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.
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128
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2017–2026
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University of Cambridge
Cambridge, United Kingdom
9 h-index
15 publications
725 citations

University of Bristol
Bristol, United Kingdom
3 h-index
5 publications
621 citations
Instituto Andaluz de Ciencias de la Tierra
Granada, Spain
3 h-index
3 publications
133 citations

James Cook University
Townsville, Australia
3 h-index
4 publications
293 citations
University of Bremen
Bremen, Germany
3 h-index
8 publications
375 citations

Ghent University
Ghent, Belgium
3 h-index
9 publications
826 citations

Delft University of Technology
Delft, The Netherlands
3 h-index
5 publications
90 citations

Bowdoin College
Brunswick, United States
2 h-index
2 publications
133 citations
1–8 of 128
19 publications · 877 citations
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5 publications · 912 citations
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JSR · 3 publications · 138 citations
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