Porewater Flow
Porewater Flow is the subsurface movement of water through the interconnected pore spaces within sediments or soils, driven by hydraulic gradients, that mediates biogeochemical exchange between surface water and groundwater in aquatic systems such as the hyporheic zone and wetlands.
157
Publications
11.1K
Citations
509
Authors
265
Institutions
Publications per year
2017–2026
31
157
Groundwater and pore water inputs to the coastal zone
William C. Burnett, Henry Bokuniewicz, Markus Huettel et al. · Biogeochemistry · 2003 · 1K citations
Natural Resources, Hydrology, Water Resources Management +14
1–5 of 157
509
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265
Max Planck Institute for Marine Microbiology
Bremen, Germany
15 h-index
43 publications
5.1K citations

Centre National de la Recherche Scientifique
Paris, France
8 h-index
20 publications
853 citations

Chinese Academy of Sciences
Beijing, China
6 h-index
19 publications
712 citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
5 h-index
10 publications
768 citations
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering
Nanjing, China
5 h-index
14 publications
1.1K citations

Hohai University
Nanjing, China
5 h-index
14 publications
1.1K citations

The University of Queensland
Brisbane, Australia
5 h-index
11 publications
324 citations
University of South Carolina
Columbia, United States
4 h-index
11 publications
1.9K citations
1–8 of 265
12 publications · 1.3K citations
12
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6 publications · 377 citations
6
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5 publications · 280 citations
5
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5 publications · 374 citations
5
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5 publications · 395 citations
5
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