Interplay of air and sand: Faraday heaping unravelled

Henk Jan van Gerner, Martin A. van der Hoef, Devaraj van der Meer, and Ko van der Weele
Phys. Rev. E 76, 051305 – Published 26 November 2007
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Abstract

We report on numerical simulations of a vibrated granular bed including the effect of the ambient air, generating the famous Faraday heaps known from experiment. A detailed analysis of the forces shows that the heaps are formed and stabilized by the airflow through the bed while the gap between bed and vibrating bottom is growing, confirming the pressure gradient mechanism found experimentally by Thomas and Squires [Phys. Rev. Lett. 81, 574 (1998)], with the addition that the airflow is partly generated by isobars running parallel to the surface of the granular bed. Importantly, the simulations also explain the heaping instability of the initially flat surface and the experimentally observed coarsening of a number of small heaps into a larger one.

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  • Received 21 June 2006

DOI:https://doi.org/10.1103/PhysRevE.76.051305

©2007 American Physical Society

Authors & Affiliations

Henk Jan van Gerner1, Martin A. van der Hoef1, Devaraj van der Meer1, and Ko van der Weele2

  • 1Faculty of Science and Technology, University of Twente, P.O. Box 217, 7500 AE Enschede, The Netherlands
  • 2Department of Mathematics, University of Patras, 26500 Patras, Greece

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Issue

Vol. 76, Iss. 5 — November 2007

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