3 < -' $2 We may write the equations of the transformation _ _ _ ci (~y- y y \ n T" /-. Tf /'iv-ii, A, AS; ga^s g\A at dZ2 = dt ' "' dt ' ' where in the most general case gi, g2 , gs are each of them a function of Xi} X%} X$. When a steady state is established, so that the derivatives -7- Cvt vanish we have, evidently 7? ~Y -V /1 o\ A-i-^-z-^-s (Id; from which it is seen that, in the steady state, that component is most abundant, which has the slowest proportional rate of decomposition, the smallest g. This smaller g acts as a "bottle neck"12 in the cycle, causing material to accumulate in front of it. It acts as a brake, as a limiting factor, upon the rate of circulation through the system. 12 1 am borrowing this term from the language of efficiency engineers, who employ it to denote a point, in a consecutive series in industrial operations, at which the progress of work is arrested by a local "limiting capacity." DISPLACEMENT OF EQUILIBEIUM 293 If the total mass of Si, $ and Ss is in some way fixed, so that we put Xi + ^2 + Xa = M = const., we have, evidently, for a steady state jA. I ~~ . , ., , . _. . *' * * . ~~~ IrL \ 14:7 Similarly Xz = *W M. (15) X9 --M (16) f/l ~|- (72 + f/8 The circulation I, i.e., the mass circulating through the system per unit of time, is evidently given by M (17) tfi -I- f/a + f/a and .^/^.ff^lM.) OHi (r/i H- r/z -I- f > ' (/< l . '"*"''" co'"- rol reptiles DISPLACEMENT OF IIQUILIBRrUM 207 were swept on upon a tidal wave of unremitting growth, until their cost of living exceeded their earning capacity, until their very (strength proved their fatal weakness; unable to gather, in a day's run, sufficient food to fill their .monstrous paunch, they became the victims of their colossal ambition; their carcases remained enshrouded in the rocks, monumental wrecks by the wayside, where, the caravan of evolution has passed on. . . . . But there is another view which may account for this chapter in Natural History, as lias boon pointed out to me by Mr. ,1. !. S. Haldanc in correspondence the gist of which is, briefly, as follows: The large reptiles of the secondary age had large, pituitary glands. It was probably the secretion of these that determined their large size. Now a large animal has a high blood pressure- -a fact which is exemplified, in a way, in statistics of clinical observations on human material, witness table 32 p. 295. With high blood pressure there would be a tendency for the capillaries to leak. The thing that stops them leaking is pituitrin. Thus selection will tend to increase the pituitary gland in large animals. Unless it is possible for variations to arise increasing the output of pituitrin but not that of the anterior lobe, successive generations will tend to become bigger and bigger, till they ultimately perish of hyperpituitarism. 1 ' 1 Sometimes, it seems, the trend of evolution by a cumulative cydc may be grotesque rather than pernicious. This might well be the explanation of such singular vagaries as those observed, for example, in a group of fishes related to the shark. This series (fig. />{)) (to which my attention was drawn by Mr. J. T. Nichols of the American Museum of Natural History) exhibits progressive flattening of the body accompanied by thinning out of the tail, until the latter I'M reduced to a more lash.. Hero some gland controlling growth may have become increasingly active in response to selection operating on some useful quality, and meanwhile some secondary effect had to be taken into the bargain, regardless of utility. But cumulative cycles do not always work toward destruction or toward mere caprices devoid of utility. The effect of gathering momentum is equally potent in the constructive sphere. ' Perhaps' the most striking examples of this have occurred in the realm of 14 Somewhat similar views have boon oxprosHod by A. I I. Hturtcvant. Science 1924, vol. 59, p. 579. ' 2gg ELEMENTS OP PHYSICAL BIOLOGY mental phenomena. The oyc lfi and the hand have probably contributed more than any other single cireumstancn to the evolution of the human mind up to its present level. The possession of tin agile member gave opportunity for exercise of the menial faculties, this in turn reacted towards increased development, of the tactile sense and manipulative skill of the hand, and so on in a cumulative cycle. A similar "cumulative cycle" has probably had a, large part, in developing our faculty of speech. In the present stage of our development, we find it almost indispensable, in Ihinkiny, to use language, a vehicle whose primary function would seem to bo the transmission of thought from one individual to another, and which would seem wholly superfluous in the traffic of thought within the precincts of one mind, as money currency is needless in the giveand-take within the same household. Which, then came first, thought, or language? Neither, of course, can claim dear precedence. They must have developed together, in mutual stimulation. The habit of communicating thoughts to others- must have reacted upon the thinker and made him more perfect, first as a thinker, and then again, in turn, as a communicator of thought, as a speaker; and so, in a species of cycle, not vicious but benign, thought promoted speech arid speech furthered thought,, in an endless chain of cause and effect, such as thai; which we witness in the somewhat useless but rather entertaining spectacle of a wit chasing its tail, or (to turn from, the fine to the useful arts), in the economically more significant performance of the donkey urged to unwonted productive effort by the hope of (witching up with that elusive wisp of hay dangled by the driven' before the poor beast's nose. Cause and effect are so intermingled in a chain of alternations that they have become indistinguishable, To cite in third place a more modern instance, the mutually fertilizing influence upon each other of pure and applied science falls into the same class of benign cycles. Here also cau.se and effect are so intermingled that the relative merits of the two not very clearly separated branches of scientific endeavor are hardly 1B Of. G. H. Parker, Proc. Am. Phil. Soc-.., 1022, vol. 01, p. 107; alno (1. Elliot, Nature, 1923, vol. 112, p. 443. DISPLACEMENT OF EQUILIBRIUM 299 a subject for profitable debate. If, as some18 bold, "the final justification of science is the power it creates for the use of mankind/' then we must call to remembrance that this "power must be created before it is used."17 The instances cited should be sufficient to demonstrate how effectively resourceful nature makes use, in her economy, of instability, with its cumulative potency, as a progressive force; as well as of stability, the essentially conservative element in evolution. Indeed, we, of the human race, have good reason to be mindful of this fact, for the wholly unparalleled rapidity of our scientific and industrial evolution in past decades is itself the most brilliant example of instability and its cumulative power as a factor in evolution. 16 The writer is not among these, if by final justification is meant the only sufficient justification. No one would think of demanding such justification for art. Why require it of science? Such an attitude towards her is like that of the man who, having received repeated favors from his fellow, begins to acquire the habit, and to look upon such favors as due to him, and as the sole justification for the other's existence. 17 C. S. Minot, Science, 1911, p. 119. CHAPTER THE PARAMETERS OF STATE In dealing with any natural phenomenon especially one of a vital nature, with all the complexity of living organisms in type and habit the mathematician has to simplify the conditions until they reach the attenuated character which lies within the power of his analysis. Karl Pearson. Little has been said, so far, of the parameters P employed to define the state of the systems under consideration. In the earlier chapters these parameters have, in fact, been largely eliminated from discussion by restricting the treatment to the case of evolution under constant parameters P; subsequently the special cases of evolution with slowly changing P's, and the influence upon *| equilibrium alone of changes of unrestricted kind in the P's have been discussed; but all of this from a general standpoint, without giving much thought to the particular nature and properties of these parameters. It is desirable now to give some attention to this hitherto neglected phase of the subject. The simplest, and in many respects a very illuminating example of the nature and function of the parameters P is furnished in the thermodynamic treatment of physical systems. Here we are accustomed to the use of such parameters as pressure, temperature, surface tension, etc., to define the state of the systems under con- sideration. Topographic Parameters. Obviously there is much latitude in the choice of such parameters; for if any parameter P can be employed to define the state of a given system, any single-valued function F (P) of that parameter will also serve, though certain selections of parameters may be found much more advantageous in practice than others. In particular, it is found, in systems amenable to thermodynamic treatment, that P's can be so selected that they appear as the intensity factors of an energy. 1 This selection has actually been made in the example cited above. Or, alternatively, any one of the P's so selected, can be replaced by 1 Helmholtz, Die Thermodynamisch-chemischen Vorgange 1882 (Ges. < Abh., vol. 3, p. 958) ; P. Ehrenfest, Zeitschr. f. phys. Chemie, 1911, p. 234. \ 300 PAEAMETEES OF STATE 301 the extensity factor of an energy. So, in place of the pressure p we can introduce the volume v, these two parameters being connected by a functional relation of the form. v = (1) The parameter v (volume) is almost the simplest type imaginable of a topographic parameter. In many systems commonly considered in physical chemistry the only way in which the topography of the system plays any appreciable role in the processes going on therein is through the volume defined by the boundaries of the system. Even the shape of the boundary is in most cases immaterial. In the systems in which organic evolution is proceeding, the situation is very different. In one respect the topographic parameters are often, in this case, even simpler than in the physicochemical example, namely in this, that living organisms (except aquatic species) make their excursions, extend their activities, essentially in a space of two dimensions the earth's surface, or at least a rather thin shell near that surface. Hence we are interested in areas rather than volumes; in place of a parameter v, volume, we may expect to find figuring in the discussion a parameter a, area. But aside from this slight simplification (which does not always apply), the influence of topography in systems in the course of organic evolution is immeasurably more complex than in the simple physico-chemical systems that form the chief subjects of study in the laboratory and in theory. Indeed, the conditions presented in nature are so complex that we can hardly hope to construct any systematic mathematical analysis of this phase of the subject, except by the expedient of dealing in somewhat radical abstractions, such as evolution "in a uniform environment" or, perhaps, in an environment reproducing in very greatly simplified form some of those principal geographic features that are typical of our globe. There is something unsatisfactory in such abstractions that seem rather far remote from conditions actually met in nature. But it must be remembered that such abstractions are a necessary, and, as experience has abundantly shown, a very effective aid to our limited mental powers, which are incompetent to deal directly with unexpurgated nature in all its complexity. Neither should it be forgotten that the worker in the laboratory, though he may seem to be nearer to nature, himself is dealing essentially in abstractions. 302 ELEMENTS OF PHYSICAL BIOLOGY When the physical chemist investigates a chemical reaction in a constant temperature bath, he is not copying nature, where constant temperature is an exception, but is deliberately establishing an "unnatural" situation. He does this in order to separate the influence of one factor upon the course of events from that of a multitude of others; feeling confident that when he has gained an insight into the workings of such a simplified and, in a sense, unnatural system, he will be the better equipped to understand, or at least to make a further study of more complicated systems, approaching more and more nearly those occurring in nature. It is precisely the same principle which justifies us, in "substituting an ideal, upon which it is possible to operate, for intractable reality," 2 when we essay the systematic treatment of natural processes by mathematical analysis. So, for example, Karl Pearson in his memoir on Random Migration treats among others the case in which "breeding grounds and food supply are supposed to have an average uniform, distribution over the district under consideration;" 3 and the simple case of "migration into a cleared rectangular area," etc. Somewhat similar topographic simplicity is assumed as the basis of studies of Brownlee on the Mathematical Theory of Random Migration and Epidemic Distribution. We shall have occasion to refer to these studies again in another connection. It is not intended to follow up this phase of the subject here. Neither will any attempt be made to sketch here even in outline the empirical side of the subject, our observational knowledge regarding the dependence of life in its various forms upon the parameters of state. There is a ripe and extensive literature available on this special phase of biology, which it is unnecessary to duplicate here. It will suffice to refer to standard works on geographical biology and to general ecology. 4 2 Nature, 1922, p. 764. 3 Draper's Company Memoirs, Biometric Series III, 1906. 4 The following may be mentioned: A. Engler and 0. Drude, Die Vegetation der Erde, Sammlung pflanzengeographischer Monographien (a cyclopedic work in many volumes). A. F. W. Schimper, Clarendon Press, 1903, Plant Geography. E. Warming, Clarendon Press, 1909, Oecology of Plants. A. R. Wallace, 1876, The Geographical Distribution of Animals. F. E. Beddard, 1895, Textbook of Zoogeography. H. Gadow, Cambridge University Press, 1913, The Wandering of Animals. E. L, Trouessart, 1922, La Distribution Geographique des Animaux, PARAMETERS OF STATE 303 In physico-chemical systems the topographic parameter v (volume) is the capacity factor of an energy, as had already been noted; and associated with v is what may be termed a conjugate parameter Pi (pressure), which is the intensity factor of the energy in question, i.e., that factor which determines the direction of any change in the capacity factor v, according to the scheme = according as pi = pe (2) dt < ^ where pe is the external pressure. 