Rapid Recharge Processes
Rapid Recharge Processes is a hydrological phenomenon characterized by the swift infiltration and subsurface conveyance of floodwaters through highly conductive karst pathways, distinguished from slower groundwater recharge mechanisms by its direct and temporally compressed response to precipitation or flood events.
21
Publications
783
Citations
72
Authors
39
Institutions
Publications per year
2017–2026
3
Parents
21
1–5 of 21
72
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39

British Geological Survey
Nottingham, United Kingdom
3 h-index
9 publications
268 citations
United States Geological Survey
Reston, United States
3 h-index
6 publications
180 citations

University of Aberdeen
Aberdeen, United Kingdom
2 h-index
4 publications
258 citations

University of Birmingham
Birmingham, United Kingdom
1 h-index
2 publications
46 citations

Université de Nîmes
Nîmes, France
1 h-index
2 publications
124 citations

Monash University
Melbourne, Australia
1 h-index
4 publications
184 citations
Université Paris-Sud
Orsay, France
1 h-index
1 publications
62 citations
Schlumberger (Ireland)
Dublin, Ireland
1 h-index
2 publications
184 citations
1–8 of 39
GW · 3 publications · 81 citations
3
h-index
2 publications · 69 citations
2
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WEJ · 2 publications · 44 citations
2
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2 publications · 138 citations
2
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2 publications · 115 citations
2
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1–5