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.

168

Publications

8.3K

Citations

532

Authors

225

Institutions

Publications per year

2017–2026

56

Authors

532

  1. AH
    Andreas Hartmann

    University of Freiburg, Germany

    9 publications · 760 citations

    9

    h-index

  2. NG
    Nico Goldscheider

    Karlsruhe Institute of Technology, Germany

    6 publications · 265 citations

    6

    h-index

  3. JL
    Jens Lange

    University of Freiburg, Germany

    5 publications · 461 citations

    5

    h-index

  4. ML
    Mingming Luo

    China University of Geosciences, China

    4 publications · 100 citations

    4

    h-index

  5. RL
    Rudolf Liedl

    Technische Universität Dresden, Germany

    4 publications · 582 citations

    4

    h-index

1–5 of 532

Venues

  1. Journal of Hydrology

    32 publications · 2.1K citations

    26

    h-index

  2. Hydrogeology Journal

    17 publications · 1.4K citations

    15

    h-index

  3. Water Resources Research

    11 publications · 949 citations

    11

    h-index

  4. Environmental Earth Sciences

    10 publications · 239 citations

    10

    h-index

  5. Environmental Geology

    8 publications · 352 citations

    8

    h-index

1–5