New Papers in Fluid Mechanics

Author(s): Charlie Lloyd and Robert Dorrell

Sediment-laden flows are inherently density stratified due to their vertical variation of particulate concentration. Stratification provides an inherent mechanism for flow-scale mixing processes. Here we investigate how this change in mixing mechanics impacts sediment transport using simulations of a thermally stratified turbulent channel flow with passively transported particulates. Flow-scale mixing structures (hairpin vortices) are shown to have a profound impact on sediment transport due to their coincidence with strong concentration gradients. As a result classical diffusive-based Fickian models, which assume small-scale mixing, underpredict the capability of flows to suspend sediment.

[Phys. Rev. Fluids 10, 114501] Published Wed Nov 12, 2025