5 The Intensity Law in Organic and Economic Systems. Is there anything corresponding to the relation (2), the Intensity Law, as it has been termed, in the case of the topographic parameter a (area) which enters into the definition of the state of a system in the course of organic evolution? This matter has already been referred to, in a way, in discussing the Principle of Le Chatelier. It was there noted that, in the case of human population area and rent are related to each other in accordance with a scheme of the type (2). More generally, supply and demand in economics stand in a relation of this type, and accordingly present a certain analogy to the capacity and intensity factors of an energy an analogy which, by some writers, has been construed as actual identity in kind, prices having, by these writers, been identified with the intensity factor of an "economic energy." Now energy is a perfectly definite, measurable thing, of definite dimensions. Those who thus speak of a special form of "economic energy" should be prepared to give us at least some indication how this energy is to be measured, in the customary units of energy. No such indication is forthcoming. On 6 The relation (2) is essentially the Helm-Ostwald Intensity Law. Although this law is not as universal as its sponsors would make it appear, yet it has a certain field of utility. For a critique of this law see M. Planck, Eight Lectures on Theoretical Physics, Columbia University Press, 1915, p. 11. The form of the relation (2) may be taken as the definition of a pair of conjugate parameters. However, the definition must be made a little more general to cover certain cases. We shall say that G, g are conjugate parameters if either dG ^ n > -5- < according as gt < ge (1) dG > . .. < -j- according as g. = g, (2) 304 ELEMENTS OF PHYSICAL BIOLOGY the contrary, as we shall see in dealing with the dynamics of evolution, the economic equivalent of a form of energy (which is something quite different from its mechanical equivalent), is not constant but variable though it tends to approach, or to fluctuate about, a certain value. On the mistaken identification of prices and related economic quantities with the intensity factor of an energy, some authors have sought to build a system of biodynamics (social dynamics). 6 The analogy which certain conjugate parameters of the perfectly general kind bear to intensity and capacity factors of an energy present the opportunity for such efforts, which are, in themselves, well worth while. But it must not be forgotten that the result of such efforts can be only a species of quasi-dynamics, something analogous to, but not identical with, the dynamics of physical forces. Just what the relation between such quasi-dynamics and true dynamics may be, is a separate problem, to which we shall have occasion to give some attention in the section devoted specifically to the dynamics of life-bearing systems. The paying of rent in coin of the realm is, of course, a phenomenon peculiar to the human species. But the peculiarity is one of mode of manifestation rather than of inherent quality. We may speak of the rent per unit area that the representative individual is willing to pay as a measure or at least an index of the "population pressure." Now this population pressure this willingness to sacrifice effort for the sake of gaining elbowroom is present quite independently of our peculiar method of expressing it in terms of rent. It exists also among other species, though we may lack so convenient a gauge for it as we have, in our own case, in rent. We shall see later how at least a quantitative conception of such biophysical (economic) entities as population pressure and the like can be gained on a general basis, which applies to species other than human. 6 Compare G. Helm, Die Lehre von der Energie, 1887, pp. 72 et seq.; Ostwald, W., Energetische Grundlagen der Kulturwissenschaften, Leipsic, 1909, p. 155. Die Philosophic der Werte, Leipsic, 1913, pp. 260, 314-317, 326, 328. Among other writers who touch on the subject of the relation of economic value and price to energy are : Budde, Energie und Recht, Leipsic, 1902, p. 56; Winiarski, "Essai sur la Mecanique Sociale," Revue Philosophique, 1900, vol. 49, p. 113. See also J. Davidson, Qu. Jour. Economics, August, 1919, p. 717. PARAMETERS OF STATE 305 For the present, without making here a closer analysis of the conjugate parameters a, p, (area, rent or population pressure) it will suffice to point out that the mere existence of the relation = according as p\ = pe (3) at < *^ may give into our hand the means of drawing certain conclusions regarding the behavior of the system, Quite independently of the intimate -nature of these quantities, a, p. In illustration of this it is only necessary to refer once more to the discussion of the principle of Le Chatelier in Chapter XXII. Distant Analogy to Gas Law. Again, still without any searching analysis of all the physical implications of the parameters a and p, we may note certain facts regarding the relation. a = $(P) Zlt Xt, . . . Xn) (4) which connects the conjugate parameters a, p, just as pressure p and volume v, in physico-chemical systems, are connected by the relation v = p(p, XL, Xa> . . .) (5) This latter, in the simple case of a gas takes the form v = m (6) P m. ,, , ., , or, since is the density d T = RT (7) d constant, at constant temperature Let N be the total number of a (human) population, a the area occupied by it, and Ni the total income of the population. Let p be the rent per unit area; and let the population spend a fraction R' of its income on rent. Then evidently pa = NR'i (8) 306 ELEMENTS OF PHYSICAL BIOLOGY A.r Putting = population density = d' we haveto a ~^R'i (9) a It will be seen that there is a certain analogy between the formulae (8), (9) as applied to the relation between rent (population pressure) and area occupied by a population, on the one hand, and the formulae (6), (7) as applied to the relation between the pressure p and the volume v of a gas. The analogy is particularly close if the income per head i, and the factor Rr are constant as a changes. The former may be true, approximately, if the inhabitants of area a derive their income from some extraneous source quite independent of this area. It will not be true, even in rough approximation, if the inhabitants derive their income from the produce of the area a itself. It is not the author's intention to emphasize unduly mere analogies. Nevertheless, the one here presented seems worthy of passing notice. Compare also E. Woodruff, Expansion of Races. The actual relation between population density and rent or land value is a subject of great economic interest. Research in this subject is in progress under the auspices of the Institute for Research in Land Economics, Madison, Wis., but has not, at this time of writing, matured to published results. Law of Urban Concentration. An empirical law of urban concentration was pointed out some years ago by F. Auerbach (Petermanns Mittheilungen, 1923, p. 74). Arranging in order of magnitude the cities of a given country, he found that the product of population and ordinal number (rank) was approximately constant. Thus, plotting rank against population, he obtained a hyperbolic curve, or, plotting the product of these two quantities, he obtained, roughly speaking, a straight line. For some of his curves the reader must be referred to the original publication. The illustration (fig. 60) shows the graph obtained by plotting the logarithm of the population of the cities of the United States (1920) against the logarithm of their respective rank. In the higher ranks only every fifth city has been plotted. It will be seen that, excepting cities of rank 4, 5 and 6, the plot does approximate quite closely to a straight line. The slope of this line, however, is not exactly unity, as demanded by Auerbach's law, but 0.93, so that the PARAMETERS OF STATE 307 actual law of urban concentration in the United States, in 1920, was, within the limits indicated, given by where P denoted the population of the city of rank R. ^ rOPULATiCFi (Tens of thoussndsj 3 4- 5 6 T 9 9 10 RANK CO UO 40 50 GO TO 09(5 SM FIG. 60. LAW OF URBAN CONCENTRATION Graph obtained by plotting as ordinates, on logarithnic scale, Population of United States Cities, and as abscissae the corresponding Rank (in order of magnitude), also on logarithmic scale. It may be left an open question how much significance is to be attached to this empirical formula. We shall meet with a similar relation in Chapter XXIII in dealing with Willis' theory of Age and Area. 308 ELEMENTS OP PHYSICAL BIOLOGY The Biological Background of Population Pressure. In the preceding paragraphs we have accepted it as a fact that there is at any rate some degree of relation between population density and the "desire for expansion" which finds expression, in the human species, in the willingness to spend a certain fraction of the income upon ground rent or its equivalent in interest and taxes upon real estate. It is not proposed to attempt here any searching analysis of the precise physical significance of this desire for expansion. But that it is ultimately referable to very cogent biological and physical factors is self-evident. The degree of crowding of a group of organisms affects both its death rate (mean length of life) and also its rate of reproduction, as well as, no doubt other significant vital fimctions. As Pearl and Parker7 remark, in their paper on the influence of population density upon rate of reproduction in Drosophila : It has long been known that degree of crowding of organisms in a given space, or the density of the population, has an influence upon various vital processes of the individuals composing the population. In the matter of growth Semper8 and before him Jabez Hogg showed that volume of water apart from food and other conditions has an influence upon the rate. This subject has again been studied recently by Bilski. 10 Farr11 showed that there is in man a definite relation between population and death rate. This old work of Farr has recently been gone over carefully and confirmed by Brownlee. 12 Drzwina13 and Bohn show that a particular concentration of a toxic substance, just lethal for a single individual in a given volume of water (working with such organisms as infusoria, planarians, hydra, tadpoles, etc.), will be sub-lethal if several individuals are present in the same fixed volume of water. Influence of Population Density on Rate of Reproduction. Pearl and Parker14 have determined experimentally the relation between rate of reproduction and the density of a population of Drosophila (fruit flies) in a universe of constant volume (glass bottle). This 7 R. Pearl, and S. Parker, Proc. Natl. Acad. Sci., vol. 8, 1922, p. 212. 8 K. Semper, Animal life as affected by the natural conditions of existence. Fourth Edition, London, 1890. 9 Cited from Semper, loc. cit, 10 F. Bilski, Pfliiger's Arch., vol. 188, 1921, p. 254. 11 W. Farr, Decenn. Suppl. Reg. Gen., 1861-1870. 12 J. Brownlee, Jour. Roy. Stat. Boo., vol. 82, 1919, pp. 34-77; vol. 83, 1920, pp. 280-283. 13 A. Drzwina and G. Bohn, C. R. Soc. Biol. Paris, vol. 84, 1921, pp. 917-919. R. Pearl and S. Parker, Proc. Natl. Acad. Sci., vol. 8, 1922, p. 212. PARAMETERS OF STATE 309 relation is found to resemble in form Farr's law for the death rate D in a human population of density d: log D = log a + k log d (10) in which a and k are constants. Pearl and Parker found log y = 1.54 - O.OOSz - 0.658 log x (11) 16 cS Of I 10 10 SO 3O ^0 &0 SO 70 ffO fl/fS PER BOTTLE FIG. 61. RELATION BETWEEN RATE OF REPRODUCTION IN DROSOPHILA (FRUIT FLY) AND DENSITY OF MATED POPULATION The circles indicate observed values; the drawn-out curve is computed according to equation (11). After Pearl and Parker. 310 ELEMENTS OF PHYSICAL BIOLOGY where y denotes the number of imagoes per mated female per \ and x denotes the mean density of the mated population (measured a s flies per bottle) over a sixteen-day period. The results obtainea by Pearl and Parker are exhibited graphically in figure 61, the small circles denoting observed values, and the drawn-out curve values computed by the formula cited above. It should be noted, however, that in Farr's law the coefficient k of log d is positive, whereas in the Pearl and Parker formula it is negative; death rate in- 40 "60 ~60 100 /10" 14$ 160 180 OF FLIES IN BOTTLE AT BBSfNMtf& FIG. 62. RELATION BETWEEN MEAN LENGTH OP LIFE AND POPULATION DENSITY IN DROSOPHILA The curve is a freehand smoothing of the observations indicated by the small circles. After Pearl and Parker. creases with population density, whereas rate of reproduction, in this series of experiments, was found to decrease as the density in- creases. Influence of Population Density on Duration of Life. The same authors have also investigated the relation between population density and duration of life in Drosophila. 15 Their results are shown graphically in figure 62. The smoothed curve exhibits a very interesting feature. While crowding unmistakably diminishes 1S R. Pearl and S. Parker, Am. Jour. Hygiene, vol. 3, 1922, p. 94; Amer. Naturalist, vol. 56, 1922, p. 312. PARAMETERS OF STATE 311 the average length of life, as one would naturally expect, the curve does not fall continuously from left to right, but has a maximum. The flies do not thrive best when they have the most ample space per individual; there is an optimum density which is best suited to their needs for company or for some other obscure factor supplied by a certain moderate amount of crowding. TOPOGRAPHIC PARAMETERS DURING PERIOD OF DIFFUSION Willis' Theory of Age and Area. As regards the influence of those topographic parameters which define the boundaries of the system, a special case arises during that period in the life of a body of organisms, when its spread has not yet extended to those boundaries. Certain aspects of the phenomena presented during this period of diffusion have been made the subject of a painstaking study, conducted with much originality of view, by C. J. Willis. 16 One may not agree in all points with Dr. Willis' conclusions, but the material of fact collated by him is in itself significant and of value. As Prof. W. Bateson in a review of this book remarks : "To have hit on a new method of investigating even a part of the theory of evolution is no common achievement, and that the author has done this cannot in fairness be denied." Dr. Willis' principal thesis is essentially this, that the area occupied by a biological species is a measure of its antiquity in evolution. To be more precise, and to quote the author's own words: ' The area occupied at any given time, in any given country, by any group of allied species at least ten in number, depends chiefly, so long as conditions remain reasonably constant, upon the ages of the species of that group in that country, but may be enormously modified by the presence of barriers, such as seas, rivers, mountains, changes of climates from one region to the next, or other ecological boundaries, and the like, also by the action of man and other The thesis, thus stated, is "well hedged" with qualifications. Professor Bateson remarks: "Every evolutionist agrees that, apart 16 Age and Area: A Study in Geographical Distribution and Origin of Species; Cambridge University Press, 1922. For review see Nature, 1923, p. 39; Science Progress, January, 1923, p. 474. 