Introduction to the Physics of Cohesive Sediment in the Marine Environment¶
Winterwerp, J. C., & van Kesteren, W. G. M. (2004). Introduction to the Physics of Cohesive Sediment in the Marine Environment. Elsevier.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Estuarine Turbidity Maximum
- The gravitational component of estuarine circulation produces a near-bed landward residual current that advects fine particles inward against the seaward freshwater flow; at salinities between roughly 1 and 10 psu, salt-induced flocculation causes clay and silt particles to aggregate into flocs with settling velocities far higher than the component particles
This sourceThe monograph treatment of cohesive-sediment flocculation and of floc settling velocity as a function of floc size.
Supported in partVerified against the source
- The gravitational component of estuarine circulation produces a near-bed landward residual current that advects fine particles inward against the seaward freshwater flow; at salinities between roughly 1 and 10 psu, salt-induced flocculation causes clay and silt particles to aggregate into flocs with settling velocities far higher than the component particles
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Registry ID ref:19d3637108b2 · see in the full table