Hydraulic Gradient Effects
Hydraulic Gradient Effects is a hydrogeological phenomenon that refers to the influence of the spatial rate of change in hydraulic head on the effective stress distribution within a porous medium, distinguishing it from other stress-modifying factors by its direct dependence on fluid flow magnitude and direction.
257
Publications
13.9K
Citations
752
Authors
352
Institutions
Publications per year
2017–2026
71
Parents
257
1–5 of 257
752
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Institut de Recherche en Génie Civil et Mécanique, France
3 publications · 419 citations
3
h-index
1–5 of 752
352

Hohai University
Nanjing, China
7 h-index
20 publications
607 citations
Colorado State University
Fort Collins, United States
5 h-index
6 publications
177 citations

University of British Columbia
Vancouver, Canada
5 h-index
9 publications
987 citations

Central South University
Changsha, China
5 h-index
15 publications
552 citations
Queen's University
Kingston, Canada
5 h-index
11 publications
402 citations
China Institute of Water Resources and Hydropower Research
Beijing, China
4 h-index
7 publications
106 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
20 publications
1.6K citations
Institut de Recherche en Génie Civil et Mécanique
Nantes, France
4 h-index
13 publications
1.5K citations
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GW · 19 publications · 699 citations
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17 publications · 1.1K citations
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15 publications · 1.7K citations
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11 publications · 591 citations
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SSSAJ · 8 publications · 395 citations
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