Erosion and Deposition of Cohesive Soils

TLDR

Deposition rates of suspended cohesive sediment and bed erosion patterns have been studied less extensively. Erosion rates of cohesive beds in salt water are independent of bed shear strength and suspended sediment concentration but strongly depend on bed shear stress, initiation shear stresses are also independent of bed strength, and a critical velocity exists for clay particles above which they remain suspended and below which they deposit rapidly, with scouring confined to a narrow central zone.

Abstract

The effects of shear stress, suspended sediment concentration, and shear strength of bed on the erosion rates of a cohesive bed in an open channel with salt water have been investigated. The deposition rates of suspended cohesive sediment and the patterns of bed erosion have been studied to a lesser extent. For the experimental range the erosion rates were found to be independent of the shear strength of the bed and the concentration of suspended sediment. They depend strongly on the bed shear stress. The minimum shear stresses for initiation of erosion were also found to be independent of the shear strength of bed. There seems to exist a critical velocity for the clay part of suspended sediment, above which all such sediment remains in suspension, whereas even for velocities slightly below this critical limit, the suspended clay deposits rapidly. Scouring occurred predominantly within a well defined narrow and relatively straight zone near the center of the flume.