arXiv · cond-mat/9801132
Triangular avalanches and uphill instabilities
Abstract
Recent experiments show that an avalanche initiated from a point source propagates downwards by invading a triangular shaped region. The opening angle of this triangle appears to reach 180$^o$ for a critical inclination of the pile, beyond which avalanches also propage upwards. We propose a simple interpretation of these observations, based on an extension of a phenomenological model for surface flows.
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Jean-Philippe Bouchaud, Michael Cates. 1998-01-14. Triangular avalanches and uphill instabilities. https://arxiv.org/abs/cond-mat/9801132
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