Particle segregation and diffusion in fluid-saturated granular shear flows

Kahlil F. E. Cui, Gordon G. D. Zhou, and Lu Jing
Phys. Rev. Fluids 7, 014305 – Published 11 January 2022

Abstract

Differently sized particles in sheared granular mixtures undergo size segregation and diffusive remixing, the relative magnitude of which controls the degree to which distinct particle layers form. The presence of viscous interstitial fluids affects individual particle dynamics, resulting in complex segregation and diffusion behaviors. In this study, the effects of different types of fluids (characterized by fluid density and viscosity) on these two processes are investigated, for various flow conditions and material parameters, via coupled numerical simulations of immersed granular shear flows. We observe that both the segregation velocity and the diffusion strength decrease with the fluid viscosity, but these effects occur only when the viscosity exceeds certain threshold values, indicating a transition from viscous to inertial regimes. In the low-viscosity limit where fluid and grain inertia dominate, both segregation and diffusion processes depend on flow conditions and material properties in a manner that is similar to those in dry inertial granular flows. On the other hand, decreasing the relative density between the particles and the fluid slows down segregation but does not significantly affect diffusion. Based on scaling analysis of the simulation data, empirical relationships for the segregation velocity and diffusion coefficient are developed as functions of a modified Stokes number, and are then used to extend an existing segregation-diffusion continuum equation for granular mixtures immersed in different types of fluids.

  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
4 More
  • Received 4 October 2021
  • Accepted 21 December 2021

DOI:https://doi.org/10.1103/PhysRevFluids.7.014305

©2022 American Physical Society

Physics Subject Headings (PhySH)

Fluid Dynamics

Authors & Affiliations

Kahlil F. E. Cui1,2, Gordon G. D. Zhou1,2,3,*, and Lu Jing4,†

  • 1Key Laboratory of Mountain Hazards and Earth Surface Process, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610000, China
  • 2University of Chinese Academy of Sciences, Beijing 100000, China
  • 3China-Pakistan Joint Research Center on Earth Sciences, CAS-HEC
  • 4Department of Civil Engineering, The University of Hong Kong, Pokfulam Road, Hong Kong, China

  • *gordon@imde.ac.cn
  • Present address: Department of Chemical and Biological Engineering, Northwestern University, Evanston, IL 60208, USA.

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 7, Iss. 1 — January 2022

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review Fluids

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×