Vadose Zone Flow is a hydrological process representing the movement of water through the unsaturated porous media below the land surface and above the groundwater table, distinguished by its dependence on capillary forces, gravity, and matric potential gradients within the vadose zone.
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114
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597
A Network of Terrestrial Environmental Observatories in Germany
Steffen Zacharias, Heye Bogena, Luis Samaniego et al. · Vadose Zone Journal · 2011 · 603 citations · Full text
Natural Sciences, Earth Sciences, Environmental Sciences +13
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630
University of Arizona
Tucson, United States
22 h-index
65 publications
2.5K citations
Centre National de la Recherche Scientifique
Paris, France
19 h-index
74 publications
3.3K citations
Colorado School of Mines
Golden, United States
18 h-index
36 publications
3.4K citations
Pacific Northwest National Laboratory
Richland, United States
18 h-index
65 publications
2.5K citations
Ben-Gurion University of the Negev
Beersheba, Israel
18 h-index
50 publications
3.7K citations
Lawrence Berkeley National Laboratory
Berkeley, United States
16 h-index
70 publications
4K citations
University of California, Davis
Davis, United States
14 h-index
40 publications
2.6K citations
United States Geological Survey
Reston, United States
14 h-index
33 publications
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Venues
- Water Resources Research
87 publications · 7K citations
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- Vadose Zone Journal
VZJ · 114 publications · 8.1K citations
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- Journal of Hydrology
30 publications · 2.5K citations
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- Journal of Contaminant Hydrology
21 publications · 1.1K citations
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- Ground Water
GW · 19 publications · 943 citations
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