Saturated Zone Flow
Saturated Zone Flow is a hydrological process characterized by the movement of water through fully saturated porous media, where all interconnected pore spaces are filled with water under pressure, distinguished from unsaturated flow by the absence of air-water interfaces within the pore network.
141
Publications
7.6K
Citations
396
Authors
193
Institutions
Publications per year
2017–2026
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United States Geological Survey
Reston, United States
8 h-index
14 publications
741 citations

Lawrence Berkeley National Laboratory
Berkeley, United States
5 h-index
16 publications
655 citations
Los Alamos National Laboratory
Los Alamos, United States
4 h-index
13 publications
452 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
8 publications
222 citations
National Centre for Groundwater Research and Training
Adelaide, Australia
3 h-index
8 publications
205 citations
Texas A&M University
College Station, United States
3 h-index
3 publications
115 citations
Sandia National Laboratories California
Livermore, United States
3 h-index
3 publications
133 citations
University of Arizona
Tucson, United States
3 h-index
9 publications
327 citations
1–8 of 193
26 publications · 2.4K citations
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SSSAJ · 8 publications · 634 citations
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8 publications · 332 citations
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GW · 8 publications · 695 citations
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6 publications · 376 citations
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