Capillary Fringe Effects is a hydrological phenomenon characterized by the upward movement of water into the unsaturated zone above the water table due to capillary forces, thereby influencing bank storage dynamics by enhancing moisture retention and modulating groundwater-surface water exchange.
60
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2.9K
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137
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78
Institutions
Publications per year
2017–2026
6
Parents
Publications
60
1–5 of 60
Authors
137
- RW
6
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5
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3
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3
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1–5 of 137
Institutions
78
The University of Queensland
Brisbane, Australia
7 h-index
13 publications
713 citations
University of Waterloo
Waterloo, Canada
6 h-index
15 publications
1.1K citations
University of Notre Dame
Notre Dame, United States
2 h-index
4 publications
200 citations
McMaster University
Hamilton, Canada
2 h-index
4 publications
198 citations
Weizmann Institute of Science
Rehovot, Israel
2 h-index
2 publications
100 citations
University of Florida
Gainesville, United States
2 h-index
9 publications
394 citations
University of Neuchâtel
Neuchâtel, Switzerland
2 h-index
2 publications
134 citations
Weatherford College
Weatherford, United States
2 h-index
5 publications
124 citations
1–8 of 78
Venues
- Water Resources Research
10 publications · 605 citations
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- Ground Water
GW · 6 publications · 240 citations
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- Journal of Hydrology
6 publications · 624 citations
6
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- Advances in Water Resources
5 publications · 164 citations
5
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- Journal of Contaminant Hydrology
4 publications · 348 citations
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