Unsaturated Flow

Unsaturated Flow is a form of water flow in porous media in which liquid water moves through a soil matrix that is not fully saturated, with pores partly filled by air, such that the flow is governed by gradients in soil water potential and unsaturated hydraulic conductivity rather than by conditions of full saturation.

889

Publications

53.1K

Citations

1.8K

Authors

680

Institutions

Publications per year

2017–2026

114

Authors

1.8K

  1. TJ
    T.‐C. Jim Yeh

    University of Arizona, United States

    12 publications · 1.7K citations

    12

    h-index

  2. JR
    J. R. Philip

    Cochin University of Science and Technology, India

    13 publications · 879 citations

    12

    h-index

  3. MT
    Martinus Th. van Genuchten

    U.S. Salinity Laboratory, United States

    12 publications · 1.4K citations

    12

    h-index

  4. AW
    A. W. Warrick

    University of Arizona, United States

    10 publications · 404 citations

    10

    h-index

  5. DR
    David Russo

    Agricultural Research Organization, Israel

    10 publications · 647 citations

    10

    h-index

1–5 of 1.8K

Venues

  1. Water Resources Research

    160 publications · 13.4K citations

    62

    h-index

  2. Journal of Hydrology

    94 publications · 4.4K citations

    36

    h-index

  3. Advances in Water Resources

    55 publications · 3.3K citations

    30

    h-index

  4. Soil Science Society of America Journal

    SSSAJ · 34 publications · 2.4K citations

    24

    h-index

  5. Transport in Porous Media

    31 publications · 1.2K citations

    20

    h-index

1–5