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Modeling Subsurface Hillslope Runoff Dominated by Preferential Flow: One- vs. Two-Dimensional Approximation

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F14%3A00219049" target="_blank" >RIV/68407700:21110/14:00219049 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.2136/vzj2013.05.0082" target="_blank" >http://dx.doi.org/10.2136/vzj2013.05.0082</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.2136/vzj2013.05.0082" target="_blank" >10.2136/vzj2013.05.0082</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Modeling Subsurface Hillslope Runoff Dominated by Preferential Flow: One- vs. Two-Dimensional Approximation

  • Original language description

    Shallow saturated subsurface flow, frequently observed on hillslopes of headwater catchments in humid temperate climates, often dominates hydrologic responses of the catchments to major rainfall events. Typically, these responses are significantly affected by the presence of preferential flow. In this study, two approaches to modeling hillslope responses to rainstorms, which differ in dimensionality and thus also in the complexity of geometric, material, and boundary conditions, were tested and used onthe hillslope discharge data observed in an experimental trench. In the one-dimensional (1D) approach, 1D variably saturated vertical soil water flow is combined with 1D lateral saturated flow above the soil?bedrock interface. In this approach, verticalflow is modeled by means of a dual-continuum concept involving two coupled Richards? equations (representing flow in the soil matrix and in the preferential pathways), while lateral flow is described by the diffusion wave equation. In the

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DA - Hydrology and limnology

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GA205%2F08%2F1174" target="_blank" >GA205/08/1174: Hydrological fluxes in soil-plant-atmosphere system</a><br>

  • Continuities

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

Others

  • Publication year

    2014

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Vadose Zone Journal

  • ISSN

    1539-1663

  • e-ISSN

  • Volume of the periodical

    13

  • Issue of the periodical within the volume

    6

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    13

  • Pages from-to

  • UT code for WoS article

    000343161000003

  • EID of the result in the Scopus database