Unsaturated Zone Flow

Unsaturated Zone Flow is a hydrological flow process in porous media hydrogeology characterized by the movement of water through soil pores under variable saturation conditions where pore spaces contain both air and water, distinguishing it from saturated groundwater flow by the dependence of hydraulic conductivity and capillary forces on moisture content.

433

Publications

22.5K

Citations

1.1K

Authors

407

Institutions

Publications per year

2017–2026

59

Authors

1.1K

  1. KM
    Krishna M. Pillai

    University of Wisconsin–Milwaukee, United States

    12 publications · 657 citations

    12

    h-index

  2. MT
    Martinus Th. van Genuchten

    U.S. Salinity Laboratory, United States

    9 publications · 877 citations

    9

    h-index

  3. JR
    John R. Nimmo

    United States Geological Survey, United States

    8 publications · 512 citations

    8

    h-index

  4. IN
    Insa Neuweiler

    Leibniz University Hannover, Germany

    6 publications · 172 citations

    6

    h-index

  5. HT
    Hua Tan

    Washington State University Vancouver, United States

    6 publications · 281 citations

    6

    h-index

1–5 of 1.1K

Venues

  1. Water Resources Research

    70 publications · 5.1K citations

    40

    h-index

  2. Vadose Zone Journal

    VZJ · 39 publications · 2K citations

    25

    h-index

  3. Journal of Hydrology

    30 publications · 1.1K citations

    21

    h-index

  4. Soil Science Society of America Journal

    SSSAJ · 22 publications · 942 citations

    19

    h-index

  5. Hydrological Processes

    16 publications · 1.1K citations

    14

    h-index

1–5