Coexistence and Transition between Shear Zones in Slow Granular Flows

Robabeh Moosavi, M. Reza Shaebani, Maniya Maleki, János Török, Dietrich E. Wolf, and Wolfgang Losert
Phys. Rev. Lett. 111, 148301 – Published 3 October 2013

Abstract

We report experiments on slow granular flows in a split-bottom Couette cell that show novel strain localization features. Nontrivial flow profiles have been observed which are shown to be the consequence of simultaneous formation of shear zones in the bulk and at the boundaries. The fluctuating band model based on a minimization principle can be fitted to the experiments over a large variation of morphology and filling height with one single fit parameter, the relative friction coefficient μrel between wall and bulk. The possibility of multiple shear zone formation is controlled by μrel. Moreover, we observe that the symmetry of an initial state, with coexisting shear zones at both side walls, breaks spontaneously below a threshold value of the shear velocity. A dynamical transition between two asymmetric flow states happens over a characteristic time scale which depends on the shear strength.

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  • Received 11 December 2012

DOI:https://doi.org/10.1103/PhysRevLett.111.148301

© 2013 American Physical Society

Authors & Affiliations

Robabeh Moosavi1, M. Reza Shaebani2,3, Maniya Maleki1, János Török4, Dietrich E. Wolf2, and Wolfgang Losert5

  • 1Department of Physics, Institute for Advanced Studies in Basic Sciences, Zanjan 45137-66731, Iran
  • 2Computational Physics Group, University of Duisburg-Essen, D-47048 Duisburg, Germany
  • 3Department of Theoretical Physics, Saarland University, D-66041 Saarbrücken, Germany
  • 4Department of Theoretical Physics, Budapest University of Technology and Economics, Budapest H-1111, Hungary
  • 5Department of Physics, University of Maryland, College Park, Maryland 20742, USA

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Issue

Vol. 111, Iss. 14 — 4 October 2013

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