Particle-resolved Navier-Stokes simulations with the Immersed Boundary Method yield a complete parameterization of the Gibson equation for self-weight consolidation of cohesive and non-cohesive sediments from first principles.
Winterwerp, On the flocculation and settling velocity of estuarine mud, Continental Shelf Research 22, 1339 (2002)
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Consolidation of freshly deposited cohesive and non-cohesive sediment: particle-resolved simulations
Particle-resolved Navier-Stokes simulations with the Immersed Boundary Method yield a complete parameterization of the Gibson equation for self-weight consolidation of cohesive and non-cohesive sediments from first principles.