Spatial-Temporal Evolution of the Unique Preserved Meandering System in Central Europe

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F15%3A33156549" target="_blank" >RIV/61989592:15310/15:33156549 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Spatial-Temporal Evolution of the Unique Preserved Meandering System in Central Europe

Popis výsledku v původním jazyce

The channels of alluvial lowland rivers are formed by the action of flowing water on materials that have been deposited by the stream and that can be eroded and transported. The major factors that a ect the forms of an alluvial channel include water discharge, sediment characteristics, longitudinal slope, resistance of the bank and bed to erosion, vegetation, geology and human activity. According to [1], meandering rivers can be classi ed as either stable (passive) or actively meandering(active). An actively meandering river has sucient stream power to deform its channel bends through active bed and bank erosion and the growth of point bars. The result of uvial processes in a lowland region is an actively meandering river reach. Meanders evolve and respond to floods that have sucient stream power to mobilise bed and bank sediments. Conversely, a stable meandering (passive) river is one that has insucient stream power to erode its banks under current conditions. The objectives of this s

Název v anglickém jazyce

Spatial-Temporal Evolution of the Unique Preserved Meandering System in Central Europe

Popis výsledku anglicky

The channels of alluvial lowland rivers are formed by the action of flowing water on materials that have been deposited by the stream and that can be eroded and transported. The major factors that a ect the forms of an alluvial channel include water discharge, sediment characteristics, longitudinal slope, resistance of the bank and bed to erosion, vegetation, geology and human activity. According to [1], meandering rivers can be classi ed as either stable (passive) or actively meandering(active). An actively meandering river has sucient stream power to deform its channel bends through active bed and bank erosion and the growth of point bars. The result of uvial processes in a lowland region is an actively meandering river reach. Meanders evolve and respond to floods that have sucient stream power to mobilise bed and bank sediments. Conversely, a stable meandering (passive) river is one that has insucient stream power to erode its banks under current conditions. The objectives of this s

Druh

C - Kapitola v odborné knize

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

<a href="/cs/project/EE2.3.20.0170" target="_blank" >EE2.3.20.0170: Budování výzkumně-vzdělávacího týmu v oblasti modelování přírodních jevů a využití geoinformačních systémů, s vazbou na zapojení do mezinárodních sítí a programů.</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název knihy nebo sborníku

Modern Trends in Cartography

ISBN

978-3-319-07925-7

Počet stran výsledku

11

Strana od-do

507-517

Počet stran knihy

534

Název nakladatele

Springer

Místo vydání

Heidelberg

Kód UT WoS kapitoly

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