Soil Interface Flow

Soil Interface Flow is a type of subsurface stormflow process in which water moves laterally along a soil-bedrock interface due to differences in hydraulic conductivity and permeability between the soil and underlying impermeable or less permeable geological layers.

81

Publications

4.5K

Citations

249

Authors

111

Institutions

Publications per year

2017–2026

35

Authors

249

  1. GZ
    Ga Zhang

    Tsinghua University, China

    3 publications · 182 citations

    3

    h-index

  2. JY
    Jian-lin Yu

    Zhejiang University, China

    2 publications · 49 citations

    2

    h-index

  3. XP
    Xudong Peng

    Guizhou University, China

    2 publications · 51 citations

    2

    h-index

  4. AH
    Annette Holzapfel-Pschorn

    Max Planck Institute for Chemistry, Germany

    2 publications · 291 citations

    2

    h-index

  5. JL
    Jian Liu

    Shandong University, China

    2 publications · 81 citations

    2

    h-index

1–5 of 249

Venues

  1. Computers and Geotechnics

    5 publications · 387 citations

    5

    h-index

  2. Vadose Zone Journal

    VZJ · 4 publications · 130 citations

    4

    h-index

  3. Journal of Hydrology

    4 publications · 316 citations

    4

    h-index

  4. Soil Dynamics and Earthquake Engineering

    3 publications · 107 citations

    3

    h-index

  5. Soil and Tillage Research

    3 publications · 94 citations

    3

    h-index

1–5