Přehled značek Detailní fluviálně-geomorfologické mapování: návrh univerzálního značkového klíče Jan Miklín & Tomáš Galia | jan.miklin@osu.cz, tomas.galia@osu.cz | Katedra fyzické geografie a geoekologie, Přírodovědecká fakulta, Ostravská univerzita | © Journal of Maps 2017 1.Koryto 2.Zdrojnice (koryto-svah) 3.Niva (údolnídno) 4.Antropogennízásahy 5. Křížení 1.1 Ohraničení 1.2 Převažující proces 1.3 Dnový substrát 1.4 Proudění 1.5 Morfologie 1.6 Korytové formace 1.7 Říční dřevo 2.1 Přírodní 2.2 Antropogenní 3.1 Vegetatace 3.2 Formace 4.2 Opevnění dna 4.3 Spádové objekty 4.5 Opevnění břehů 6.1 Měřické body 1.1.1 bankfull 1.1.2 nízký průtok 1.1.3 údolní dno/niva 1.2.1 erozní 1.2.2 akumulační 1.2.3 transportně-vyrovnaný 1.3.1 jíl/prach 1.3.2 písek 1.3.3 štěrk 1.3.4 valouny 1.3.5 balvany 1.3.6 skalní dno 1.4.1 směr proudění 1.4.2 zóna rychlejšího proudění 1.4.3 zóna pomalejšího proudění 1.4.4 proudnice 1.5.1 stupňovitá 1.5.2 planární 1.5.3 tůň-peřej 1.5.4 duna-čeřina 1.5.5 skalní koryto 1.5.6 větvící se koryto 1.6.1 stupeň 1.6.2 tůň 1.6.3 peřej 1.6.4 lavice 1.6.5 ostrov 1.6.6 skalní stupeň 1.6.7 skalní skluz 1.6.8 balvan 1.7.1 LWD 1.7.2 nápěch 1.7.3 akumulace SW 1.7.4 bobří hráz 2.1.1 strž 2.1.2 náplavový kužel 2.1.3.1 sesuv aktivní 2.1.3.2 sesuv stabilizovaný 2.1.4.1 nátrž aktivní 2.1.4.2 nátrž stabilizovaná 2.1.5 kamenný proud 2.2.1 halda 2.2.2 násep 3.1.1 travino-bylinná vegetace 3.1.2 keřová vegetace 3.1.3.1 listnaté stromy (les) 3.1.3.2 jehličnaté stromy (les) 3.1.3.3 smíšený les přírodní vegetace antropogenně ovlivněná vegetace 3.2.1 avulzní koryto 3.2.2 slepé rameno 3.2.3 mrtvé rameno 3.2.4 mokřina 3.2.5 agradační val 3.2.6 výplavový kužel 3.2.7 nivní (terasový) stupeň 3.2.8 murová akumulace 4.1 protipovodňový val 4.2.1 beton 4.2.2 kamenná dlažba 4.3.1 spádový stupeň 4.3.2 přehrážka 4.3.3 balvanitý skluz 4.3.4 jez 4.3.5 vývařiště 4.4 usměrňovací výhon 4.5.1 vrbové řízky 4.5.2 kulatina 4.5.3 haťový válec 4.5.4 polovegetační tvárnice 4.5.5 kamenný zához/pohoz 4.5.6 kamenná rovnanina 4.5.7 gabiony 4.5.8 souvislé zpevnění betonem 4.5.9 svislé opěrné zdi 5.1 brod 5.2 propustek 5.3 most 5.4 přemostění inženýrských sítí 6.1.1 geodetický bod (oficiální) 6.1.2 geodetický bod (vlastní) 6.1.3 stabilizovaný bod 6.2 bod odběru vzorků 6.3 příčný profil geometrie atributy topologie definice, poznámkyznačka A L L A A A A A A B B B L L L L L L L B, L A A A A B, L A B B B B B, L B, L, A1) A B, L B, L B, L B, L B, L, A1) A B, L, A1) B, A B, A B, A B, A B, A L, A L, A L, A A B, L, A1) A L A L, A A A B, L B, L B, L B, L A L, A B, L B, L B, L B, L B, L B, L B, L B, L B, L B B B B B B B B B, L převažující proces určuje barvu hranice 1.3 uvnitř 1.1.1 barva 1.3 leží kolmo na 1.4.4 znázorněna 1.5 umístěna jako 1.4.4 zrnitost stejně jako 1.3 velikost, orientace na konci 2.1.1 definován ohraničením břehy, přítomností suchozemské vegetace nebo změnou sedimentární facie (viz přehled metod vymezení dle Navratil et al. 2006). obvykle protékané koryto (za běžného vodního stavu) hranice nivy nebo úpatí svahů viditelné znaky hloubkové