Karst Groundwater

Karst Groundwater is a hydrogeological system characterized by the movement and storage of groundwater in soluble rock formations, such as limestone or dolomite, where flow occurs predominantly through dissolution-enlarged conduits and fractures resulting from chemical weathering processes.

1.1K

Publications

45.7K

Citations

2.9K

Authors

933

Institutions

Publications per year

2017–2026

427

Authors

2.9K

  1. NG
    Nico Goldscheider

    Karlsruhe Institute of Technology, Germany

    23 publications · 2.3K citations

    21

    h-index

  2. DY
    Daoxian Yuan

    Southwest University, China

    25 publications · 1.3K citations

    20

    h-index

  3. BA
    Bartolomé Andreo

    Universidad de Málaga, Spain

    23 publications · 1.2K citations

    19

    h-index

  4. HJ
    Hervé Jourde

    Laboratoire HydroSciences Montpellier, France

    18 publications · 1.1K citations

    16

    h-index

  5. OB
    Ognjen Bonacci

    University of Split, Croatia

    19 publications · 917 citations

    16

    h-index

1–5 of 2.9K

Venues

  1. Journal of Hydrology

    145 publications · 8K citations

    53

    h-index

  2. Environmental Earth Sciences

    98 publications · 3K citations

    30

    h-index

  3. Hydrogeology Journal

    67 publications · 4.3K citations

    30

    h-index

  4. The Science of The Total Environment

    42 publications · 2K citations

    28

    h-index

  5. Environmental Geology

    61 publications · 2.4K citations

    27

    h-index

1–5