Approach to criticality in sandpiles

Anne Fey, Lionel Levine, and David B. Wilson
Phys. Rev. E 82, 031121 – Published 15 September 2010

Abstract

A popular theory of self-organized criticality predicts that the stationary density of the Abelian sandpile model equals the threshold density of the corresponding fixed-energy sandpile. We recently announced that this “density conjecture” is false when the underlying graph is any of Z2, the complete graph Kn, the Cayley tree, the ladder graph, the bracelet graph, or the flower graph. In this paper, we substantiate this claim by rigorous proof and extensive simulations. We show that driven-dissipative sandpiles continue to evolve even after a constant fraction of the sand has been lost at the sink. Nevertheless, we do find (and prove) a relationship between the two models: the threshold density of the fixed-energy sandpile is the point at which the driven-dissipative sandpile begins to lose a macroscopic amount of sand to the sink.

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  • Received 16 March 2010

DOI:https://doi.org/10.1103/PhysRevE.82.031121

©2010 American Physical Society

Authors & Affiliations

Anne Fey1, Lionel Levine2, and David B. Wilson3

  • 1Delft Institute of Applied Mathematics, Delft University of Technology, Delft, The Netherlands
  • 2Department of Mathematics, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA
  • 3Microsoft Research, Redmond, Washington 98052, USA

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Issue

Vol. 82, Iss. 3 — September 2010

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