312 ELEMENTS OF PHYSICAL BIOLOGY from disturbing elements, area is a measure of age. 17 .... We are, however, asked to believe that in practice this mode of estimating the age of a species is, on the whole, trustworthy; that endemic species and varieties in general can and must be for the most part accepted as new starters in evolution, and not as (remnants of) survivors." Dr. Willis supports his views by observations gathered chiefly in Ceylon and New Zealand. His evidence is not altogether convincing. Professor Bateson in the review already quoted remarks pointedly: "On any theory of evolution endemics (and rare species) must be in part novelties and in part relics; but why, apart from the theory of Age and Area, we should believe that endemics are in such great majority novelties I do not clearly understand, for though we know little of origins, we are certain that myriads of species have become extinct. It is surely contrary to all expectation that the process of extinction should be in general so rapid, and the final endemic phase so short that the number of species in that final stage should be so insignificant." Referring to the same point A. G. Thacker remarks: "Species and genera do die out, and therefore there are diminishing ranges as well as expanding ranges. . . , . Dr. Willis thinks that veiy few of the small range species are, in fact, decreasing. 55 For a further critique of the theory of Age and Area the reader may well be referred to the two reviews already cited, while Dr. Willis 5 own presentation of his case will be found expanded in detail in his book Age and Area, Cambridge University Press, 1922. Quite recently (I add this in correcting proof) Prof. G. V. Yule has lent his able advocacy to Willis 5 theory in an extensive paper published in the Phil. Trans. Roy. Soc., 1924, vol. 213, Series B, pp. 21-87, Some of the assumptions underlying Professor Yule's argument do not seem to commend themselves to the critical reader, in particular his supposition that 17 '"'Tor this and other reasons Dr. Willis 5 findings seem hardly competent to furnish a basis of attack against any otherwise established or suggested theory of evolution. On this point Dr. Willis himself does not seem wholly consistent, for though he advises in one place that it would be 'wiser to abandon natural selection 5 as the general principle that has guided evolution, in another place he admits that 'nothing can come into lasting existence without its permission.' This admission is all that any thoughtful adherent of any theory of evolution asks. 55 A. G. Thacker, The Dynamics of Distribution, Science Progress, 1923, vol. 17, p. 474. PARAMETERS OF STATE 313 the number of new species thrown is independent of the number of individuals. Turning from the theoretical and debatable portion of Dr. Willis' contribution, to the factual material presented by him, we are confronted by a number of very remarkable relations, such as those represented graphically in figure 63. In this drawing ordinates represent the number of genera in the several natural families of plants and animals indicated, and the corresponding abscissae represent the number of species in each genus plotted. So, for example (fig. 63), of the family Cornpositae 1143 genera were noted, as follows: 446 genera of 1 species 140 genera of 2 species 97 genera of 3 species 43 genera of 4 species 55 genera of 5 species etc. An examination of these drawings clearly brings out the following facts: The rnonotypic genera, with one species each, are always the most numerous, commonly forming about one third of the whole group; the ditypics, with two species each, are next in frequency, genera with higher numbers of species becoming successively fewer. Set out graphically as in figure 63, the genera exhibit what Dr. Willis calls a "hollow curve" of frequency (in point of fact a hyperbola of the generalized type), and, as Professor Bateson remarks, there is no gainsaying the fact that these curves, though collected from miscellaneous sources, have a remarkable similarity. Perhaps more striking still is the relation established in figures 64, 65, and 66. The quantities plotted here are of the same character as in figure 63, but they are plotted on a doubly logarithmic scale, with the remarkable result that the graphs obtained are in close approximation straight lines. Thus if x denotes the number of species in a genus, and y denotes the number of genera comprising x species, we have log x + a log y b = (12) or xy = const* (13) 314 ELEMENTS OF PHYSICAL BIOLOGY that is to say, the variables x and y are connected by a hyperbolic 18 relation. It should be noted that this relation covers a wide variety of cases, including both plants and animals. Monospecific Genenaal this end of curvs o Linepf GeneraJ of 5spp. MIXED CURVES The large dots represent the Origins By courtesy of Nature dumber of species for size of area.) Mi T d h "OT CUrVeS ' ^^"-^" !?"? ^ Beginning of each are thenumbers of monotypes. FIG. 63. HYPEHBOLIC CORVES OBTAINED BY PLOTTING AS ORDINATES THE-\USIBBB OF GBKEBA HAvmc 1, 2, 3, . . . n SPECIES, AND AS ABSCXSSAE THE N0MBEE n OP SUCH SPECIES The last curve above shows as ordinates the number of species of endemic compositae in the Galapagos Islands, as abscissae the corresponding areaso\er which such species have spread. After J. C. Willis. **** **" ^h^erbola *V = const, falls as a PARAMETERS OF STATE 315 Mumber of spacfes 10 20 30 40 50 100 1-0 1-2 1-4 16 1-8 2-0 log (N 9 of species) -2 -4 JS# courtesy of Nature FIG. 64. RELATION BETWEEN NUMBER AND SIZE OF GENERA op ALL PLANTS, PLOTTED LOGARITHMICALLY After J. C. Willis NS of species 10 30 10.000 100 8 "Tb"~" 1-2 log fN? of species) By eourttty of Natws FIG. 65. RELATION BETWEEN NTTMBEE AND SIZE OF RTOIACBAK Pr.OTran LOGAEITHMICALLT After J. C. Willis 316 ELEMENTS OP PHYSICAL BIOLOGY Dr. Willis' interpretation of the remarkable curves obtained by him may be quoted in his own words (Nature, February 9, 1924, p. 178): If species of very limited area and genera of one species (which also have usually small areas) are, with comparatively few exceptions, the young beginners in the race of life, and are descended in general from the species of wider dispersal and the larger genera, and if the number of species in a genus is, broadly speaking, a measure of its age, the idea at once suggests itself that a Number of species FIG. 68. RELATION BETWEEN NUMBER AND SIZE OF GENBEA OF BEETLES, PLOTTED LOGARITHMICALLY After J. C. Willis given stock may be regarded as "throwing" generic variations much as it throws offspring, so that the number of genera descended from one prime ancestor may be expected to increase in geometric ratio or according to the law of compound interest. The number of species descended from one ancestor might be expected to follow the same form of law with a more rapid rate of growth. On such a very rough conception it is found that the form of frequency distribution for sizes of genera should follow the rule that the logarithm of the number of genera plotted to the logarithm of the number of species gives a straight line. PAEAMETBBS OF STATE 317 It follows from the conception stated that the excess of the slope of the line over unity should measure the ratio of the rate of increase of genera to that of species. The slope should always, therefore, lie between the limits 1 and 2, for a slope of less than unity would have no meaning, and a slope exceeding 2 would imply that generic variations were more frequent than specific variations. Hitherto no exception has been found to the required rule. One group of fungi tested (Hymenomycetineae) gave a line with a slope very little exceeding unity (1.08), but the figures found for flowering plants lie between the narrow limits 1.38 and 1.64, with an average of about 1.43. Snakes and lizards both give a figure very near 1.50, and the Chrysomelidae about 1.37. For further details the reader must be referred to Dr. Willis' book Age and Area, and to a paper by E. S. Pearson, in Biometrika, August, 1923, vol. 15, of which the following passage, part of that author's conclusions, may be quoted: There is no doubt that these principles represent a certain aspect of the process of evolution, but I believe that Dr. Willis has stressed their importance beyond the limits which the evidence of observation will bear. They cannot explain everything, and we have seen that in many cases results which we are led to predict with their assistance are scarcely borne out, while in other cases recurrent distributions can also be accounted for on different hypotheses. Climatic Parameters. The state of a physico-chemical system is commonly described in terms of its temperature (in addition to pressure, etc.). Without attaching any deep significance to the analogy, it may be remarked that systems in which organic evolution is under way commonly require, as essential parameters to define their state, the statement of sundry quantities that describe climatic conditions, such as temperature, humidity, precipitation, light, etc. The influence of these upon the course of events must form an essential part of the study of evolution in life-bearing systems. The investigations of the influence of temperature upon metabolic processes an approximate doubling of reaction velocities for every 10C. rise in temperature we shall here note only very briefly as belonging rather to the field of biochemistry than to the more strictly ecological studies in which we are here interested. More in the line of our immediate interests are certain data gathered in oceanographic researches, which have already furnished us with much illustrative material. The influence of light, temperature, and 318 ELEMENTS OF PHYSICAL BIOLOGY C02 concentration is discussed by G. W. Martin in his paper already cited. 19 He remarks: Plants on land receive the full benefit of the sun's rays as we know them. Plants living under water receive only a portion of the rays that reach the land. Part of the light that strikes the water is reflected, and the part that penetrates the water is gradually absorbed in passing through that medium, the red and yellow rays first, the blue and violet last. This differential absorption is reflected in the curious and well-known distribution of marine algae according to color the green kind growing in shallow water, the brown in an intermediate zone, and the red in the deepest water, although there are, of course, numerous exceptions to this general rule of distribution. Another property FIG. 67. SOLUBILITY OP CARBON DIOXIDE IN WATER, EXPRESSED IN VOLUMES OF C02 MEASURED AT NORMAL TEMPERATURE AND PRESSURE, PER VOLUME OF WATER After G. W. Martin of light is that it is refracted by water, and the greater the angle at which the rays strike the water, the greater will be the refraction. In the tropics, where the rays are practically vertical, the amount of refraction is insignificant, but in high latitude, where the rays strike the water at a sharp angle, the refraction is marked, as a result of which the rays are bent into a more nearly vertical direction, thus increasing their penetration in depth, and partly compensatingfor the unfavorable angle at which they strike the water. Helland Hansen was able to show that in the Atlantic Ocean south of the Azores, on a brightsummer's day, light is abundant at a depth of 100 meters, still including at that depth a few red rays. At 500 meters the red rays have completely disappearedbut blue and ultra-violet rays are still plentiful, and may be detected at 1000 19 G. W. Martin, Scientific Monthly, 1922, p. 456. PARAMETEKS OF STATE 319 meters, but have completely disappeared at 1700 meters. It is not probable, however, that under the most favorable conditions photosynthesis may be carried on at depths greater than 200 meters. Temperature is less directly important in the sea than on the land since there is no great danger of injurious extremes being reached. Indirectly, its importance lies in the fact that carbon dioxide is much more soluble in cold water than in warm (see fig. 67) and it is probably this, rather than the direct influence of temperature, which accounts for the fact that the most luxurious development of plant life is in the colder waters of the earth. Among laboratory investigations of the influence of "climatic parameters," under controlled conditions, may be reckoned the work of R. Pearl and S. Parker in their studies "On the Influence of Certain Environmental Factors on the Duration of Life in Drosophila." 20 In these experiments it was found, for example, that certain species of flies, kept in bottles closed by a single layer of silk bolting cloth ("ventilated bottles"), had 10 per cent longer life, on an average, than similar flies kept in bottles whose neck was plugged with cotton wool. PARAMETERS OF STATE AND THE ANALYTICAL CONDITION FOR EQUILIBRIUM In the fundamental equations both of the Kinetics and of the Statics of material transformations, as set forth in earlier chapters, the coefficients are in general functions of the parameters of state, and it is only on the supposition that evolution is proceeding under essentially constant conditions of topography, climate, etc., that these coefficients could be treated as constants. Furthermore, since these same coefficients enter into the analytical conditions for equilibrium, as set forth in Chapter XII, these conditions must be read in the sense that they hold true when certain specified parameters of state are held constant. If another set of parameters, instead, is held constant, the equilibrium conditions will retain the same form, but the values of the coefficients will change accordingly. This is precisely analogous to the state of affairs regarding the thermodynamic conditions for equilibrium Generally it can be said that in equilibrium the thermodynamic potential is a minimum, but the expression for this potential will 80 Arner. Naturalist, vol. 56, 1922, p. 385. 