Richard's Equation
Richard's Equation is a partial differential equation that describes the movement of water in unsaturated porous media by relating the rate of change of soil moisture content to the spatial gradients of hydraulic conductivity and capillary pressure, distinguishing it as the fundamental mathematical model for quantifying variably saturated flow in the vadose zone.
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560
Citations
55
Authors
32
Institutions
Publications per year
2017–2026
6
Variants
Richards' Equation
Parents
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32

University of Tehran
Tehran, Iran
2 h-index
5 publications
96 citations

University of Alberta
Edmonton, Canada
1 h-index
1 publications
27 citations
Google (United States)
Mountain View, United States
1 h-index
2 publications
144 citations

Stellenbosch University
Stellenbosch, South Africa
1 h-index
1 publications
15 citations

Shiraz University
Shiraz, Iran
1 h-index
1 publications
22 citations
Universidade de Brasília
Brasília, Brazil
1 h-index
1 publications
33 citations
Islamic Azad University of Arsanjan
Arsanjān, Iran
1 h-index
1 publications
22 citations

Sharif University of Technology
Tehran, Iran
1 h-index
2 publications
38 citations
1–8 of 32
2 publications · 47 citations
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2 publications · 41 citations
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1 publications · 34 citations
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IJOG · 1 publications · 33 citations
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GW · 1 publications · 27 citations
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