Karst Recharge
Karst Recharge is a type of groundwater recharge process characterized by the infiltration and subsurface flow of water through conduits, fractures, and solution-enhanced pathways in soluble rock formations, primarily limestone and dolomite, where accelerated flow occurs due to the development of karstified porosity and preferential flow networks.
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8.3K
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532
Authors
225
Institutions
Publications per year
2017–2026
56
Parents
168
Karst groundwater: a challenge for new resources
Michel Bakalowicz · Hydrogeology Journal · 2005 · 931 citations
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225

University of Freiburg
Freiburg im Breisgau, Germany
11 h-index
25 publications
1.7K citations
China University of Geosciences
Wuhan, China
8 h-index
38 publications
984 citations

Université de Montpellier
Montpellier, France
7 h-index
22 publications
1.2K citations

Universidad de Málaga
Málaga, Spain
6 h-index
12 publications
875 citations

University of Göttingen
Göttingen, Germany
6 h-index
7 publications
579 citations
Karlsruhe Institute of Technology
Karlsruhe, Germany
6 h-index
22 publications
657 citations

University of Bristol
Bristol, United Kingdom
6 h-index
15 publications
1.4K citations
Laboratoire HydroSciences Montpellier
Montpellier, France
5 h-index
12 publications
726 citations
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32 publications · 2.1K citations
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17 publications · 1.4K citations
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11 publications · 949 citations
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10 publications · 239 citations
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8 publications · 352 citations
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