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

Result code in 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>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Spatial-Temporal Evolution of the Unique Preserved Meandering System in Central Europe
Original language description
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
Czech name
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Czech description
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Project
<a href="/en/project/EE2.3.20.0170" target="_blank" >EE2.3.20.0170: Building of Research Team in the Field of Environmental Modeling and the Use of Geoinformation Systems with the Consequence in Participation in International Networks and Programs</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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