The shape and erosion of pebbles

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dc.creatorDurian, D. J.
dc.creatorBideaud, H.
dc.creatorDuringer, P.
dc.creatorSchroder, A.
dc.creatorMarques, C. M.
dc.date2006-07-05
dc.date.accessioned2026-07-07T07:48:06Z
dc.date.available2026-07-07T07:48:06Z
dc.descriptionThe shapes of flat pebbles may be characterized in terms of the statistical distribution of curvatures measured along their contours. We illustrate this new method for clay pebbles eroded in a controlled laboratory apparatus, and also for naturally-occurring rip-up clasts formed and eroded in the Mont St.-Michel bay. We find that the curvature distribution allows finer discrimination than traditional measures of aspect ratios. Furthermore, it connects to the microscopic action of erosion processes that are typically faster at protruding regions of high curvature. We discuss in detail how the curvature may be reliable deduced from digital photographs.
dc.description10 pages, 11 figures
dc.identifierhttps://arxiv.org/abs/cond-mat/0607122
dc.identifierhttp://arxiv.org/abs/cond-mat/0607122
dc.identifierPhys. Rev. E 75, 021301 (2007)
dc.identifierdoi:10.1103/PhysRevE.75.021301
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/124382
dc.subjectSoft Condensed Matter
dc.titleThe shape and erosion of pebbles
dc.typetext

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