Unsaturated Zone Flow
Unsaturated Zone Flow is a hydrological flow process in porous media hydrogeology characterized by the movement of water through soil pores under variable saturation conditions where pore spaces contain both air and water, distinguishing it from saturated groundwater flow by the dependence of hydraulic conductivity and capillary forces on moisture content.
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Unsaturated water flow within porous materials observed by NMR imaging
R. J. Gummerson, Christopher Hall, William D. Hoff et al. · Nature · 1979 · 315 citations
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United States Geological Survey
Reston, United States
21 h-index
60 publications
2.6K citations

Lawrence Berkeley National Laboratory
Berkeley, United States
11 h-index
43 publications
1.5K citations

University of Wisconsin–Milwaukee
Milwaukee, United States
11 h-index
20 publications
872 citations
University of Arizona
Tucson, United States
10 h-index
17 publications
1.5K citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
24 publications
1.1K citations

Pacific Northwest National Laboratory
Richland, United States
8 h-index
17 publications
853 citations
Wuhan University
Wuhan, China
8 h-index
31 publications
1.1K citations
Desert Research Institute
Reno, United States
7 h-index
18 publications
770 citations
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70 publications · 5.1K citations
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VZJ · 39 publications · 2K citations
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SSSAJ · 22 publications · 942 citations
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