Driving sandpiles to criticality and beyond
arXiv:0912.3206 · doi:10.1103/PhysRevLett.104.145703
Abstract
A popular theory of self-organized criticality relates driven dissipative systems to systems with conservation. This theory predicts that the stationary density of the abelian sandpile model equals the threshold density of the fixed-energy sandpile. We refute this prediction for a wide variety of underlying graphs, including the square grid. Driven dissipative sandpiles continue to evolve even after reaching criticality. This result casts doubt on the validity of using fixed-energy sandpiles to explore the critical behavior of the abelian sandpile model at stationarity.
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Cited by in corpus (12)
- Self-Organized Bistability Associated With First-Order Phase Transitions
- Feedback mechanisms for self-organization to the edge of a phase transition
- The approach to criticality in sandpiles
- Multiple and inverse topplings in the Abelian Sandpile Model
- Numerical Study of the Correspondence Between the Dissipative and Fixed Energy Abelian Sandpile Models
- Sandpiles on the square lattice
- Exact integration of height probabilities in the Abelian Sandpile Model
- Dynamic correlations in the conserved Manna sandpile
- Cut-off for sandpiles on tiling graphs
- The spectrum of the abelian sandpile model
- Critical Density of the Abelian Manna Model via a Multi-type Branching Process
- The hockey-stick conjecture for activated random walk