Hydraulic Conductivity Estimation is a methodological framework within hydrogeological analysis that quantifies the ability of a porous medium to transmit water under a hydraulic gradient, distinguishing it from other aquifer property assessments by specifically characterizing the proportionality between Darcy flux and hydraulic gradient.
1.2K
Publications
101.8K
Citations
2.7K
Authors
979
Institutions
Publications per year
2017–2026
242
Publications
1.2K
1–5 of 1.2K
Authors
2.7K
- MT
17
h-index
- JJ
14
h-index
- WD
11
h-index
- VB
11
h-index
- DE
11
h-index
1–5 of 2.7K
Institutions
979
United States Geological Survey
Reston, United States
27 h-index
93 publications
6.4K citations
Centre National de la Recherche Scientifique
Paris, France
23 h-index
76 publications
3.8K citations
U.S. Salinity Laboratory
Riverside, United States
19 h-index
32 publications
38.9K citations
University of Arizona
Tucson, United States
19 h-index
41 publications
2.8K citations
Chinese Academy of Sciences
Beijing, China
18 h-index
66 publications
2.8K citations
University of Wisconsin–Madison
Madison, United States
17 h-index
29 publications
2.6K citations
University of Kansas
Lawrence, United States
16 h-index
45 publications
4K citations
University of Waterloo
Waterloo, Canada
16 h-index
38 publications
2.1K citations
1–8 of 979
Venues
- Water Resources Research
144 publications · 21.8K citations
64
h-index
- Soil Science Society of America Journal
SSSAJ · 98 publications · 37K citations
49
h-index
- Journal of Hydrology
100 publications · 7.8K citations
40
h-index
- Ground Water
GW · 84 publications · 4.3K citations
37
h-index
- Geoderma
42 publications · 2.5K citations
32
h-index
1–5