Vortices Enhance Diffusion in Dense Granular Flows

Prashidha Kharel and Pierre Rognon
Phys. Rev. Lett. 119, 178001 – Published 23 October 2017
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Abstract

This Letter introduces unexpected diffusion properties in dense granular flows and shows that they result from the development of partially jammed clusters of grains, or granular vortices. Transverse diffusion coefficients D and average vortex sizes are systematically measured in simulated plane shear flows at differing inertial numbers I revealing (i) a strong deviation from the expected scaling Dd2γ˙ involving the grain size d and shear rate γ˙ and (ii) an increase in average vortex size at low I, following dI12 but limited by the system size. A general scaling Ddγ˙ is introduced that captures all the measurements and highlights the key role of vortex size. This leads to establishing a scaling for the diffusivity in dense granular flow as Dd2γ˙/ti involving the geometric average of shear time 1/γ˙ and inertial time ti as the relevant time scale. Analysis of grain trajectories is further evidence that this diffusion process arises from a vortex-driven random walk.

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  • Received 23 May 2017

DOI:https://doi.org/10.1103/PhysRevLett.119.178001

© 2017 American Physical Society

Physics Subject Headings (PhySH)

Polymers & Soft Matter

Authors & Affiliations

Prashidha Kharel* and Pierre Rognon

  • Particles and Grains Laboratory, School of Civil Engineering, The University of Sydney, Sydney, NSW 2006, Australia

  • *prashidha.kharel@sydney.edu.au
  • pierre.rognon@sydney.edu.au

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Issue

Vol. 119, Iss. 17 — 27 October 2017

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