Variably Saturated Flow
Variably Saturated Flow is a hydrological flow process in which the degree of pore-space saturation with water varies spatially and temporally within a porous medium, distinguishing it from fully saturated or completely unsaturated flow regimes by explicitly accounting for dynamic transitions between saturated and unsaturated zones.
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5.5K
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164
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88
Institutions
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2017–2026
8
Variants
Unsaturated-saturated Flow
Parents
63
Hsin-Chi J. Lin, David Richards, Gour‐Tsyh Yeh et al. · US Army Corps of Engineers: Engineer Research and Development Center (Knowledge Core) · 1997 · 178 citations · Full text
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Lawrence Berkeley National Laboratory, United States
2 publications · 81 citations
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University of Waterloo
Waterloo, Canada
7 h-index
15 publications
1.4K citations
University of Arizona
Tucson, United States
4 h-index
7 publications
225 citations
U.S. Salinity Laboratory
Riverside, United States
4 h-index
6 publications
717 citations
United States Geological Survey
Reston, United States
3 h-index
8 publications
704 citations
Sandia National Laboratories California
Livermore, United States
3 h-index
3 publications
125 citations

Czech Technical University in Prague
Prague, Czechia
2 h-index
2 publications
434 citations

Lawrence Berkeley National Laboratory
Berkeley, United States
2 h-index
6 publications
243 citations
Los Alamos National Laboratory
Los Alamos, United States
2 h-index
3 publications
147 citations
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VZJ · 8 publications · 509 citations
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7 publications · 383 citations
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6 publications · 567 citations
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