Phase diagram for inertial granular flows

E. DeGiuli, J. N. McElwaine, and M. Wyart
Phys. Rev. E 94, 012904 – Published 12 July 2016

Abstract

Flows of hard granular materials depend strongly on the interparticle friction coefficient μp and on the inertial number I, which characterizes proximity to the jamming transition where flow stops. Guided by numerical simulations, we derive the phase diagram of dense inertial flow of spherical particles, finding three regimes for 104I101: frictionless, frictional sliding, and rolling. These are distinguished by the dominant means of energy dissipation, changing from collisional to sliding friction, and back to collisional, as μp increases from zero at constant I. The three regimes differ in their kinetics and rheology; in particular, the velocity fluctuations and the stress ratio both display nonmonotonic behavior with μp, corresponding to transitions between the three regimes of flow. We rationalize the phase boundaries between these regimes, show that energy balance yields scaling relations between microscopic properties in each of them, and derive the strain scale at which particles lose memory of their velocity. For the frictional sliding regime most relevant experimentally, we find for I102.5 that the growth of the macroscopic friction μ(I) with I is induced by an increase of collisional dissipation. This implies in that range that μ(I)μ(0)I12b, where b0.2 is an exponent that characterizes both the dimensionless velocity fluctuations LIb and the density of sliding contacts χIb.

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  • Received 4 December 2015
  • Revised 21 June 2016

DOI:https://doi.org/10.1103/PhysRevE.94.012904

©2016 American Physical Society

Physics Subject Headings (PhySH)

Polymers & Soft Matter

Authors & Affiliations

E. DeGiuli1,2, J. N. McElwaine3, and M. Wyart2

  • 1New York University, Center for Soft Matter Research, 4 Washington Place, New York, New York 10003, USA
  • 2Institute of Theoretical Physics, Ecole Polytechnique Fédérale de Lausanne (EPFL), CH-1015 Lausanne, Switzerland
  • 3Department of Earth Sciences, Durham University, Science Labs, Durham, DH1 3LE, United Kingdom

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Issue

Vol. 94, Iss. 1 — July 2016

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