Current-induced Sedimentation

Current-Induced Sedimentation is a hydrodynamic process in which suspended sediment particles are deposited and accumulated on the seabed or port infrastructure due to the deceleration or redirection of ambient currents, distinguishing it from other sedimentation mechanisms by its direct dependence on current velocity gradients and flow-induced shear stresses.

86

Publications

4.1K

Citations

247

Authors

128

Institutions

Publications per year

2017–2026

18

Authors

247

  1. IN
    I Nick McCave

    University of Cambridge, United Kingdom

    5 publications · 320 citations

    5

    h-index

  2. AW
    Andrew W. Woods

    University of Cambridge, United Kingdom

    3 publications · 104 citations

    3

    h-index

  3. MV
    Marta Vázquez‐Urbez

    Universidad de Zaragoza, Spain

    2 publications · 50 citations

    2

    h-index

  4. TS
    Tilmann Schwenk

    University of Bremen, Germany

    2 publications · 95 citations

    2

    h-index

  5. BK
    Ben Kneller

    University of Aberdeen, United Kingdom

    2 publications · 757 citations

    2

    h-index

1–5 of 247

Venues

  1. Marine Geology

    19 publications · 877 citations

    16

    h-index

  2. Sedimentology

    5 publications · 912 citations

    5

    h-index

  3. Sedimentary Geology

    4 publications · 91 citations

    4

    h-index

  4. Geo-Marine Letters

    3 publications · 74 citations

    3

    h-index

  5. Journal of Sedimentary Research

    JSR · 3 publications · 138 citations

    3

    h-index

1–5