Lateral Flow Paths is a hydrological flow pathway characterized by subsurface water movement predominantly parallel to the land surface, driven by soil permeability and topographic gradients, distinguishing it from vertical or direct surface runoff processes.
168
Publications
8.9K
Citations
631
Authors
279
Institutions
Publications per year
2017–2026
51
Variants
Lateral Flow Pathways
Parents
Publications
168
1–5 of 168
Authors
631
- MV
3
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- RO
3
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- YA
3
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- MW
3
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- ME
3
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1–5 of 631
Institutions
279
United States Geological Survey
Reston, United States
6 h-index
19 publications
1K citations
Centre National de la Recherche Scientifique
Paris, France
5 h-index
12 publications
562 citations
Pennsylvania State University
State College, United States
5 h-index
16 publications
1.1K citations
University of British Columbia
Vancouver, Canada
5 h-index
8 publications
601 citations
Boise State University
Boise, United States
4 h-index
11 publications
753 citations
University of Maryland, College Park
College Park, United States
3 h-index
3 publications
161 citations
Clemson University
Clemson, United States
3 h-index
8 publications
480 citations
Virginia Tech
Blacksburg, United States
3 h-index
3 publications
247 citations
1–8 of 279
Venues
- Water Resources Research
13 publications · 1.2K citations
13
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- Hydrological Processes
12 publications · 1.1K citations
11
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- Journal of Hydrology
7 publications · 442 citations
6
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- Biosensors and Bioelectronics
5 publications · 190 citations
5
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- Soil Science Society of America Journal
SSSAJ · 5 publications · 170 citations
5
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1–5