Onset of Convection in Strongly Shaken Granular Matter

Peter Eshuis, Devaraj van der Meer, Meheboob Alam, Henk Jan van Gerner, Ko van der Weele, and Detlef Lohse
Phys. Rev. Lett. 104, 038001 – Published 22 January 2010
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Abstract

Strongly vertically shaken granular matter can display a density inversion: A high-density cluster of beads is elevated by a dilute gaslike layer of fast beads underneath (“granular Leidenfrost effect”). For even stronger shaking the granular Leidenfrost state becomes unstable and granular convection rolls emerge. This transition resembles the classical onset of convection in fluid heated from below at some critical Rayleigh number. The same transition is seen in molecular dynamics (MD) simulations of the shaken granular material. The critical shaking strength for the onset of granular convection can be calculated from a linear stability analysis of a hydrodynamiclike model of the granular flow. Experiment, MD simulations, and theory quantitatively agree.

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  • Received 2 April 2009

DOI:https://doi.org/10.1103/PhysRevLett.104.038001

©2010 American Physical Society

Authors & Affiliations

Peter Eshuis1, Devaraj van der Meer1, Meheboob Alam2, Henk Jan van Gerner1, Ko van der Weele3, and Detlef Lohse1

  • 1Physics of Fluids Group, Department of Science and Technology, J. M. Burgers Center, and Impact and Mesa+ Institutes, University of Twente, P.O. Box 217, 7500 AE Enschede, The Netherlands
  • 2Engineering Mechanics Unit, Jawaharlal Nehru Center for Advanced Scientific Research, Jakkur P.O. Bangalore 560064, India
  • 3Department of Mathematics, Division of Applied Analysis, University of Patras, 26500 Patras, Greece

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Issue

Vol. 104, Iss. 3 — 22 January 2010

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