eroze, jako jsou odhalené kořeny, časté nátrže nebo erodované skalní výchozy tok s akumulačními tendencemi charakterizovanými např. vývojem velkých štěrkových lavic, zjemňováním sedimentů a rozšiřováním koryta bez jasných erozních/akumulačních znaků dominantní sedimentární facie podle zjednodušené Wentworthovi (1922) škály: > 0,063 mm (kohezivní materiál) 0,063-2 mm (převažující písková frakce) 2-64 mm (převažující štěrková frakce) 64-256 mm (převažující valounová frakce) > 256 mm (převažující balvanitá frakce) vystupující skalní podloží směr proudnice dle sklonu koryta zóna rychlejšího proudění za běžných podmínek (obvykle přes peřeje, kaskády apod.) zóna pomalejšího proudění za běžných podmínek (obvykle v tůních) linie v nejhlubší části koryta nebo v místě nejrychlejšího proudění více či méně organizovaný stupňovitý profil dna se stupni, tůněmi a kaskádami (Montgomery & Buffington 1997, Comiti & Mao 2012). relativně uniformní koryto bez vertikální oscilace dna (Montgomery & Buffington, 1997) střídání tůní a peřejí v podélném profilu toku (Montgomery & Buffington 1997). písčitá koryta s vyvinutým systémem duna-čeřina (Montgomery & Buffington 1997). koryto s vystupujícím skalním podložím (důsledek stečení blokovobahenního proudu nebo transportní kapacity vysoce převyšující donášku sedimentů) (Montgomery & Buffington 1997). větvící se koryto zahrnující anastomózní i divočící toky (téměř) kolmý spád vody přes balvany nebo dřevní hmotu zóna relativně nižší rychlosti a větší hloubky proudění zóna relativně vyšší rychlosti a nižší hloubky proudění, obvykle také s hrubšími sedimenty akumulační forma nad běžnou úrovní hladiny akumulační forma nad běžnou úrovní hladiny porostlá vegetací (téměř) kolmý spád vody přes skalní stupeň vystupující skalní podloží, po kterém teče voda v rovnoběžném směru jednotlivě zmapovaný balvan (průměr > 256 mm) v místech s jinak jemnější sedimentární facií dřevo delší než 1 m s minimální tloušťkou 10 cm (Wohl et al. 2010). akumulace více než tří LWD (Wohl & Cadol 2011). akumulace menšícho dřeva než LWD nebo méně než tří LWD v kombinaci s jemnějším dřevem bobří hráz zcela nebo částečně přehrazující vodní tok konkávní podélná forma, občasně protékaná, včetně koluviálních koryt sensu Montgomery & Buffington (1997). akumulační forma mimo koryto vyvinutá jako důsledek fluviálního transportu nebo murové aktivity (obvykle v dolním závěru údolí, v místě s lokálně sníženým sklonem údolnice) sesuv aktivně dodávající sedimenty do toku stabilizovaný sesuv v interakci s korytem (např. hradící údolí, ovlivňující směr proudění) relativně čerstvá nátrž, aktivně dodávající sedimenty do toku vegetací stabilizovaná nátrž, reaktivace možná při vyšších průtocích boční vstup hrubšího sedimentárního materiálu (kamenné proudy, proudy z hald, blokovobahenní proudy) antropogenní akumulace vznikající při těžební činnosti vyvýšená antropogenní forma (obvykle pro silnice, železnice apod.) travinobylinná vegetace v nivě nebo údolním dnu křovinná vegetace v nivě nebo údolním dnu listnatý les v nivě nebo