320 ELEMENTS OF PHYSICAL BIOLOGY vary according as pressure and temperature, or volume and temperature, for example, are held constant. In concluding this section it is desirable to call attention to a modification, in outward form, of which the analytical condition for equilibrium, Q' = minimum, dQ' = (14) (see Chapter XII) is susceptible. Since certain parameters pi, j?2, . . . are to be held constant in the application of this condition, the addition of a set of terms PI dpi + P2 dpz -f . . .to the expression 8Q' for a small virtual displacement will in nowise alter its value. We may, then replace the condition (14) by the fully equivalent one dO' dQ' = (d$)p = ^ dXi -f ^dXs + . . . -f Pidpj. + P2dp, + . . . (15) where the subscript p denotes that the parameters pi, p2, . . . , conjugate to the parameters P1} P2, , . . . are to be held constant in forming the expression (15). This statement of the condition (15) adds, of course, nothing new to the case. It is mentioned here only on account of its formal agreement 21 with the similar conditions for equilibrium which, as already pointed out, play an important role in thermodynamics. However, in the analogous equations erf thermodynamics the expression d $ is a complete differential. In the present instance we have no basis for the supposition that (15) is the true differential of a function $ (Zi, Z2 , PI, P2 , . . .) The question may, indeed be raised, whether by a suitable choice of parameters and variables it can be achieved that (15), in the case here under consideration, is such a complete differ- 21 Compare, for example, Van Laar, Seehs Vorlesungen iiber das thermodynamische Potential, 1906, p. 43. This formal agreement seems to extend also to another feature The thermodynamic condition for stable equilibrium demands that the second differential (d**) p shall be positive, and this in turn demands that ^shall be negative. (See M. Planck, Thermodynamik, 1905, pp. 134, 190; Duhem, Traite d'Energ^tique 1911 vo . 1, p. 466; A. Winkelmann, Handbuch der Physik, 1906, vol. d, p. o90.) Similarly, in the general case, stability demands that if Q, g are conjugate parameters of the type (1) of footnote 5, then ^- < 0. PARAMETERS OF STATE 321 ential. But this is a separate problem, on which we shall not here expend further effort. Only this shall be noted in passing: Whereas, in the thermodynamical treatment of physico-chemical phenomena a function <3? is given (essentially as the expression of the laws of thermodynamics), and whereas certain consequences are derived from this known function, the type of problems with which we are here concerned is of inverse nature. We are given certain data regarding the behavior of these systems, for example, the fact that their evolution follows more or less closely a system of equations of the type of the general equations (1) (Chapter VI) of the Kinetics of material transformation; and the problem may be raised, as to whether there exist functions $ analogous to the functions known as thennodynamic potentials, in terms of which the behavior of the system can be concisely epitomized, after the manner of thermodynamics. If such a plan could be successfully carried out, the result would be a species of quasi-dynamics of evolving systems, in which certain parameters P played a rdle analogous to forces, without being in any sense identical with forces (or even with generalized forces); certain other conjugate parameters p would play a role analogous to displacements, and certain functions <& would resemble in their relations to certain events in the system, the energy functions $ (free energy, thermodjrnamic potentials) of thermodynamics. That certain isolated portions of such a general system of quasidynamics have some degree of viability seems probable. Whether the general system is capable of development in a form possessing any considerable utility shall here be left an open question. For at this point we shall leave the path followed so far, and shall strike out in a new direction, with a view to sketching, not a system of quasi-dynamics or quasi-energetics, but the dynamics and energetics, in the strict sense, as ordinarily understood, of life-bearing systems in the course of evolution. PART IV DYNAMICS UK*. CHAPTER XXW THE ENERGY TRANSFORMERS OF NATURE Die Natur hat sich die Aufgabe gestellt das der Erde zustromende Licht im Fluge zu erhasehen und die beweglichste aller Krafte, in die starre Form verwandelt, aufzuspeiehern. Zur Erreichung dieses Zweckes hat sie die Erdkruste mit Organismen iiberzogen,welche iebend das Sonnenlicht in sich aufnehmen und unter Verwendung dieser Kraft eine fortlaufende Summe chemischer Differenzen erzeugen. Diese Organismen sind die Pflanzen. Die Pflanzenwelt bildet ein Reservoir, in welchem die fliichtigen Sonnenstrahlen fbdert und zur Nutzniessung geschickt, niedergelegt werden. /. R. Mayer. We approach now the third and last stage in our enquiry, toward which all that has gone before may be said, in a way, to have been in the nature of preparation. The fundamental equations of kinetics d ^=Fi (X1 ,Xi , . . .;P,Q) (1) dt may appear at first sight to contain no hint of dynamical, of energetic implications. These can be read into the equations only by calling to mind the physical nature of certain of the components whose masses X appear in the equations : These components aggregates of living organisms are, in their physical relations, energy transformers. The evolution which we have been considering, and shall continue in this last phase to consider, is, then, essentially the evolution of a system of energy transformers; the progressive redistribution of the matter of the system among these transformers. The dynamics which we must develop is the dynamics of a system of energy transformers, or engines. 1 Fundamental Characteristics of Energy Transformers. We shall do well to begin by calling to mind some of the fundamental elements or characteristics of energy transformers or engines, and of the manner of their working. An engine, such as a steam engine, for example, receives energy from a source such as a coal fire. This energy is absorbed by a working substance (water or steam), which, in the proc- 1 See also A. J. Lotka, Jl. Wash. Acad. Sci., 1924, p. 352. 325 326 ELEMENTS OF PHYSICAL BIOLOGY ess, undergoes modification or change of state (in a general sense of the term) ; the working substance, at some stage in the operation of the engine, again gives out energy, of which a part in engines of human construction, commonly appears in a particular, selected form adapted to some end useful to and purposed by the maker or owner. Another fraction of the energy discharged by the working substance, is passed on to a sink or absorber of energy, which may be simply the surrounding air, or in the case of a naval engine it may be the sea water employed to cool the condensed steam before it returns to the boiler. This discharge of a portion of the energy from the source into a sink is practised, not designedly because any useful purpose is served thereby, but unavoidably because, in the case of all forms of heat engines, the second law of thermodynamics inexorably demands this payment of a tax to nature, as it were. Cyclic Working; Output and Efficiency. A finite change of the working substance, performed just once, can yield only a finite amount of work. Hence an engine of this type, in order to operate continuously so as to furnish a steady supply of energy of indefinite amount, must of necessity work in a cycle, returning periodically to its initial state many times. For a given engine, working under given conditions, the total output W/t per unit of time is proportional to the quantity M (mass) of working substance and its frequency of circulation, n, per unit of time, through the cycle; thus W ~~kMn (2) Regarding the variation in the output for different engines, and for operation under different conditions, two fundamental laws of the greatest theoretical and practical importance, the very corner-stones of the edifice of thermodynamics, inform us that 1. The maximum output of which a heat engine is capable under ideal conditions of working is independent of the nature of the working substance, and of the details of mechanism and construction of the engine. 2. This maximum output obtainable under ideal conditions of operation depends solely upon the temperature of the source and that of the sink; with a suitably chosen temperature scale the law of the maximum output W can be put in the extremely simple form W=Q~~ (3) -i a 327 ENERGY TRANSFORMERS OF NATURE where Q is the energy drawn from the source, T the (at).. ^ temperature of the source, and ^ that of the sink. The ratio -Q which measures the fraction of the energy Q converted into woi ^ spoken of as the efficiency of the transformer. ^ j The actual performance of a heat engine always falls shoit - ^ usually far short of the theoretical maximum (3) attainable ideal conditions of reversible operation, whereas all real pio "~ ' '77 I llO as has been pointed out in an earlier chapter, are irreversible. first service rendered by the laws of thermodynamics is thus a neg "lIlMPV live one, to save us from vain efforts to achieve the impossible, tell us what we cannot do; they give us no guarantee as to what we c( do, in this matter of engine efficiency. In other fields these same principles are, indeed, found competent to yield us information most positive character, as the physicist and physical chemist know> from boundless wealth of example; the very fact that they hold independently of substance and form lends to their application a catholicity hardly equalled elsewhere in science, and at the same time givfv into our hands an instrument of the most extreme economy of thought, since we are relieved, in such application, of the necessity of treating each particular case, with all its complication of detail, on its own merits, but can deal with it by the short cut of a general formula. Still, the austere virtue of this impartiality with respect to substance and form becomes something of a vice when information is sought' regarding certain systems in which mechanism plays, not an incidental, but the leading role. Here thermodynamics may be found powerless to assist us greatly, and the need for new methods may bo folk The significance of this in our present concerns will be seen as the topic develops. Composite and Coupled Transformers. The simplest typo of transformer of the kind that here chiefly interests us would comprise one working substance fed from one source and discharging to omi sink. Two or more such transformers may, however, work in paralln! from one source, thus forming in the aggregate one composite trariK" former. Or, two or more may be coupled in series or cascade, tho, sink of one functioning as the source for the next of the series. Ho, for example, W. L. R. Emmett has constructed a composite engine, consisting of two separate engines, the first operating with mercury 328 ELEMENTS OF PHYSICAL BIOLOGY for its working substance, at a higher temperature, and the second operating with water at a lower temperature. It is to be observed that two such "coupled' 7 transformers again constitute a transformer, a compound transformer, which may possess certain special virtues, from the standpoint of the engineer, or in other respects. Accumulators. A special type of transformers is that in which the energy is transformed into a latent form, and is thus stored up for future use. A great variety of accumulators are in technical use. In the simplest case such an accumulator may consist of empounded water or a raised storage tank, ready upon the opening of a sluice or a valve to discharge its stored up energy. More closely akin to the systems in which we are here primarily interested is the lead accumulator or secondary battery, in which electrical energy is transformed into and stored as chemical energy, somewhat as the energy of sunlight is, in the leaves of plants, transformed into chemical energy and stored up in the form of starch. This type of chemical storage is of very particular interest because of the remarkable phenomena to which it is competent to give rise through the circumstance that the substance in which the energy is stored in chemical form is itself the working substance of a transformer. For in that case, if a mass TiM stores an amount of energy IT 7 , we have, according to (2) for a small interval of time dt dW hdM T IF" IT-**71 (4) If the transformer functions at a constant rate (i.e., with a fixed number of cycles per unit of time) and if the coefficient k is independent of the size of the transformer, we have by integration of (4) kn M = MQe~h (5) The transformer under these conditions, grows according to the law of compound interest. 2 For small ranges of size the assumption of a sensibly constant k is reasonable, and the law thus deduced may be expected to represent the facts tolerably well. For greater range we must regard k as a function of If and write k = a + b M + c M2 + . . . (6) 2 Compare L. J. Briggs, The Living Plant as a Physical System Jour Wash. Acad. Sc., 1917, vol. 7, p. 95. ENERGY TRANSFORMERS OF NATURE 329 so that (4) becomes ^=n(a+6M+. . .) (7) Mdt In second approximation, therefore, (breaking off the bracketed series at the second term) we find for the law of growth of the transformer the Verhulst-Pearl law (see Chapter VII). where m = M + a/6 and the subscript zero denotes the value of the variable at the instant t = 0. Anabions and Catabions. The living organism partakes of the functions both of an energy accumulator and of an energy dissipator. The former function is especially marked in plants and in the young growing organism. Biological terminology speaks of the process of energy accumulation by the growth (synthesis) of the working substance as anabolism, and of the liberation of the stored energy with conversion into other forms as catabolism. Organisms in which anabolic processes predominate are conveniently classed together as anabions (plants), those in which catabolic processes predominate, as catabions (animals). The line of division cannot be sharply d) awn, a fact which was commented upon in some detail in the first chapter. But in the majority of cases organisms have a pronounced bias toward one or the other of the two forms, and no difficulty arises in classifying them. We may form the conception of a system of transformers comprising, in the most general case, individual single transformers, aggregates of composite transformers, and coupled transformers; some or all of which may partake in greater or less degree of the nature of accumulators. It is precisely such a system of transformers that is presented to us, on a vast scale, in nature, by the earth with its population of living organisms. Each individual organism is of the type of the simple transformer, though it does not operate with a single working substance, but with a complex variety of such substances, a fact which has certain important consequences. 