Crack Flow

Crack Flow is a hydrological process in tile drainage systems whereby subsurface water preferentially moves through naturally occurring fissures or fractures in soil or bedrock, distinguished from matrix flow by its pathway through discontinuities rather than the porous medium itself.

83

Publications

3.3K

Citations

261

Authors

118

Institutions

Publications per year

2017–2026

20

Authors

261

  1. DE
    D.W. Etheridge

    University of Nottingham, United Kingdom

    2 publications · 79 citations

    2

    h-index

  2. AP
    Ahmad Pouya

    Laboratoire Navier, France

    2 publications · 67 citations

    2

    h-index

  3. JY
    J.R. Yates

    University of Sheffield, United Kingdom

    2 publications · 39 citations

    2

    h-index

  4. SB
    S.B.M. Beck

    University of Sheffield, United Kingdom

    2 publications · 39 citations

    2

    h-index

  5. KL
    Kuan Lu

    Northwestern Polytechnical University, China

    1 publications · 37 citations

    1

    h-index

1–5 of 261

Venues

  1. Journal of Sound and Vibration

    JSV · 2 publications · 83 citations

    2

    h-index

  2. Building and Environment

    2 publications · 79 citations

    2

    h-index

  3. Rock Mechanics and Rock Engineering

    2 publications · 216 citations

    2

    h-index

  4. 2

    h-index

  5. Geoderma

    2 publications · 69 citations

    2

    h-index

1–5