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Steady state of tapped granular polygons

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Steady state of tapped granular polygons

Auteurs : Carlos M. Carlevaro [Argentine] ; Luis A. Pugnaloni [Argentine]

Source :

RBID : ISTEX:FAC215E8152A70950D6B8B0D60534B5912395D59

Abstract

The steady state packing fraction of a tapped granular bed is studied for different grainshapes via a discrete element method. Grains are monosized regular polygons, fromtriangles to icosagons. Comparisons with disc packings show that the steady state packingfraction as a function of the tapping intensity presents the same general trends inpolygon packings. However, better packing fractions are obtained, as expected, forshapes that can tessellate the plane (triangles, squares and hexagons). In addition,we find a sharp transition for packings of polygons with more than 13 verticessignaled by a discontinuity in the packing fraction at a particular tapping intensity.Density fluctuations for most shapes are consistent with recent experimentalfindings in disc packing; however, a peculiar behavior is found for triangles andsquares.

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DOI: 10.1088/1742-5468/2011/01/P01007

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ISTEX:FAC215E8152A70950D6B8B0D60534B5912395D59

Le document en format XML

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<div type="abstract">The steady state packing fraction of a tapped granular bed is studied for different grainshapes via a discrete element method. Grains are monosized regular polygons, fromtriangles to icosagons. Comparisons with disc packings show that the steady state packingfraction as a function of the tapping intensity presents the same general trends inpolygon packings. However, better packing fractions are obtained, as expected, forshapes that can tessellate the plane (triangles, squares and hexagons). In addition,we find a sharp transition for packings of polygons with more than 13 verticessignaled by a discontinuity in the packing fraction at a particular tapping intensity.Density fluctuations for most shapes are consistent with recent experimentalfindings in disc packing; however, a peculiar behavior is found for triangles andsquares.</div>
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