Comparison of Two Different Approaches to Modeling Subsurface Runoff at the Hillslope Scale

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F06%3A00125053" target="_blank" >RIV/68407700:21110/06:00125053 - 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

Comparison of Two Different Approaches to Modeling Subsurface Runoff at the Hillslope Scale

Popis výsledku v původním jazyce

Two conceptually different approaches to numerical modeling of a hillslope response to a rainstorm are presented and compared. In the first approach, the flow of water in a variably saturated hillslope segment is described as vertical planar flow using two-dimensional Richards' equation. Preferential flow effects are taken into account by formulating a dual set of two-dimensional governing equations, which reflects the dual character of the flow in the soil matrix and in the preferential flow domain. Inthe second approach, one-dimensional variably saturated vertical flow is coupled with one-dimensional saturated subsurface flow along the soil-bedrock interface. The saturated downhill flow is described by one-dimensional diffusion wave equation while the vertical flow is modeled using a dual set of one-dimensional Richards' equations.

Název v anglickém jazyce

Comparison of Two Different Approaches to Modeling Subsurface Runoff at the Hillslope Scale

Popis výsledku anglicky

Two conceptually different approaches to numerical modeling of a hillslope response to a rainstorm are presented and compared. In the first approach, the flow of water in a variably saturated hillslope segment is described as vertical planar flow using two-dimensional Richards' equation. Preferential flow effects are taken into account by formulating a dual set of two-dimensional governing equations, which reflects the dual character of the flow in the soil matrix and in the preferential flow domain. Inthe second approach, one-dimensional variably saturated vertical flow is coupled with one-dimensional saturated subsurface flow along the soil-bedrock interface. The saturated downhill flow is described by one-dimensional diffusion wave equation while the vertical flow is modeled using a dual set of one-dimensional Richards' equations.

Druh

D - Stať ve sborníku

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F05%2F2312" target="_blank" >GA205/05/2312: Dynamika půdní vlhkosti ve vztahu k tvorbě odtoku v horských povodích ČR</a><br>

Návaznosti

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

Rok uplatnění

2006

Kód důvěrnosti údajů

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

Název statě ve sborníku

Geophysical Research Abstracts: Volume 8, 2006

ISBN

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ISSN

1029-7006

e-ISSN

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Počet stran výsledku

1

Strana od-do

999

Název nakladatele

European Geosciences Union

Místo vydání

Strasbourg Ceres

Místo konání akce

Vídeň

Datum konání akce

2. 4. 2006

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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