Simplified Dual Continuum Approach to Modeling Subsurface Runoff from a Hillslope Segment

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F05%3A01116860" target="_blank" >RIV/68407700:21110/05:01116860 - 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
Simplified Dual Continuum Approach to Modeling Subsurface Runoff from a Hillslope Segment
Original language description
Shallow subsurface flow usually takes place at the interface of well permeable surface soil layers and less permeable underlying soil or bedrock strata. This type of saturated downhill flow is often encountered in hillslopes of mountainous or upland watersheds. Typically, it occurs only for a short period of time as an immediate response to intense rainfall events. Within the proposed conceptual model, the flow in a hillslope can be regarded as superposition of two components: one-dimensional vertical component (variably saturated matrix/macropore soil water movement) and onedimensional downhill component (saturated flow along the impervious or less permeable soil-bedrock interface). Illustrative example of the model application is provided.
Czech name
Zjednodušený přístup modelování hypodermického odtoku ze svahového segmentu pomocí principu duálního kontinua
Czech description
Zjednodušený přístup modelování hypodermického odtoku ze svahového segmentu pomocí principu duálního kontinua

Project
<a href="/en/project/GA205%2F05%2F2312" target="_blank" >GA205/05/2312: Soil water dynamics and its impact on runoff generation in headwater basins of the Czech Republic</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2005
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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