Infiltration Excess Flow
Infiltration Excess Flow is a type of surface and subsurface hydrological flow process wherein water moves downslope along soil-bedrock interfaces due to the saturation of infiltration capacity, distinguished from other flow types by its dependence on precipitation intensity exceeding soil infiltrability.
74
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3.9K
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257
Authors
141
Institutions
Publications per year
2017–2026
10
Variants
Horton Overland Flow
Parents
74
Development of WEP model and its application to an urban watershed
Yangwen Jia, Guangheng Ni, Yoshihisa KAWAHARA et al. · Hydrological Processes · 2001 · 183 citations · Full text
Preferential Flow Effects on Infiltration and Runoff in Grassland and Forest Soils
Abdallah Alaoui, Ursin Caduff, Horst H. Gerke et al. · Vadose Zone Journal · 2011 · 179 citations
1–5 of 74
257
University of Illinois Urbana-Champaign, United States
7 publications · 664 citations
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141

Cornell University
Ithaca, United States
6 h-index
25 publications
2.1K citations

The University of Western Australia
Perth, Australia
5 h-index
9 publications
340 citations
Lancaster University
Lancaster, United Kingdom
4 h-index
7 publications
332 citations
Purdue University West Lafayette
West Lafayette, United States
3 h-index
8 publications
124 citations
Tsinghua University
Beijing, China
3 h-index
6 publications
322 citations
Amhara Agricultural Research Institute
Bahir Dar, Ethiopia
3 h-index
4 publications
302 citations

Bahir Dar University
Bahir Dar, Ethiopia
3 h-index
8 publications
700 citations

Pacific Northwest National Laboratory
Richland, United States
3 h-index
11 publications
172 citations
1–8 of 141
21 publications · 1.3K citations
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10 publications · 1K citations
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6 publications · 157 citations
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3 publications · 108 citations
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2 publications · 38 citations
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