Feedback mechanisms for self-organization to the edge of a phase transition
Victor Buend\'ia, Serena di Santo, Juan A. Bonachela, Miguel, A. Mu\~noz

TL;DR
This paper reviews feedback mechanisms that enable systems to self-organize near phase transitions, focusing on self-organized criticality and bistability, and discusses their implications across physical, geological, and biological systems.
Contribution
It provides a comprehensive comparison of SOC and SOB, introduces related concepts, and discusses how feedback mechanisms drive self-organization to critical or bistable states.
Findings
SOB explains sandpile experiments more accurately than SOC.
Both SOC and SOB produce scale-invariant activity avalanches.
Feedback mechanisms are key to self-organization at phase transition edges.
Abstract
Scale-free outbursts of activity are commonly observed in physical, geological, and biological systems. The idea of self-organized criticality (SOC), introduced back in 1987 by Bak, Tang and Wiesenfeld suggests that, under certain circumstances, natural systems can seemingly self-tune to a critical state with its concomitant power-laws and scaling. Theoretical progress allowed for a rationalization of how SOC works by relating its critical properties to those of a standard non-equilibrium second-order phase transition that separates an active state in which dynamical activity reverberates indefinitely, from an absorbing or quiescent state where activity eventually ceases. Here, we briefly review these ideas as well as a recent closely-related concept: self-organized bistability (SOB). In SOB, the very same type of feedback operates in a system characterized by a discontinuos phase…
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