Partial Saturation
Partial Saturation is a rock physical state in which the pore space of a porous medium is incompletely filled with one or more immiscible fluids, such that the fluid phases coexist in a non-uniform distribution affecting the bulk elastic properties of the rock.
481
Publications
26.1K
Citations
1.3K
Authors
573
Institutions
Publications per year
2017–2026
79
Parents
481
Seismic attenuation: Effects of pore fluids and frictional-sliding
Kenneth W. Winkler, Amos Nur · Geophysics · 1982 · 486 citations
Natural slopes and cuts: movement and failure mechanisms
Serge Leroueil · Géotechnique · 2001 · 432 citations · Full text
1–5 of 481
1.3K
National Institute of Oceanography and Applied Geophysics, Italy
8 publications · 772 citations
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1–5 of 1.3K
573

Centre National de la Recherche Scientifique
Paris, France
14 h-index
37 publications
2.5K citations
Stanford University
Stanford, United States
10 h-index
20 publications
2.3K citations

Imperial College London
London, United Kingdom
7 h-index
17 publications
1.4K citations
National Institute of Oceanography and Applied Geophysics
Trieste, Italy
7 h-index
13 publications
1.3K citations
Hammersmith Hospital
London, United Kingdom
6 h-index
12 publications
349 citations
Michigan State University
East Lansing, United States
6 h-index
13 publications
381 citations

University of Edinburgh
Edinburgh, United Kingdom
6 h-index
9 publications
422 citations
Curtin University
Perth, Australia
5 h-index
12 publications
720 citations
1–8 of 573
20 publications · 2K citations
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16 publications · 3.2K citations
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12 publications · 694 citations
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GJI · 10 publications · 797 citations
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JGR · 8 publications · 822 citations
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