Particle segregation within bidisperse turbidity current evolution

doi:10.1017/jfm.2023.623

2023-09-18

PRE

DOI：10.1017/jfm.2023.623

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摘要

En 中文

Multigrain/polydispersity has a significant impact on turbidity current (TC). Despite the fact that several researches have looked into this effect, the impact of the fluid-particle interactions is not fully understood. Motivated by this, we employ the Eulerian-Lagrangian computational fluid dynamics-discrete element method model to investigate the dynamics of the bidisperse lock-exchange TC. Results show that, because the coarse particles will settle faster and stop moving forward, the two phases of bidisperse transport and fine component transport can be distinguished in the evolution of the bidisperse TC. During the bidisperse transport stage, the upper interface of each component is primarily determined by their own settling and transport characteristics and does not strongly depend on the relative fine particle volume fraction fF. Fine particles are primarily responsible for the vortical structures near the upper interface of the TC head, and the increase of fF promotes their streamwise development. In comparison, fragmented vortical coherent structures are closely related to the presence of coarse particles, which can be seen in the lower layers. Bidisperse segregation alters the collision process between dispersed phases, which differs from monodisperse TC. The collisions and segregation-induced flow establish interconnections between the two dispersed phases. In the latter stage, the transport of fine particles is inhibited by both the lift force and the contact force produced by the collision with the deposited materials. As fF rises, the negative contact force weakens, and its change is essentially balanced by the rise in negative lift force.

Keyword:

gravity currents

sediment transport

particle/fluid flows