330 ELEMENTS OF PHYSICAL BIOLOGY Plant and Animal as Coupled Transformers . Coupled transformers are presented to us in profuse abundance, wherever one species feeds on another, so that the energy sink of the one is the energy source of the other, A compound transformer of this kind which is of very special interest is that composed of a plant species and an animal species feeding upon the former. The special virtue of this combination is as follows. The animal (catabiotic) species alone could not exist at all, since animals cannot anabolise inorganic food. The plant species alone, on the other hand, would have a very slow working cycle, because the decomposition of dead plant matter, and its reconstitution into C02 , completing the cycle of its transformations, is very slow in the absence of animals, or at any rate very much slower than when the plant is consumed by animals and oxidized in their bodies. Thus the compound transformer (plant and animal) is very much more effective than the plant alone. We shall have occasion to refer to this matter again. It is, of course, conceivable that the anabolic and catabolic functions should, in their entirety of a complete cycle, be combined in one structure, one organism. Physically there is no reason why this should not be, and, in fact, nature has made some abortive attempts to develop the plant-animal type of organism; there are a limited number of plants that assimilate animal food, and there are a few animals, such as Hydra viridis, that assimilate carbon dioxide from the air by the aid of chlorophyll. 3 But these are exceptions, freaks of nature, so to speak. For some reason these mixed types have not gained for themselves a significant position in the scheme of nature. Selection, evolution, has altogether favored the compound type of transformer, splitting the anabolic and the catabolic functions, and assigning the major share of each to a separate organism. The several individual organisms of one species form in the aggregate one large transformer built up of many units functioning in parallel. 3 Hydra viridis, however, is probably not a single organism, but an organism of the animal type harboring in its body separate plant-like organisms with, which it lives in symbiosis. ENERGY TRANSFORMERS OF NATURE 331 And lastly, the entire body of all these species of organisms, together with certain inorganic structures, constitute one great world-wide transformer. It is well to accustom the mind to think of this as one vast unit, one great empire. The "World Engine. The great world engine in which each of us is a most insignificant little wheel has its energy source, its firebox, so to speak in the sun, 4 ninety-eight million miles away from the working substance (the "boiler"). From the engineer's standpoint this would be an execrably bad design, if a high efficiency alone were the aim in view. For of the five hundred thousand million million million horsepower which the fiery orb radiates into space year in, year out, a ridiculously small fraction 2 is intercepted by the earth. It would take more than two billion, earths placed side by side to form a continuous shell around our sun at the earth's distance, and thus to receive the total output of solar heat. The other planets receive corresponding amounts. The remainder of the sun's disbursements sweeps past us into the depths of space, to unknown destiny. Of the energy that reaches the earth, 35 per cent is reflected (principally from the clouds), and 65 per cent is absorbed. The surface of the solid globe receives on an average 5 not quite 2 gramcalories (1.94) per square centimeter, placed normal to the beam, per minute, or enough heat to melt a layer of ice 424 feet thick every year. Arrhenius8 quotes Schroeder to the effect that about 0.12 per cent of this energy is absorbed by the green vegetation, the gate of entrance through which practically 7 all the energy taking part in the 4 The recognition of this fact is credited by Herbert Spencer (First Principles, 172, footnote) to Herschel (Outlines of Astronomy, 1833). 5 C. G. Abbot, The Sun, 1911, p. 298. In the tropics, at noon, a plot of 250 acres receives energy at the rate of one million horsepower (W. W. Campbell, Science, 1920, vol. 52, p. 548). 6 Jour. Franklin Inst., 1920, p. 118. Compare also G. Ciamician, Die Photochemie der Zukunft (Sammlung Chemischer Vortrage, 1922, p. 429). Asstiming an area of one hundred twenty-eight million square kilometers as inhabited by plants, Ciamician computes that thirty-two billion tons of dry matter per annum is produced, the equivalent of 17 times the world's annual coal production. 7 Certain bacteria whose metabolism is based on iron, sulphur or selenium derive their energy from other sources. They are thus independent of sun- 332 ELEMENTS OF PHYSICAL BIOLOGY life cycle must pass. And of this last amount only 24 per cent falls to plants cultivated for human needs.8 The forests take the major share, 67 per cent; 7 per cent falls on the grass steppes, and 2 per cent on desert plants. If these figures leave the mind somewhat confused with detail, it may assist the imagination to form an adequate picture of the life cycle in its totality if we reflect that the total energy thus corn-sing through the system every year is of the order of 22 times'5 the world's annual coal production. Conversely this statistical fact may serve to form for us a correct estimate of the really cosmic magnitude of human interference with the course of nature. The organic circulation, the living part of the world engine, though to us of most direct interest, is quantitatively speaking only a small part of the whole. If the organic cycle gives occupation to an amount of energy of the order of 20 times the world's coal consumption, light a fact of the greatest significance in connection with the problem of the origin of terrestial life as we know it today. For green plants carry on their life business by the aid of chlorophyll, a substance representing a high degree of specialization, such ae could not very well be supposed to exist in the most primitive life forms. 8 H. A. Spoehr, Jour. Ind. and Eng. Chem., 1922, vol. 14, p. 1144. Regarding the efficiency of cultivated plants in recovering solar energy for the use of man, the calculations of H. A. Spoehr are of interest. On the basis of 1.5 gram calories per square centimeter per minute for the value of the solar radiation received at the earth's surface, he computes the daily energy income per square meter (six hours insolation) as 5400 kilogram calories. Figuring the heat of combustion of coal at 8000 kilogram calories, this gives the equivalent of 0.675 kilograms of coal per square meter, or 16.4 tons of coal per acre. For ninety days of insolation this represents the equivalent of 1476 . 63 tons of coal. Spoehr then proceeds to obtain a figure for the efficiency of a wheat crop in the utilization of this energy. Assuming a large yield of 50 bushels or 17 . 619 hectoliters per acre, and considering this entirely as starch, we find an energy equivalent of 0.623 ton of coal. The efficiency here, then, is measured by the , - 0.623 very low figure - = 0.0004 = 0.04 per cent. 14/0 It should be noted, however, that not all the heat absorbed by the plant appears stored up in the body of the plant. A large amount is used up in the work of evaporation (transpiration). According to L. J. Briggs (Jour. Washington Acad., 1917, p. 92; Journal Agr. Research, 1914, pp. 1-63), the energy stored by the plant represents from 1 to 5 per cent of the energy dissipated during the growth of the plant. See also C. L. Holsberg, Jour. Ind. Eng Chem., 1924, vol. 6, pp. 524-525: Progress in Chemistry and the Theory of Population. ENERGY TBANSFORMERS OP NATURE 333 the winds represent some 5000 times that amount of coal. 9 Ocean currents are another large item. Some idea of the magnitude of the energy here involved may be gathered from an estimate given by L. J. Henderson according to which the gulf stream alone conveys 10 two-hundred million tons of water per second through the straits of Yukatan. If this body of water were cooled to arctic temperature we should have a transfer of energy at the rate of eight and a half billion horsepower. Most important of all, in the inorganic cycle, is the circulation of water by evaporation, precipitation, and river flow (including waterfalls) back to the ocean. Of the masses involved a picture had been presented in Chapter XVI. As to the energy involved, Henderson estimates the horsepower of evaporation from. 100 square kilometers of tropical ocean at over one-hundred million horsepower. C. P. Steinmetz11 has calculated that if eveiy raindrop falling in the United States could be collected, and all the power recovered which it could produce in its descent to the ocean, this would yield about three-hundred million horsepower. G, Ciamician12 quotes an estimate by Engler of the world's total water power as the equivalent of seventy billions of tons of coal. According to C. G. Gilbert and J. E. Pogue 13 the production of hydroelectricity in the United States in 1910 was the equivalent of forty-million tons of coal, whereas nearly ten times that amount went into the production of steam and carboelectric power. These authors further estimated that the water power developed at the date indicated represented about 10 per cent of that readily available, and 3 per cent of the total that might be open to development under elaborate arrangements for storage. 14 9 For a discussion of the Atmosphere considered as an engine see Sir Napier Shaw's Rede Lecture, published in Nature, 1921, p. 653. This author arrives at the estimate that "the best you can expect from the steam-laden air of the equatorial region working between the surface and the stratosphere, under favorable conditions, is a brake-horsepower efficiency of 25 per cent." 10 L. J. Henderson, The Fitness of the Environment, p. 182. 11 Survey Graphic, 1922, vol. 1, p. 1035 (cited by H. A. Spoehr, Jour. Ind. Eng. Chem., 1922, vol. 14, p. 1143). 12 Die Photochemie der Zukunft; Samml. Techn. Vortrage, 1914, p. 431. 13 Power, its significance and needs; Smithsonian Institution Bulletin 102, Part 5. 14 For a comprehensive survey of power development actual and potential see F. G. Baum, II. S. A. Power Industry. Also W. S. Murray, A Superpower System for the Region between Boston and Washington. United States Geological Survey Professional Paper 123 of 1921. 334 ELEMENTS OF PHYSICAL BIOLOGY Relation of Transformer Cycle to Circulation of the Elements. The circulation of substance in the organic world and its inorganic background, which was considered in an earlier chapter in its purely material relations, now acquires a new significance. We recognize in it now a typical characteristic of the great world engine which, for continued operation, must of necessity work thus in cycles. The picture presented to our minds is that of a gigantic overshot mill wheel, receiving from above the stream of sunlight with its two hundred twenty-seven million gross horsepower though much of this is spilt without effect and discharging below its dissipated energy in the form of heat at the general temperature level. The FIG. 68. THE MILL-WHEEL OF LIFE main outstanding features of the wheel are represented diagrammatically in figure 68. But in detail the engine is infinitely complex, and the main cycle contains within itself a maze of subsidiary cycles. And, since the parts of the engine are all interrelated, it may happen that the output of the great wheel is limited, or at least hampered, by the performance of one or more of the wheels within the wheel. For it must be remembered that the output of each transformer is determined both by its mass and by its rate of revolution. Hence if the working substance, or any ingredient of the working substance of any of the subsidiary transformers, reaches its limits, a limit may at the same time be set for the performance of the great transformer as a whole. Conversely, if any one of the subsidi- ENEBGY THANSFOBMEBS OF NATUBE 335 ary transformers develops new activity, either by acquiring new resources of working substance, or by accelerating its rate of revolution, the output of the entire system may be reflexly stimulated. As to the significance of this for the evolution of the system as a whole more will be said later, in the discussion of certain phases of the evolution of the human species in particular; for it is hardly necessary to remark that the case of man presents features of so remarkable character that it calls for special consideration, quite aside from the pardonable excess of interest which we personally feel in the creature. Evolution of the World Engine; The picture we must keep before us, then, is that of a great world engine or energy transformer composed of a multitude of subsidiary units, each separately, and all together as a whole, working in a cycle. It seems, in a way, a singularly futile engine, which, with a seriousness strangely out of keeping with the absurdity of the performance, carefully and thoroughly churns up ah 1 the energy gathered from the source. It spends all its work feeding itself and keeping itself in repair, so that no balance is left over for any imaginable residual purpose. Still, it accomplishes one very remarkable thing; it improves itself as it goes along, if we may employ this term to describe those progressive changes in its composition and construction which constitute the evolution of the system. For the statement will bear reiteration and emphasis this is the conception we must form of organic evolution: the evolution of the great world engine as a whole, not merely that of any single species of organisms considered separately. What is the trend of this development? Toward what end does the great transformer shape and reshape itself? A provisional answer to the question will be suggested in due course. For a time we must now abandon our broad viewpoint, and turn from the consideration of the great transformer as a whole, to a discussion of certain of its subsidiary engines which present points of special interest and importance. CHAPTER XXV RELATION OF THE TRANSFORMER TO AVAILABLE SOURCES As an enterprise, mathematics is characterized by its aim, and its aim is to think rigorously whatever is rigorously thinkable or whatever may become rigorously thinkable in course of the approved striving and refining evolution of ideas. C. J. Keyser. Distributed and Localized Sources of Energy. In Garnet's classical analysis of the operation of a heat engine the source of energy is taken for granted as one of the fundamental data of the problem. In nature sources of energy are not thus supplied unconditionally, and for our present purposes it becomes necessary to extend the analysis of transformer operation so as to take into its scope also some of the significant characteristics of the sources from which the engines of nature derive their supplies. And here a fundamental distinction is to be made between two lands of sources, namely, (1) evenly, or at least continuously distributed sources, and (2) localized sources, heterogeneously distributed. If the transformer draws its energy supply from a source uniformly distributed over a region R, at any point of which it can make contact with the source, then, evidently, within the region R the performance of the transformer is independent of its location. So, for example, plants derive their energy from sunlight falling upon them gratuitously, and draw their supplies of material partly from atmospheric carbon dioxide and oxygen diffusing to them by a spontaneous process, and partly from dissolved salts seeping to their roots automatically, that is to say, by a process essentially independent of any intervention on the part of the plant. And quite in accord with this general distribution of plant food, the typical plant is a sessile, passive organism. If, on the contrary, the transformer draws its supply from discontinuous, heterogeneously distributed sources, then continued operation demands at least some degree of relative motion between the transformer and the sources, so that the occasional collisions may occur between the transformer and a source. 