Richards Equation
Richards Equation is a partial differential equation in porous media flow theory that describes the movement of water in unsaturated soils by extending Darcy's law to account for capillary and gravitational forces, thereby distinguishing it from saturated flow models through its dependence on soil moisture content and pressure head.
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2017–2026
184
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Richards' Equation
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Modeling infiltration during a steady rain
Russell G Mein, Curtis L. Larson · Water Resources Research · 1973 · 1K citations
Alexandre M. Tartakovsky, Carlos Ortiz Marrero, Paris Perdikaris et al. · Water Resources Research · 2020 · 475 citations · Full text
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Institut National de la Recherche Scientifique, Canada
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Centre National de la Recherche Scientifique
Paris, France
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65 publications
3.1K citations
University of Arizona
Tucson, United States
16 h-index
24 publications
1.3K citations
Wageningen University & Research
Wageningen, The Netherlands
14 h-index
30 publications
2.2K citations
Forschungszentrum Jülich
Jülich, Germany
11 h-index
40 publications
1.8K citations
University of Bergen
Bergen, Norway
10 h-index
19 publications
1.5K citations
University of Stuttgart
Stuttgart, Germany
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11 publications
860 citations
Los Alamos National Laboratory
Los Alamos, United States
9 h-index
20 publications
929 citations
University of California, Davis
Davis, United States
9 h-index
16 publications
712 citations
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VZJ · 52 publications · 2.6K citations
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SSSAJ · 21 publications · 910 citations
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