Saturated Flow

Saturated Flow is a type of water flow in soil and other porous media in which all pores are completely filled with water and the movement of water occurs under positive hydraulic pressure gradients, so that the hydraulic conductivity is constant and equal to its saturated value.

588

Publications

32.8K

Citations

1.4K

Authors

584

Institutions

Publications per year

2017–2026

82

Authors

1.4K

  1. MT
    Martinus Th. van Genuchten

    U.S. Salinity Laboratory, United States

    12 publications · 1.3K citations

    12

    h-index

  2. DA
    D. A. Nield

    University of Auckland, New Zealand

    6 publications · 659 citations

    6

    h-index

  3. IP
    Ioan Pop

    Babeș-Bolyai University, Romania

    6 publications · 178 citations

    6

    h-index

  4. JY
    Jinzhong Yang

    Wuhan University, China

    5 publications · 338 citations

    5

    h-index

  5. JR
    J. R. Philip

    Cochin University of Science and Technology, India

    5 publications · 433 citations

    5

    h-index

1–5 of 1.4K

Venues

  1. Water Resources Research

    57 publications · 4.3K citations

    35

    h-index

  2. Journal of Hydrology

    36 publications · 1.7K citations

    23

    h-index

  3. Advances in Water Resources

    33 publications · 1.8K citations

    22

    h-index

  4. Soil Science Society of America Journal

    SSSAJ · 26 publications · 2.1K citations

    19

    h-index

  5. International Journal of Heat and Mass Transfer

    18 publications · 924 citations

    16

    h-index

1–5