údolním dnu jehličnatý les v nivě nebo údolním dnu smíšený les v nivě nebo údolním dnu (polo)přirozená skladba vegetace člověkem značně ovlivněná skladba vegetace s nepřirozenými druhy boční koryto protékané jen za vysokých průtoků (povodňové koryto) bývalý meandr, hydraulicky propojený s korytem bývalý meandr, hydraulicky nepropojený s korytem plošná sníženina v nivě s jemnozrnným sedimentem, obvykle za agradačním valem vyvýšenina mimo hlavní koryto, s korytem rovnoběžná, obvykle vznikající během ústupu povodně akumulační forma kuželovitého tvaru, vznikající v místech, kde tok prorazí agradační nebo antropogenní protipovodňový val stupeň oddělující plošiny nivy o různé výškové úrovni akumulační forma kuželovitého nebo protáhlého tvaru, vznikající uložením sedimentů blokovo-bahenního proudu v horském terénu antropogenní vyvýšená forma podél vodního toku, bránící vybřežování stabilizace dna pomocí betonu stabilizace dna kameny (obvykle zpevněno betonem či jiným pojivem) nizká příčná stavba (obvykle do 1,5 m výšky) vyšší příčná stavba (obvykle nad 1,5 m výšky) zdrsněný prudký úsek toku stabilizovaný velkým imobilním materiálem, přírodě bližší náhrada příčných objektů přičná stavba, užívaná pro plavební nebo vodohospodářské účely nebo výrobu elektřiny prohlubeň pod příčnou stavbou, obvykle se zpevněným dnem či břehy, slouží k tlumení energie vody antropogenní struktura, více či méně kolmá na směr toku, sloužící k usměrnění proudění (např. jako protierozní ochrana břehů) tradiční forma zpevnění břehů používající živé vrbové řízky k vytvoření flexibilní a rostoucí stabilizace stabilizace břehů využívající klády umístěné rovnoběžně s tokem tradiční forma zpevnění břehů používající válce z vrbových prutů moderní typ opevnění břehů, tvárnice prorostlé vegetací opevnění břehů pomocí více či méně pravidelného uspořádání imobilních balvanů opevnění břehů balvany tak, aby tvořily rovnou plochu a často jsou stabilizovanými pojivem (např. beton), někdy jsou spáry vyplněny jen zeminou či štěrkem drátokamenné opevňovací struktury voda tekoucí v betonovém korytě zdi budované rovnoběžně s vodním tokem zpevněná příčná struktura, umožňující průjezd vozidel za obvyklých průtoků struktura umožňující vodě protékat pod cestou, železnicí apod., obvykle kruhového nebo obdélníkového průměru s menší šířkou, než je šířka toku struktura překonávající tok, se silnicí, cestou nebo železnicí struktura překonávající tok, se zatrubněním oficiální geodetický bod, vedený v národní databázi vlastní měřický bod, zaměřený geodetickými metodami stabilizovaný bod (např. pro opakovaná měření) ostatní vzorkovací body (např. odběr sedimentů, fytocenologické snímkování apod.) místo zaměřeného příčného profilu tokem 1) záleží na měřítku; u plošné geometrie se používají liniové symboly pro hrany fotky barva 3.1 barva dle přírodnosti vylučuje se s 1.3 migračně prostupný (s rybím přechodem): Ano/Ne výška, sklon Barvy: 90-115-45 125-145-120240-180-180 240-240-180 210-240-1800-0-0 65-230-240 55-90-190 110-95-45 195-150-15 korytové formace, křížení erozní transportně-vyr. převa žující pro ces akumulační proudění vodní prvky v nivě tvary reliéfu dřevo přírodní antrop. ovlivněná antrop. objekty veget ace 160-75-180 Ke stažení: TT TrueType Font file  ArcGIS Style file ArcGIS database velikost mapování 220-40-0 6. 