Saturated Zone Flow

Saturated Zone Flow is a hydrological process characterized by the movement of water through fully saturated porous media, where all interconnected pore spaces are filled with water under pressure, distinguished from unsaturated flow by the absence of air-water interfaces within the pore network.

141

Publications

7.6K

Citations

396

Authors

193

Institutions

Publications per year

2017–2026

24

Authors

396

  1. JM
    Jacques Mudry

    Université de Franche-Comté, France

    3 publications · 113 citations

    3

    h-index

  2. WD
    W. D. Graham

    University of Florida, United States

    3 publications · 311 citations

    3

    h-index

  3. PX
    Pei Xin

    Hohai University, China

    2 publications · 60 citations

    2

    h-index

  4. XL
    Xiuyu Liang

    Southern University of Science and Technology, China

    2 publications · 47 citations

    2

    h-index

  5. GD
    Georgia Destouni

    Stockholm University, Sweden

    2 publications · 144 citations

    2

    h-index

1–5 of 396

Venues

  1. Water Resources Research

    26 publications · 2.4K citations

    21

    h-index

  2. Soil Science Society of America Journal

    SSSAJ · 8 publications · 634 citations

    8

    h-index

  3. Journal of Hydrology

    8 publications · 332 citations

    8

    h-index

  4. Ground Water

    GW · 8 publications · 695 citations

    8

    h-index

  5. Advances in Water Resources

    6 publications · 376 citations

    6

    h-index

1–5