Subsurface Flow Connectivity
Subsurface Flow Connectivity is a hydrological construct that denotes the degree to which subsurface pathways enable continuous water movement between spatially distinct hydrologic units through porous media or fractures below the land surface.
30
Publications
2K
Citations
103
Authors
62
Institutions
Publications per year
2017–2026
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103
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The University of Texas at Austin
Austin, United States
3 h-index
6 publications
134 citations

The University of Western Australia
Perth, Australia
3 h-index
8 publications
585 citations
University of California, Davis
Davis, United States
2 h-index
2 publications
138 citations
University of Zurich
Zurich, Switzerland
2 h-index
2 publications
210 citations

University of Freiburg
Freiburg im Breisgau, Germany
2 h-index
2 publications
187 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
2 h-index
2 publications
210 citations
Universitat Politècnica de Catalunya
Barcelona, Spain
2 h-index
5 publications
79 citations
Oregon State University
Corvallis, United States
2 h-index
2 publications
183 citations
1–8 of 62
9 publications · 334 citations
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1 publications · 69 citations
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2 publications · 200 citations
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2 publications · 258 citations
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PRE · 1 publications · 69 citations
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