336 RELATION OF TRANSFORMER TO AVAILABLE SOURCES 337 Random and Aimed Collisions. Purely random collisions, such as those contemplated in the kinetic theory of gases, may suffice to bring an adequate supply to the transformer.1 But evidently the output of the transformer will be enhanced if, instead of relying upon a precarious supply gleaned in fortuitous encounters, a suitable correlation is established between the motion of the transformer and the location of the sources. This may be accomplished in two ways, as follows: 1. There may be actual mechanical union2 positively connecting transformer and source, so that there is a functional relation (in the mathematical sense) between the motion of the transformer and the topography of the source. A simple instance in point is a trolley car. Here there is a definite relation between the topography of the system (track), the reaction of the transformer up it, and the distribution of the source. The car is not free to move except along the track and along the trolley wire. 2. Contact with the source may not be positively secured, but merely rendered more probably than in purely random collisions, by the occurrence of more or less accurately aimed collisions. Source and transformer are in this case mechanically independent, the motion of the source is not fully determined when the topography of the system is given; a certain freedom remains. There is, in this case, not functional relation, but only correlation between the motion of the transformer and the topography of the system: no specific motion is determined, only certain motions are rendered more probable than others. Negative Correlation. It is to be noted, of course, that such correlation between the motion of a transformer and the location of features 1 For an experimental investigation of the movements of lower organisms (Paramecium, Colpidium, Trachelomonas) see Przibram, Pftiigers Archlv, 1913, vol. 153, pp. 401-405. The movements were found to follow the law deduced by Einstein and Smoluchowski for Brownian movement (which, of course is random), namely that the mean square of the displacements of a particle in any direction in equal intervals of time t is proportional to t. The order of magnitude of the movements of the organisms, however, and the influence of temperature, were quite different in the case of Brownian movement. (For an account of the Einstein-Smoluchowski law see, for example, C. Schaefer, Einfiihrung in die theoretische Physik, 1921, vol. 2, p. 487.) 2 Compare L. T. y Quevedo, Essai sur 1'automatique, Revue Ge'ne'rale des Sciences, 1915, vol. 26, p. 601. 338 ELEMENTS OF PHYSICAL BIOLOGY of its environment is competent to bring other benefits aside from a a supply of energy and material (food). All transformers are more or less vulnerable. Exposed to an environment varying from point to point and from instant to instant, a transformer will in general sooner or later meet with an injurious stress, that is to say, a stress that will change its structure or constitution to a point where effective operation is impaired or altogether abolished. If it is desirable, in the interest of increased output, that collisions with suitable energy sources be rendered more probable than in purely random motion, it is evidently equally desirable, in the interest of continued operation of the transformer, that collision with harmful features in the environment be rendered less probable. In other words, in addition to apparatus establishing a positive correlation between the motion of the transformer and the location of sources, it is desirable that there be also provided apparatus establishing negative correlation between such motion and the location of injurious features of the environment. Collisions should, as far as possible, be aimed toward sources, and away from points of danger. The fate, the success of the transformer, will evidently depend both on the versatility of the aim, and on its accuracy; on the number and character of targets picked out for aim, and on the closeness with which the hits upon the target cluster around the bull's eye. The Correlating Apparatus. It is on the general plan indicated in the preceding paragraph that nature's mobile transformers, especially the typical animal organisms, operate. In the competition among these, for food and for safety, the accuracy and the versatility of aim characteristic of each species will evidently be most important determinants of relative success or failure, and hence of the trend of evolution. The dynamics of evolution thus appears essentially as the statistical dynamics of a system of energy transformers, each having a characteristic vulnerability, a characteristic versatility and accuracy of aim. It is here that the method of thermodynamics is inadequate. Its austere virtue of impartiality toward different mechanisms becomes a vice when information is sought regarding systems in which mechanism plays a leading r61e. The mechanism, or, to use a somewhat broader term free from mechanistic implications, the apparatus, by which the correlation is established between motion and environment, by which behavior is adapted to circumstances, is here not an incidental detail to be lightly dismissed as of secondary RELATION" OP TRANSFOEMEB TO AVAILABLE SOTJBCES 339 importance, but must occupy the very center of attention. To a somewhat detailed consideration of this apparatus we now proceed; in the interest of vivid, realistic presentation of the subject it will, however, be desirable to abandon from this point on the veiy general treatment and, to speak now specifically in terms of biological units, organisms, rather than in terms of the broader physical concept of energy transformers. It should be constantly borne in mind, however, that this change in attitude, or, it were better to say, in terminology, is chiefly a matter of convenience and effectiveness of presentation, and the fundamental physical principles involved, as set forth in the more general terms, should never be allowed to sink far below the surface of our immediate thought. The Component Elements of the correlating Apparatus. The continued existence of the organism, toward which his actions are aimed, demands that he shall direct his energies, his activities in accordance with the state of his environment, of the external world, avoiding unfavorable conditions, and seeking out those favorable or necessary to his maintenance. This includes the locating and seizing of food. But as a material, physical system, his actions are primarily determined by his own state. Hence, in order that his actions, determined immediately by the state of the organism himself, may be mediately determined by the state of the external world, apparatus must be provided whereby the state of the organism becomes in a certain suitable manner a function of the state of the external world. The external world is depicted in the organism by a certain apparatus, a set of organs and faculties, which we may appropriately term the Depictors. The depictors include first the Receptors or Organs of Special Sense (eyes, ears, nose, etc.) ; and second the Elaborators, whose function is to combine and further elaborate the crude information furnished by the senses. The physical location and structure and mode of operation of the elaborators is much less obvious than that of the receptors. In fact, we ordinarily recognize them rather as faculties (Memory, Reason) than as organs. Another set of organs and faculties, the Adjusters, determine the particular reactions, the behavior of the organism, in the light of the information brought in by the receptors and further elaborated by the elaborators. So the hungry bird, sighting a worm on the lawn, flies 340 ELEMENTS OF PHYSICAL BIOLOGY down to the spot from the tree on which it is perched, and secures its prey. The sight of the worm, together perhaps with the memory of earlier meals collected near the same spot, acts as a stimulus or Drive to responsive action. This last step, action, commonly involves the use of members, or motor organs, Effectors, such as wings, feet, hands, etc. In complicated cases, as in human behavior, the elaborators may also play an important role in the effector step of the process by which motion is correlated to environment, behavior adapted to circumstance. So, for example, the traveller, before setting out on a journey, plans his itinerary, perhaps months or years in advance. Receptor-Effector Circuit Begins and Ends in Environment. It is a noteworthy fact that this process of correlating action to conditions is essentially cyclic in character: It has its origin in the external world, which becomes depicted in the organism, provokes a response, the terminal step of which is usually, if not always, a reaction upon the external world. The net result is, in a sense, that the external world has reacted upon itself. The organism has acted as an intermediary. There is something more than a mere surface significance in this fact. For it is true generally that animals function essentially as catalysers, as agents assisting in a change that is "trying" to take place on its own account. So the green grass is, in a sense, hungry for oxygen, namely in the sense that its oxidation is accompanied by a diminution of free energy. The animal consuming the grass and deriving from its oxidation the requisite energy for further activity has not initiated any revolutionary process, but has merely helped nature in its course, has merely rolled the ball downhill, so to speak. This is all that the animal organism is competent to do, and man is not exempt from this restriction: In all our doings, whether we will it or not, we are assisting in a fundamental natural process, we are obeying an inevitable law of energetics. Correlating Apparatus Not Peculiar to Living Organisms . It must not be supposed that the typical elements of the correlating apparatus, the receptors, adjusters and effectors, are wholly peculiar to living organisms. They can be very clearly recognized also in certain mechanisms of human construction. In fact, owing to the circumstance that the operation of such man-made mechanism is fully known to us, that they harbor no mysterious "vital" principle or ill-understood element of consciousness, such purely mechanical EELATION OP TKANSFOEMEB TO AVAILABLE SOUECES 341 contrivances furnish particularly apt illustrations of the principles involved in the operation of the correlating apparatus. It is therefore well worth while to consider here a simple example of this kind. Some time ago there appeared on the market an ingenious toy, primarily designed, no doubt, merely to amuse; but, in point of fact, highly instructive. Its general appearance and simple mechanism are illustrated in figure 69. The beetle "walks" on two toothed wheels, of which one is an idler, while the other is rotated by a spring whose gradual release is ensured by a simple escapement device. At its forward end reckoning in the direction of motion (at the "head") the toy is provided with a pair of antennae, of which one is a dummy, and rises clear of the table upon which the beetle is placed to exhibit its talents. The other antenna is operative and is so bent downward as to glide along the table top, in contact with it. A little FIG. 69. MECHANICAL WALKING BEETLE, EXHIBITING THE SEVERAL CHARACTEEISTIC ELEMENTS OP THE COERELATING APPARATUS in advance of the propelling wheel is another smaller toothed wheel, running idle, and disposed transversely to the direction of the driving wheel. This transverse wheel clears the table without contact in the normal working position of the beetle. The animal, if placed somewhere near the center of the table, makes a straight track, apparently intent upon reaching the edge and seeking destruction in a species of mechanical suicide. But the moment the operative antenna clears the edge of the table, the body of the toy, till then held up by the contact of the antenna with the table surface, sinks down a fraction of an inch, and the transverse wheel now contacts with the table. In consequence the toy rotates until the running wheel is parallel with the table edge, and the insect continues its peregrinations with the operative antenna hugging the side of the table top. Clearly here the antenna is a receptor, which "apprises" the insect of certain features in its environment, which depicts, in a crude but 342 ELEMENTS OF PHYSICAL BIOLOGY sufficient manner the environment in the toy. The law of depiction is here extremely simple; a depression in the external world (table top) is translated into a downward tilt in the angle of repose of the toy. The adjuster, in this case, is the transverse wheel, about as simple an example of an adjuster as can well be imagined. It "construes" the information furnished by the receptor antenna, and modifies in accordance with this information the law of motion of the toy, in such manner as to preserve the beetle from a fall which might destroy that stability of form on which the continued operation, according to schedule, of the mechanism depends. It would be easy to cite a number of other examples of devices constructed either as toys, scientific curiosities, or for actual technical use, which exhibit more or less prominently the typical correlating apparatus, with receptor, adjuster and effector. By far the most highly perfected of such automatic devices is the modern machineswitching apparatus for telephones, which eliminates the "operator" at the central offices. This device, which fulfills an amazing multiplicity of functions, will be found briefly described in non-technical language in the April number 1923 of The Bell System Technical Journal. Perhaps more directly in line with our present interest here is a mechanical chess player that was designed some years ago by L. Torres y Quevedo; 3 this device successfully counters any move (with a limited number of pieces, merely as a matter of simplicity) that a living opponent may choose to make upon the board. The game of chess itself is so well conceived a conventionalization of the battle of life 4 that it is well worth the while to make a seeming digression to analyze the fundamental elements of this remarkable game. The bearing of this analysis upon certain problems of biological evolution will then become apparent. 