Abstract
When a layer of sand is vertically shaken, the surface spontaneously breaks up in a landscape of small conical “Faraday heaps,” which merge into larger ones on an ever increasing time scale. We propose a model for the heap dynamics and show analytically that the mean lifetime of the transient state with N heaps scales as N −2 . When there is an abundance of sand, such that the vibrating plate always remains completely covered, this means that the average diameter of the heaps grows as t 1/2 . Otherwise, when the sand is less plentiful and parts of the plate get depleted during the coarsening process, the average diameter of the heaps grows more slowly, namely as t 1/3 . This result compares well with experimental observations.
Original language | English |
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Article number | 042203 |
Pages (from-to) | - |
Number of pages | 8 |
Journal | Physical review E: Statistical, nonlinear, and soft matter physics |
Volume | 92 |
Issue number | 4 |
DOIs | |
Publication status | Published - 2015 |