Diffuse Flow is a type of groundwater flow regime in karst aquifers characterized by slow, widespread movement of water through a network of fine fractures and pores, as opposed to concentrated flow in well-defined conduits.
222
Publications
11.9K
Citations
544
Authors
262
Institutions
Publications per year
2017–2026
30
Variants
Matrix Flow
Parents
Publications
222
1–5 of 222
Authors
544
- RG
4
h-index
- MQ
3
h-index
- RL
3
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- GW
3
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- MS
3
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1–5 of 544
Institutions
262
Centre National de la Recherche Scientifique
Paris, France
7 h-index
18 publications
347 citations
Stanford University
Stanford, United States
5 h-index
9 publications
688 citations
Durham University
Durham, United Kingdom
5 h-index
9 publications
262 citations
United States Geological Survey
Reston, United States
4 h-index
7 publications
296 citations
Tsinghua University
Beijing, China
4 h-index
9 publications
555 citations
University of Florida
Gainesville, United States
4 h-index
13 publications
581 citations
Institut de Mécanique des Fluides de Toulouse
Toulouse, France
3 h-index
6 publications
133 citations
Cornell University
Ithaca, United States
3 h-index
7 publications
595 citations
1–8 of 262
Venues
- Water Resources Research
10 publications · 630 citations
10
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- Journal of Fluids Engineering
8 publications · 262 citations
8
h-index
- Journal of Hydrology
7 publications · 834 citations
7
h-index
- Journal of Computational Physics
6 publications · 1K citations
7
h-index
- Computers & Fluids
7 publications · 146 citations
7
h-index
1–5