The sheet erosion analysis and the sediment transport calculation method at the experimetal area
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F14%3A00220440" target="_blank" >RIV/68407700:21110/14:00220440 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
The sheet erosion analysis and the sediment transport calculation method at the experimetal area
Popis výsledku v původním jazyce
This article deals with describing of sheet erosion at the experimental area of The Pozarsky stream catchment. The experimental area is located near the town Krivoklát, in the Central Bohemian Region, where highlands dominate. This area is characterizedby the occurrence of very deep valley, shaped like the letter "U" to "V", which contain torrents and often deep gullies. In this experimental area, there are built five torrent control cross-section objects. Especially two of them are located in the gullies, which are surrounded by managed fields. There is an assumption of the sheet erosion occurence. The sheet erosion consideration was processed by modeling erosion and transport processes with two appropriate methods ? The sediment transport calculation method based on Gavrilovic method (Skopek, 1988) and Modeling water erosion by model WaTEM / SEDEM 2.1.0, which is based on the RUSLE model (Renard et al., 1993). Both two methods deals with annual total sediment volume, but each method
Název v anglickém jazyce
The sheet erosion analysis and the sediment transport calculation method at the experimetal area
Popis výsledku anglicky
This article deals with describing of sheet erosion at the experimental area of The Pozarsky stream catchment. The experimental area is located near the town Krivoklát, in the Central Bohemian Region, where highlands dominate. This area is characterizedby the occurrence of very deep valley, shaped like the letter "U" to "V", which contain torrents and often deep gullies. In this experimental area, there are built five torrent control cross-section objects. Especially two of them are located in the gullies, which are surrounded by managed fields. There is an assumption of the sheet erosion occurence. The sheet erosion consideration was processed by modeling erosion and transport processes with two appropriate methods ? The sediment transport calculation method based on Gavrilovic method (Skopek, 1988) and Modeling water erosion by model WaTEM / SEDEM 2.1.0, which is based on the RUSLE model (Renard et al., 1993). Both two methods deals with annual total sediment volume, but each method
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
DO - Ochrana krajinných území
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
14th Geoconference on Water Resources. Forest, Marine and Ocean Ecosystems - Conference Proceedings Volume I - Hydrology & Water Resources
ISBN
978-619-7105-13-1
ISSN
1314-2704
e-ISSN
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Počet stran výsledku
8
Strana od-do
775-782
Název nakladatele
STEF92 Technology Ltd.
Místo vydání
Sofia
Místo konání akce
Albena
Datum konání akce
17. 6. 2014
Typ akce podle státní příslušnosti
WRD - Celosvětová akce
Kód UT WoS článku
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