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Collapsing granular beds: The role of interstitial air

Tess Homan, Christa Gjaltema, and Devaraj van der Meer
Phys. Rev. E 89, 052204 – Published 9 May 2014

Abstract

A prefluidized sand bed consisting of fine particles compactifies when it is subjected to a shock. We observe that the response depends on both the shock strength and the ambient pressure, where, counterintuitively, at high ambient pressure the compaction is larger, which we connect to a decrease of the static friction inside the bed. We find that the interstitial air is trapped inside the bed during and long after compaction. We deduce this from measuring the pressure changes above and below the bed: The top pressure decreases abruptly, on the time scale of the compaction, whereas that below the bed slowly rises to a maximum. Subsequently, both gently relax to ambient values. We formulate a one-dimensional diffusion model that uses only the change in bed height and the ambient pressure as an input, and we show that it leads to a fully quantitative understanding of the measured pressure variations.

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  • Received 15 October 2013

DOI:https://doi.org/10.1103/PhysRevE.89.052204

©2014 American Physical Society

Authors & Affiliations

Tess Homan, Christa Gjaltema, and Devaraj van der Meer

  • Physics of Fluids Group, Mesa+ Institute for Nanotechnology, and J. M. Burgers Centre for Fluid Dynamics, University of Twente, 7522 NB Enschede, The Netherlands

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Issue

Vol. 89, Iss. 5 — May 2014

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