Approach to criticality in sandpiles

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 complet...

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Main Authors: Levine, Lionel, Fey, Anne, Wilson, David B.
Other Authors: Massachusetts Institute of Technology. Department of Mathematics
Format: Article
Language:en_US
Published: American Physical Society 2011
Online Access:http://hdl.handle.net/1721.1/60853
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author Levine, Lionel
Fey, Anne
Wilson, David B.
author2 Massachusetts Institute of Technology. Department of Mathematics
author_facet Massachusetts Institute of Technology. Department of Mathematics
Levine, Lionel
Fey, Anne
Wilson, David B.
author_sort Levine, Lionel
collection MIT
description 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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spelling mit-1721.1/608532022-10-01T11:19:55Z Approach to criticality in sandpiles Levine, Lionel Fey, Anne Wilson, David B. Massachusetts Institute of Technology. Department of Mathematics Levine, Lionel Levine, Lionel 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. National Science Foundation (U.S.) 2011-01-28T18:42:27Z 2011-01-28T18:42:27Z 2010-09 2010-03 Article http://purl.org/eprint/type/JournalArticle 1539-3755 1550-2376 http://hdl.handle.net/1721.1/60853 Fey, Anne, Lionel Levine, and David B. Wilson. “Approach to criticality in sandpiles.” Physical Review E 82.3 (2010): 031121. © 2010 The American Physical Society. en_US http://dx.doi.org/10.1103/PhysRevE.82.031121 Physical Review E Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf American Physical Society APS
spellingShingle Levine, Lionel
Fey, Anne
Wilson, David B.
Approach to criticality in sandpiles
title Approach to criticality in sandpiles
title_full Approach to criticality in sandpiles
title_fullStr Approach to criticality in sandpiles
title_full_unstemmed Approach to criticality in sandpiles
title_short Approach to criticality in sandpiles
title_sort approach to criticality in sandpiles
url http://hdl.handle.net/1721.1/60853
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