Coarsening of Faraday Heaps: Experiment, Simulation, and Theory

Henk Jan van Gerner, Gabriel A. Caballero-Robledo, Devaraj van der Meer, Ko van der Weele, and Martin A. van der Hoef
Phys. Rev. Lett. 103, 028001 – Published 6 July 2009
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Abstract

When a layer of granular material is vertically shaken, the surface spontaneously breaks up in a landscape of small Faraday heaps that merge into larger ones on an ever increasing time scale. This coarsening process is studied in a linear setup, for which the average life span of the transient state with N Faraday heaps is shown to scale as N3. We describe this process by a set of differential equations for the peak positions; the calculated evolution of the landscape is in excellent agreement with both the experiments and simulations. The same model explains the observational fact that the number of heaps towards the end of the process decreases approximately as N(t)t1/2.

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  • Received 14 January 2009

DOI:https://doi.org/10.1103/PhysRevLett.103.028001

©2009 American Physical Society

Authors & Affiliations

Henk Jan van Gerner1, Gabriel A. Caballero-Robledo1,2, Devaraj van der Meer1, Ko van der Weele3, and Martin A. van der Hoef1

  • 1Faculty of Science and Technology, University of Twente, 7500 AE Enschede, The Netherlands
  • 2Centro de Investigación en Materiales Avanzados S. C., Nuevo León, Mexico
  • 3Department of Mathematics, University of Patras, 26500 Patras, Greece

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Issue

Vol. 103, Iss. 2 — 10 July 2009

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