Particle Nonresolved DNS‐DEM Study of Flocculation Dynamics of Cohesive Sediment in Homogeneous Isotropic Turbulence

Abstract

AbstractA two‐phase Euler‐Lagrangian framework was implemented to investigate the flocculation dynamics of cohesive sediment in isotropic turbulence. The primary particles are modeled as sticky soft spheres using the discrete element method (DEM). The attractive van der Waals forces are modeled by the DLVO theory and the JKR adhesive contact theory. The near steady state equilibrium floc size distribution (FSD) strongly depends on the ratio of the turbulent shear to the floc strength (or particle stickiness). When turbulence is strong, a single peak around the Kolmogorov length scale appears in the FSD, and the distribution fits the Weibull distribution well. A power‐law floc size distribution develops when the floc strength is greater than the destabilizing effect of turbulent shear. Sediment concentration does not significantly affect the shape of FSD or the average floc size. The average apparent floc settling velocity Ws increases with the average floc size. Fractal dimension of flocs decreases with the floc size following a power‐law relation for large flocs. Settling velocity of flocs as a function of floc size also follows a power‐law relation. Deviation from the power‐law relationship is found for large flocs because of their porous nature. At equilibrium stage, the construction by aggregation is balanced with the destruction by breakup, and the construction by breakup is balanced with the destruction by aggregation. The aggregation kernel by turbulent shear and power‐law breakup kernel can describe the dynamics reasonably well for the flocculation of cohesive sediment in homogeneous isotropic turbulence.