Metastability of a granular surface in a spinning bucket
arXiv:cond-mat/9803112 · doi:10.1103/PhysRevE.57.4528
Abstract
The surface shape of a spinning bucket of granular material is studied using a continuum model of surface flow developed by Bouchaud et al. and Mehta et al. An experimentally observed central subcritical region is reproduced by the model. The subcritical region occurs when a metastable surface becomes unstable via a nonlinear instability mechanism. The nonlinear instability mechanism destabilizes the surface in large systems while a linear instability mechanism is relevant for smaller systems. The range of angles in which the granular surface is metastable vanishes with increasing system size.
arXiv comment8 pages with postscript figures, RevTex, to appear in Phys. Rev. E