Subsurface Connectivity
Subsurface Connectivity is a hydrological construct that characterizes the degree and spatial continuity of subsurface flow paths through which water, solutes, and energy are transmitted between landscape positions, distinguishing it from surface or near-surface hydrological connectivity by its dependence on soil and geological structure, pore network architecture, and subsurface hydraulic gradients.
31
Publications
1.8K
Citations
109
Authors
58
Institutions
Publications per year
2017–2026
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58

University of Freiburg
Freiburg im Breisgau, Germany
3 h-index
3 publications
194 citations
University of Zurich
Zurich, Switzerland
3 h-index
3 publications
291 citations
The University of Texas at Austin
Austin, United States
3 h-index
5 publications
92 citations
Duke University
Durham, United States
2 h-index
3 publications
237 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
2 h-index
3 publications
211 citations

University of Wrocław
Wroclaw, Poland
2 h-index
8 publications
130 citations

University of Minnesota
Minneapolis, United States
2 h-index
2 publications
34 citations
United States Geological Survey
Reston, United States
2 h-index
7 publications
189 citations
1–8 of 58
6 publications · 271 citations
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2 publications · 81 citations
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2 publications · 81 citations
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2 publications · 169 citations
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1 publications · 17 citations
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