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# # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ # ## ### #### ## # #### "" """ """" """ """" """" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $ $$$ $$$$ """ """ " " " " " " " " " $ $ $ $ $ $ $ $ % % % % % % % % 1 1 1 11 1 1 1 1 % ( % ( ( ( ( ( %% % % % % % % % % % % 11 1 ( % ccc c c c ccccccccc c c cc ccccccc c c c ccc ccc c 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 5 5 5 5 5 5 5 5 5 5 5 5 444 444 c c c cccc 4 4 4 555 j- j- j- j- j- j- j-j- j-j- j- j- j-j- j- j- j-j- j- j- j- ) ) ) ) )j- 5 m Vegetation trees (decidious) shrubs Channel-reach morpology pool-riffle plane bed bedrock channel low discharge zone of fast flow Bed sediment and dominant process Bedrock channel, erosion Cobble, erosion Cobble, deposition Channel units boulder step bedrock step riffle pool bar, gravel bar, cobble bar, boulder cone gully bank failure, active bank failure, stabilised floodplain terrace small wood accumulation a) Lubina 5 m 1 : 150 # 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# ####### $ $ $$$$$$$$ """""""" $$$$$$$$ """""" " " " " " """""" $$$$$$ $ $ $ $ $ $$$$$$ " " " """""" $ $ $ $ $$$$$$ 4 4 4 4 4 4 4 4 4 4 4 " "$ $ # #$ $ $ 4 4 4 555 j- j- j- j- j- j-j- j- j- j-j- j- j-j- j- j- j-j- j- j-j- j- * * * * * * * * * * * * ** * * * * * * * * j-) h=1.6 m h=0.2 m Vegetation trees (decidious) grass Channel-reach morpology plain bed low discharge zone of fast flow zone of slow flow Bed sediment and dominant process gravel, transport-balanced gravel, deposition gravel, erosion cobble, erosion Channel units step riffle scour hole bar, gravel bar, cobble rock ripraps concrete flexmats small wood accumulation bed sill check dam c) Bystrý 5 m 1 : 150 Vzorové mapy 0 1 2 �� % & ' ( / �� 9 : ; < �� )) ** �� �� �� TW ���� �� 8� ��������������� """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" """""""""""""""""""""""" ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " # # # # # # # # # # # # # # # # # # # # # " " " " " " " " " " " " $ $ $ $ $ $ $ $ $ $ $ $ # # # # # # # # # # # # # # # # # # # # # " " " " " " " " " " " " $ $ $ $ $ $ $ $ $ $ $ $ # # # # # # # # # # # # # # # # # # # # # " " " " " " " " " " " " $ $ $ $ $ $ $ $ $ $ $ $ $$$$ $$$$$ """"" """"" ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " " " " " $ $ $ $ $ $ $ $ $ $ $ $ $ $$$$$$$$ $$$$$$$$$ $$$$$$$$$ $$$$$$$ N/A N/A 7777777777777777777777777777 77777777777777777777777777 !!!!!!!!! !!!!!!!!! -- ++ ,, ###### ###### ###### """""" """""" ###### ###### ###### """""" """""" ###### ###### ###### """""" """""" no a` CBl a` CB a` lk a` lkl 1.2.1 1.2.2 1.5.1 1.5.2 1.5.3 1.5.4 1.5.5 1.6.1 1.6.2 1.6.3 1.6.4 1.6.7 1.6.8 1.7.2 1.7.4 2.1.1 2.1.2 2.2.1 2.1.3.1 2.1.4.1 5.2 5.4 3.2.1 3.2.3 4.3.1 4.3.2 4.3.3 4.5.5 4.5.6