8 A description will be found in the Scientific American Supplement, November 6, 1915, p. 296. 4 The aptness of this illustration has no doubt been remarked by many. I have recently noted the following pertinent references : F. L. Wells, Mental Adjustments, 1917, p. 6. Eddington, Time Space and Gravitation, 1920, p. 184; T. H. Huxley, A Liberal Education and Where to Find it. Collected Essays, 1894, vol. 3, p. 81. A bibliography of the mathematical treatment of chess will be found in W. W. R. Ball, Mathematical Recreations, 1911, Chapter VI, p. 109. RELATION OF TRANSFORMER TO AVAILABLE SOURCES 343 Chess as a Conventional Model of the Battlefield of Life. A game of chess is a succession of physical events. How is its course determined? The elements that determine this course are as follows : 1. A topographic map, a chart of geometric constraints, the chess board. 2. Movable upon this chart, a number of movable points (chessmen), each the center of & field of influence, defined for each movable point in relation to the geometric constraints. So, for example, the field of influence of a pawn extends to the two squares diagonally in front of the pawn. 3. A law restricting the time-rate of advance of each moving point (moves alternate from white to black). 4. A law defining the influence upon each other of two points in collision, i.e., two points whose fields of influence have interpenetrated to a prescribed extent. An example of this is the rule that a chessman arriving upon a square occupied by a hostile piece, throws the latter off the board. 5. A law restricting the movements of the points when not in collision, i.e., when outside one another's field of influence. So, for example, a bishop may move only diagonally. 6. The elements enumerated so far place restrictions upon permissible changes (moves). These elements alone cannot, evidently, determine any occurrence of any kind: Absolute immobility, for example, or any random move that did not violate the rules of the game, would equally satisfy the conditions enumerated. 7. In addition to the elements, 1, 2, 3, 4, 5, there must therefore be in operation some positive principle (tropism) which not merely restricts possible occurrences, but which determines actual events. In chess this principle is furnished by the effort of each player to bring about checkmate. Each move is so aimed (with greater or less accuracy and breadth of view, versatility, according to the skill of the player) as ultimately to force a checkmate. From the battlefield of chess we now turn our eyes on the scene of the great biological contest: Before us is a topographic map, over which move those organisms that are by nature gifted with motion. We may think of each such organism as a moving point, the center of a field of influence. As the chessplayer must accustom his mind's eye to see, radiating out from each chessman, its field of influence- 344 ELEMENTS OF PHYSICAL BIOLOGY upon the board, so we, in envisaging the battleground of organic evolution, must see each organism carrying around with it, as if rigidly attached to its body, a field, or a target, of zones, of the following character. A. Zones of Influence, In general the motion of the individual will be determined by laws too complicated to be readily analyzed, and therefore will be described as random. But there will upon occasion be a rather abrupt break away from such random movement, according as a certain feature of the environment lies without or within certain zones. For example, the movements of a fly wandering about on a window pane are, presumably, in all cases physically determinate. But in a homogeneous field (uniform illumination etc.), the motion will assume, on the whole, a random character. We may suppose that, in first approximation at any rate, the migrations of the individual will follow some such law as those developed, for example by Sir Ronald Ross, 5 by Pearson and Blakeman, 6 or by Brownlee7 for random migration. But, bring some particle of food within the field of sensuous observation of the fly, and the law of motion instantly changes from random to more or less clearly directed. We may, then, construct about each individual a sort of target of zones of influence. The ideal would be to draw this target on a quantitative plan, according as a stimulus of strength s exerts a directing influence d at a distance r. In practice there may be difficulty in constructing these zones, but we may at least conceive them as drawn. We may say that a given organism is "in encounter" with a given point (e.g., a feature of the topographic chart) when that point falls within its field of influence. Similarly we may say that two organisms are in encounter when the one falls in the field of influence of the other. This encounter is mutual or one-sided according as each is within the other's field} or as only one is in the other's field, but not conversely, for example if A sees B, but B does not see A; or, to take an example 5 Sir Ronald Ross, Prevention of Malaria, 1922, second edition, pp. 179, 700. 6 K. Pearson and J. Blakeman, Drapers' Company Research Memoirs, III: XV, 1906. 7 J. Brownlee, Proc. Roy. Soc. Edin., 1910-1911, vol. 31, pp. 262-289; of other references related to this subject the following have been noted: F. Y. Edgeworth, Entomological Statistics, Metron, 1920, vol. 1, p. 75; W. H. Cole, Science, 1922, vol. 55, p. 678; W. B. Hardy, Nature, December 30, 1922, p. 866 (Twelfth Report of the Development Commissions 1922). 345 RELATION OP TRANSFORMER TO AVAILABLE SOUBCES from chess, a bishop may threaten a pawn, though the pawn does not threaten the bishop. Zones of influence may extend over millions of miles, as in the case of a traveller steering his course by the stars. B. Zones of Mobility. We may stake out around each organism a target of zones indicating the distance which it is physically capable of travelling in 1, 2, , . .n units of time. These zones also we shall think of as attached to the organism and carried round with it in its wanderings through the landscape. It is clear that the fate of the organism, and the history, the evolution of the system as a whole, will depend, first, on the character of the zones of influence and the zones of mobility; and second, on the nature of the correlation, the law of the aimed movements,, established through these zones. We may seek to establish analytical expressions for this dependence. Let g be a parameter defining the character or "pattern" of a target of zones of influence or of mobility of the organisms of species S. Thus, for example, q might be parameter, or one of a set of parameters, defining visual acuity, measured on some suitable scale, at a distance of 5, 10, 15, . . . feet, under standard conditions. Or, g might be a parameter defining the minimum time required for the organism to reach a point 5, 10, 15, ... feet from his actual position, under standard conditions. 8 Analytical Statement of Problem. We may now enquire: 1. What will be the effect upon the rate of growth of the species if the parameter g is increased by a (small) amount dqf If r is the fractional rate of increase of the species S, can we establish an expres- d?* sion for the partial derivative ;? A glance at the chess analogy will help to make clear the nature of the question thus raised. In chess we might ask: What would be the effect upon the course of the game if, other things equal, we were to modify in some stated particular the rules limiting the permitted moves of a given piece, for instance by allowing a pawn to move two squares, instead of the conventional one? 2, A second enquiry of peculiar interest relates, not to the character (pattern) of the zones of influence and mobility, but to the form of 8 Isochrone charts of essentially this character, relating to travelling facilities, were, according to Darmstaedter, first suggested by K. Bichter in 1833 arid actually prepared by Sir Francis Galton in 1881 (L. Darmstaedter, Handbuch zur Geschichte der Naturwissenschaften und der Technik, 1908, p, 792). 346 ELEMENTS OF PHYSICAL BIOLOGY relation established, through these zones, between the action of the organism and his environment. For it is hardly necessary for us to be reminded that two individuals or species with the same visual acuity, for example, may react in very different manner on seeing the same thing. Here again the chess analogy is helpful. The corresponding enquiry with regard to chess is: What would be the effect upon the course of the game, if, with unchanged rules as to the moves of the pieces, a given change were made in the method, or the ability, of one of the players? To deal with these problems it is desirable to introduce two concepts, that of the Behavior Schedule, and that of Specific Productivity in a given activity. THE BEHAVIOR SCHEDULE It has been remarked9 that "a living organism is both cause and effect of itself." We may say in somewhat more detailed statement, that the organism goes through a certain routine of motions or activities which are rendered possible by ^& structure, and which, in turn, are a necessary condition for the continued existence of that structure. These activities in general involve the expenditure of certain quantities of free energy, and a part of the energy so expended necessarily is spent in collecting (earning} a "replacement" amount equal to the total expenditure, to balance the account, to cover the cost of living. While this phenomenon is, in a general way, characteristic of all mobile forms of life, the particular method followed in this cyclic activity of gathering and spending free energy varies in the most multiform manner from one species or type of organism to another. Each type of organism may thus be said to possess a characteristic Behavior Schedule, which may be defined in terms of certain coefficients as follows: Of its total expenditure E per unit of time, a representative individual of the population will spend, on an average a fraction Xj in a particular activity Aj, which may be defined as the maintaining of a parameter Uj at the value u$. So, for example, 10 a human being may expend on an average, per day, 9 Kant, Kritik of Judgment. Transl. Bernard, London, 1892, p. 274. 10 The figures in this example are chosen arbitrarily, although an effort has been made to make them reasonably realistic. In view of the wide variations in standards and cost of living in different countries, different social RELATION OF TRANSFORMER TO AVAILABLE SOURCES 347 number of calories ISO external work (services sold) in maintaining his daily food supply at 3,000 cal. 2,500 internal work (physiological work) in maintaining his body temperature at 9SF. 130 external work (services sold) in maintaining Ms house rent at, daily 2.00 60 external work (services sold) in maintaining his dairy supply of clothing at SO , 75 30 external work (services sold) in maintaining his daily supply of sundries at SO. 25 100 external work (services sold) in maintaining the rate of increase of the population at 1 per cent per annum 3,000 calories total expenditure and total earnings (Note: 1 calorie = 30S6 foot pounds.) SPECIFIC PRODUCTIVITY Consider some particular activity A j which results in maintaining a parameter Uj (e.g., food capture per head per unit of time) at the value Uj, then we will define P-, 3 the Specific Productivity of energy Ej spent in activity Aj by Pj = '' (cj a constant) (1) and we note that strata, and at different epochs, close figuring, in such an example as this, would be out of place. Numerical data pertinent to this example will be found scattered widely in various sources, of which the following may here be mentioned: J. Amar, Le Moteur Humain, 1914, p. 254; R. Hutchison, Food and Dietetics, 1902, p. 37:46; J. LeFevre, La Chaleur Animale, 1911; F. H. Streightoff, The Standard of Living, 1911. 348 ELEMENTS OF PHYSICAL BIOLOGY EFFECT OP CHANGE IN ZONE PATTERN (Intra-Species Evolution) We are now prepared to consider the analytical representation of the influence of changes in the pattern of the zones of influence and the zones of mobility, on the one hand, and, on the other, of a change in the behavior schedule, on the proportional rate of increase r of the species of organisms under discussion. This proportional rate of increase, r = -777 , is in general a func- .Arft tion of the parameters U (food capture, shelter, etc.), so that we may write r = r(ui, u2 , . . . Uj, . . . ) (3 ) and -^L^-^L^i (4) Now the specific productivity P-t in activity A$ itself depends upon the character of the zone pattern. For, the more perfectly the individual is apprised of the relevant features of its environment (i.e., the more perfectly developed its zones of influence), the better, other things, equal, will it be able to direct its activities to the ends defined by the parameters U; and a similar remark evidently applies to the zones of mobility. If, then, q is a parameter denning the character of these zones, we may write Pi = Pj(g) (6) and | r JL |p (7) -1^*1 (8) Ouj Oq or, more generally, since a change in q may affect not only a single productivity Pj} but also others, PI, P2, . . . Pn RELATION OF TRANSFORMER TO AVAILABLE SOURCES 349 the summation being extended over all the activities AI, Az , . . A-} , . . , Aa in so far as they are affected by the parameter q. (It is immaterial whether those not so affected are included in the summation or not, since they will contribute a zero term.) It lends a certain interest to the relation (9) if we observe that such dr dr partial derivatives as ;r , ^ possess a concrete signification, as follows : Consider two small increments Agi and Aqz in two parameters QI and go. (To make matters concrete, suppose qi measures visual acuity, qz auditory acuity.) If Aqi and Ag-2 are such that dr . dr , _A3l -g--Ag 2 = (10) i.e., such that Agi _ dr / dr A^ = d^/d^ (11) then it will be indifferent for the rate of the increase of the species whether visual acuity is increased by Agi or auditory acuity by Ag2 . We might say, in this sense, that the increments Agi and Ag2 are, in this event, equivalent, or that that they have the same total value (in exchange against each other) for the species. Moreover, from (10) it is evident, on this same understanding, that the partial deriva- dr tive ^ measures the value (in exchange) per unit, 11 to the species, of dr the parameters gi, and similarly measures the value (in exchange) per unit of the parameters gz . We may symbolize these facts by writing dr dS-** <12) dr d^. = ^ <* The relation (9) then appears in the form y-i u An arbitrary proportionality factor enters, which is conveniently made unity by suitable choice of units. 