Richard's Equation

Richard's Equation is a partial differential equation that describes the movement of water in unsaturated porous media by relating the rate of change of soil moisture content to the spatial gradients of hydraulic conductivity and capillary pressure, distinguishing it as the fundamental mathematical model for quantifying variably saturated flow in the vadose zone.

21

Publications

560

Citations

55

Authors

32

Institutions

Publications per year

2017–2026

6

Variants

Richards' Equation

Authors

55

  1. RV
    Ramón Vásquez

    University of Puerto Rico-Mayaguez, Puerto Rico

    1 publications · 13 citations

    1

    h-index

  2. BV
    B. V. Bredenkamp

    Forestry Research Institute, Uzbekistan

    1 publications · 15 citations

    1

    h-index

  3. AS
    Amirhossein Shirzad

    University of Tehran, Iran

    1 publications · 22 citations

    1

    h-index

  4. XS
    Xiaohui Su

    Dalian University of Technology, China

    1 publications · 28 citations

    1

    h-index

  5. XZ
    Xiaoxian Zhang

    University of Liverpool, United Kingdom

    1 publications · 19 citations

    1

    h-index

1–5 of 55

Venues

  1. Journal of Hydrology

    2 publications · 47 citations

    2

    h-index

  2. 2

    h-index

  3. ISH Journal of Hydraulic Engineering

    1 publications · 34 citations

    1

    h-index

  4. International Journal of Geomechanics

    IJOG · 1 publications · 33 citations

    1

    h-index

  5. Ground Water

    GW · 1 publications · 27 citations

    1

    h-index

1–5