Interrill Erodibility is a soil property representing the susceptibility of soil particles to detachment and transport by rainfall and overland flow in areas between rills, distinguished from rill erodibility by its focus on sheet erosion processes driven by splash, wash, and laminar flow rather than channelized flow.
82
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5.5K
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222
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87
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2017–2026
17
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82
How Rain Intensity Affects Interrill Erosion
L. D. Meyer · Transactions of the ASAE · 1981 · 165 citations
Agriculture, Agronomy, Soil Sciences +17
1–5 of 82
Authors
222
- DCDennis C. Flanagan
National Soil Erosion Research Laboratory, United States
4 publications · 94 citations
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- LD
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1–5 of 222
Institutions
87
National Soil Erosion Research Laboratory
West Lafayette, United States
9 h-index
14 publications
661 citations
Institute of Soil and Water Conservation
Yangling, China
8 h-index
22 publications
1K citations
Northwest A&F University
Yangling, China
6 h-index
18 publications
755 citations
Purdue University West Lafayette
West Lafayette, United States
5 h-index
9 publications
547 citations
Ministry of Water Resources of the People's Republic of China
Beijing, China
4 h-index
8 publications
328 citations
Beijing Normal University
Beijing, China
3 h-index
18 publications
584 citations
Chinese Academy of Sciences
Beijing, China
3 h-index
5 publications
289 citations
KU Leuven
Leuven, Belgium
2 h-index
3 publications
112 citations
1–8 of 87
Venues
- Transactions of the ASAE
12 publications · 2.2K citations
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- Soil Science Society of America Journal
SSSAJ · 12 publications · 795 citations
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- Soil and Tillage Research
9 publications · 382 citations
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- CATENA
7 publications · 486 citations
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- Earth Surface Processes and Landforms
5 publications · 273 citations
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