350 ELEMENTS OF PHYSICAL BIOLOGY Certain steps in the development set forth above are reminiscent of the hedonistic calculus of Jevons and his school of economists. One is thus naturally led to look for a relation between value (in exchange) as here defined, and economic value in exchange, as conceived by those authors. It should be expressly noted, however, that the reasoning here followed, and the conclusions reached, are quite independent of any economic theory. As for the relation of the present reflections to economic theory, this will become apparent in the paragraphs that follow. EFFECT OF CHANGE IF BEHAVIOR SCHEDULE We may note, first of all, that drj _ dr C)j _ 5?- , dlpd^jdipd^ j where p-} = ^77defines what we may term the marginal productivity OIL j of energy expended upon the parameter Uj. This marginal productivity p; will, in general, differ from the total productivity Pj defined by equation (1). It is, however, desirable, to express the relation between r and the behavior schedule in another way, with the following considerations in mind. Rigid or Automaton Type and Elastic Type of Behavior Schedule. The apparatus by which the coefficients X defining the behavior pattern are determined varies widely in different species of organisms. At one extreme we may suppose that we have an organism, with a rigid, inelastic behavior schedule, the coefficients X being determined explicitly, once for all, by the properties of the individual. The extreme case of this kind is to be found, presumably, in plants, where, for example, the amount of energy expended in anabolism to replace wear and tear (e.g., annual leaf-fall) may be taken as a comparatively simple function of the leaf area. Many of the lowest forms of animals, actuated by simple tropisms, no doubt also approximate closely to such a rigid behavior schedule, what might be termed the automaton type of behavior schedule. But in the higher animals, and most particularly in man, we have an elastic behavior-schedule. Here the A's are not fixed in simple explicit manner by the physical character of the organism. We BELATIOX OF TBANSFOKMER TO AVAILABLE SOURCES 351 encounter here the phenomenon which we experience in ourselves subjectively as free choice between alternative courses of action, alternative values of the X's open to us to choose from. This cannot mean, of course, that the X's are wholly arbitrary, or physically indeterminate. Some action is and must be taken. But the natural principle which operates in the determination of the X's, of the behavior schedule, is not immediately obvious. The avenue of approach which seems to give most promise of lending us an insight into the relations here involved, is the following: The elastic type of behavior schedule, the free-choice schedule, as distinguished from the automaton type, is essentially a characteristic of the more highly organized among the mobile (animal) organisms. This fact is so prominently displayed to us in our own selves, that the adaptive superiority of the elastic type over the automaton type is commonly (and perhaps in a measure unjustly) taken for granted. If this assumption of such superiority be true, then the principle which operates in determining the coefficients X's must be that they tend, on the whole, to be adjusted, in the operation of free choice, toward values favorable to the growth of the species. In the ideal case of perfect adaptation the X's would, according to this view, be such as make r, the proportional rate of increase of the species, a maximum. Let us see what this would imply. In reacting upon its environment to influence the parameter Uj, the organism itself necessarily undergoes some modification, since it gives up energy Ej, (subjectively this modification is commonly felt as fatigue). In other words, if the state of the individual is defined by the values of certain (internal) parameters /i, /a . > then the expenditure of an element of energy 8 E-} by the individual, if not accompanied by other effects, is accompanied by a change 5/i,5/2 . . . in the parameters /. At the same time the (external) parameter Uj is modified by ou-} . The effect of these modifications upon r is given by where, for brevity, the contracted notation has been employed * *' drd/k 352 ELEMENTS OF PHYSICAL BIOLOGY If r is to be a maximum, (5r) must vanish for any arbitrary small value of 5 Ej, so that we must have for every subscript j, according to (16) dr dj dr d/ . (18j or, adopting the notation of (12), (13), (15) t'uiPj + t'fpt = (19) Relation between Ideal and Actual Organism. We have thus far considered an ideal type of organism of the free choice type of behavior schedule, constructed on the principle that the X's shall be so chosen as to make the proportional rate of increase r a maximum. It remains to consider the relation between this ideal type of organism and the actual organism. The actual organism is not consciously guided by any consideration of the effect of his actions upon the rate of increase of his species. At least the instances in which such considerations are operative are so exceptional that we may well leave them out of account. What guides a human being, for example, in the selection of his activities, are his tastes, his desires, his pleasures and pains, actual or prospective. This is true, at least, of some of his actions, those which are embraced in his free-choice type of behavior schedule. That the human behavior schedule12 also contains an element of the non-elastic (automaton) type may be admitted in deference to those who have leveled their destructive criticism at the hedonistic account of human behavior. We may, however, restrict our discussion here to that portion or phase of conduct which is determined by hedonistic influences. In this case, then, we are dealing with an organism which seeks to make, not r, but 0, its total pleasure ("ophelimity" in Pareto's terminology) a maximum. Argument precisely similar to that developed above here leads to the condition. dQ 5uj dO r d/ + = C20) 12 In a modern civilized community we cannot very well speak of one typical behavior schedule of the individual, owing to the division of labor, with specialization of individuals in different pursuits. This matter will be found discussed more particularly, in Chapter XXVIII dealing with the adjusters HELATION OP TRANSFORMER TO AVAILABLE SOURCES 353 ft is immediately seen that (18) and (20) will lead to the same adjustment of the activities of the individual if, and only if the 50 marginal ophelmiities r are proportional to the corresponding A *' ' derivatives ;r~ i.e. OUj -__ _ c OUj UMj We see then, that an organism actuated by pleasure and pain will so distribute its activities as to make r a maximum, if, and only if, its marginal ophelimities are proportional to the corresponding deriva- br tives r~ . OUj Effect of Small Departure from Perfect Adjustment. If we look upon the sense of pleasure and pain as an adjunct serving the express purpose of directing the activities of the organism towards ends beneficial to the growth of the species, then a species for which condition (21) were satisfied would represent perfect adaptation in this respect. This leads us to a somewhat different setting of our problem regarding the influence of a change in the behavior pattern upon the rate of or increase of the species. Instead of enquiring after :^7 , we may seek OHij information regarding the influence, upon r, of a change in the tastes 50 or desires of the species as defined by the derivatives r . AnJ OUj answer can be given at any rate in the neighborhood of the "perfect" adjustment of tastes defined by (21), i.e., for a species whose behavior schedule does not depart materially from that defined by (18). Consider a species for which the ideal (perfect) adjustment is given by ujpj + fpf = (22) Suppose that this species actually adjusts its activities according to the plan (23) departing slightly (by an "error of valuation" 5e) from the perfect adjustment, namely (uj + 8e)pj + vfpt = (23) 354 ELEMENTS OF PHYSICAL BIOLOGY Then it can readily be shown13 that <. / ?> 7^= ~ V;Pi ?T- (SujPj + WfPf) (24) O6j y ouj j which is the required analytical expression for the influence of a small "error of valuation" upon the rate of increase of the species. The utility which such formulae as here developed may possess must be sought, not so much in their application to numerical examples data for this are now and may long remain unavailable as in the light they throw, quantitatively, upon the biological foundations of economics, in the relations which they reveal between certain biological and certain economic quantities. It must be remembered that the mathematical method is concerned, not only, and indeed not primarily, with the calculation of numbers, but also, and more particularly, with establishment of relations between magnitudes. 14 Relation of Economic Value to Physical Energy. The behavior schedule has been quantitatively defined in terms of energy. This, if not the only possible definition, is at any rate a convenient one, and has also the advantage of emphasizing the important relation of the organism to the energy sources of his environment. His correlating apparatus is primarily an energy capturing device its other functions are undoubtedly secondary. Evidence of this is manifold. The close association of the principal sense organs, eyes, ears, nose, taste buds, tactile papillae of the finger tips, with the anterior (head) end of the body, the mouth end, all point the same lesson, 15 which is further confirmed by the absence of any well developed sense organs in plants. 16 Exceptions here do indeed prove the rule, for sensitive plants, with a well-defined correlating apparatus, are just those which have departed so far from norm as to consume flesh food. And contrariwise, we ourselves are "blind" toward the one food that is omnipresent and which we consume by " A. J. Lotka, Jour. Washington Acad. ScL, 1915, vol. 5, p. 397. 14 Compare A. Cournot, Researches into the Mathematical Theory of Wealth, English translation by Irving Fisher, 1897, p. 3. 16 Herbert Spencer, Principles of Biology, vol. 2, p. 166; E. H. Starling, Science, 1909, p. 394; A. J. Lotka, Annalen der Naturphilosophie, 1910, p. 67. 16 For a resume of "plant psychology," see C. H. Farr, Atlantic Monthly, December, 1922; also Sir Frederick Keehle, The Plant Commonwealth and Its Mode of Government, Nature, 1924, vol. 144, pp. 13, 55. RELATION OF TRANSFORMER TO AVAILABLE SOURCES 355 an almost unconscious, vegetative process, namely oxygen. If we seek an insight into the "psychology of plants/' it may be well to begin by imagining what our mental state would be if, in all our food quest, we remained as passive and indifferent as in the function of breathing. The life contest, then is primarily a competition for available energy, as has been pointed out by Boltzmann.17 Energy in this sense and for this reason has value for the organism which is a very different thing from saying (as some have said or implied) that economic value is a form of energy. It is true that different kinds of energy are in a certain sense interconvertible into each other at fairly definite rates by exchange upon the market, in a human population. But the conversion factors here involved are of a totally different character from those that enter into the analytical expression of the law of conservation of energy. This must be immediately apparent from the fact alone that the 'mechanical equivalents" of the several forms of energy are absolute constants, whereas the economic conversion factors are somewhat variable, though they have often a species of approximate constancy, a fact which calls for explanation. Economic Conversion Factors of Energy, A simple example may help to clarify the view; the case of the automatic vending machine, the penny-in-the-slot chocolate dispenser, for instance. The salient facts here are : 1. A definite amount of money brings in exchange a definite amount of commodity (and of energy). 2. The physical process is a typical case of "trigger action," in which the ratio of energy set free to energy applied is subject to no restricting general law whatever (e.g., a touch of the finger upon a switch may set off tons of dynamite). 3. In contrast with the case of thermodynamic conversion factors, the proportionality factor is here determined by the particular mechanism employed. Reflection shows that all transformation of money or of economic assets of any kind into energy by exchange upon the market is of 17 Der zweite Hauptsatz der mechanischen Warmetheorie, 1886 (Gerold, Vienna), p. 210; Populate Schriften, No. 3, Leipsic, 1905; Nernst, Theoretische Chemie, 1913, p. 819; Burns and Paton, Biophysics, 1921, p. 8; H. F. Osborn, The Origin and Evolution of Life, 1918, p. XV. 356 ELEMENTS OP PHYSICAL BIOLOGY this character. It is always a case of trigger action. Somewhere there is a store of available energy, which can be tapped with an expenditure of greater or less effort. The payment of the price sets in motion the requisite machinery for the release of that energy (or for its transfer of ownership, the release being delayed at the discretion of the buyer). In view of the entire absence of any general law regulating the ratio of energy released to energy applied in such cases of trigger action, we may ask the question, how does it come about that economic conversion factors, economic ratios-in-exchange of different forms of energy, display any regularity whatever? The answer is not far to seek. The approximate constancy of the economic conversion factors is traceable to the approximate constancy in type of the mechanism involved, namely the human organism and its social aggregations. Just as one particular slot machine will always deliver a certain package of chocolate, so a certain social organization under similar conditions will render (approximately) the same amount of selected form of energy in return for a stated sum of money. As to the circumstances that quantitatively determine these economic conversion factors, for a discussion of these the reader must be referred to the literature; 18 only this may be remarked here, that the conception advanced by Ostwald, 19 for example, that the determining feature is the (physical) availability of the particular form of energy, is inadequate. Collective Effect of Individual Struggle for Energy Capture. Our reflections so far have been directed to the selfish efforts of each organism and species to divert to itself as much as possible of the stream of available energy. But if we recall once more the admonition of Bunge Nature must be considered as a whole if she is to be understood in detail we shall be led to enquire: What must be the 18 A. J. Lotka, Proc. Natl. Acad. Sei., 1921, vol. 7, p. 192. 19 W. Ostwald, Die Energie, 1908, p. 164. Of other literature more or less pertinent to the subject the following may be mentioned: G. Helm, Die Lehre von der Energie, Leipsic, 1887, pp. 72 et seq. W. Ostwald, Energetische Grundlagen der Kulturwissenschaften, Leipsic, 1909, p. 155. Die Philosophic der Werte, Leipsic, 1913, pp. 260; 314-317, 326, 328; Budde., Energie und Recht, Leipsic, 1902, p. 56; Winiarski, Essai sur la M