Vadose Zone Conductivity

Vadose Zone Conductivity is a hydrological conductivity metric that quantifies the ability of unsaturated geological materials in the vadose zone to transmit water under hydraulic gradient, distinguished from saturated hydraulic conductivity by its dependence on variable soil moisture content and matric potential.

37

Publications

2.4K

Citations

117

Authors

69

Institutions

Publications per year

2017–2026

4

Authors

117

  1. PS
    P. Sailhac

    Université de Strasbourg, France

    3 publications · 79 citations

    3

    h-index

  2. SP
    Shlomo P. Neuman

    University of Arizona, United States

    3 publications · 100 citations

    3

    h-index

  3. GM
    Guy Marquis

    Université de Strasbourg, France

    3 publications · 79 citations

    3

    h-index

  4. DB
    Daniel B. Stephens

    New Mexico Institute of Mining and Technology, United States

    2 publications · 73 citations

    2

    h-index

  5. JN
    J.J. Nitao

    Lawrence Livermore National Laboratory, United States

    2 publications · 552 citations

    2

    h-index

1–5 of 117

Venues

  1. Vadose Zone Journal

    VZJ · 6 publications · 192 citations

    6

    h-index

  2. Water Resources Research

    4 publications · 691 citations

    4

    h-index

  3. Journal of Hydrology

    5 publications · 473 citations

    4

    h-index

  4. Soil Science Society of America Journal

    SSSAJ · 3 publications · 211 citations

    3

    h-index

  5. Ground Water

    GW · 2 publications · 101 citations

    2

    h-index

1–5