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Self-Organised Criticality

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Scale Invariance
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Abstract

During this book we have encountered many examples of critical phenomenon and have highlighted their common characteristics of divergence of the range of correlations, absence of characteristic scales, fluctuations of all sizes and anomalous response (at all scales in amplitude, spatial extent and duration) to even a tiny perturbation. These characteristics are reflected in many scaling laws, expressing quantitatively the scale invariance of the phenomena. Typically, criticality occurs for a particular value of the control parameter which is adjusted externally, for example the critical temperature in second order phase transitions, percolation threshold p c or bifurcation point in a dynamic system. However, it turns out that certain systems, maintained in a nonequilibrium state by a continuous supply of material or energy, can evolve spontaneously to a critical state, without external regulation. This is the concept of self-organised criticality, which we will present in this chapter, discussing various examples.

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Notes

  1. 1.

    Other than the “trivial” scales of system size, duration of observation and, at the other extreme, the scales of the constitutive elements.

  2. 2.

    In this preliminary statement, we have deliberately omitted to take into account the spatial extension of the system. The quantity X is actually a function \(X(\vec{r})\) and will therefore evolve differently at each spatial point \(\vec{r}\). Self-organised criticality appears when, in addition, spatial correlations develop as local values of X approach the threshold X c . We will return to this point in Sect. 10.1.3.

  3. 3.

    We call hard core interaction a short ranged quasi-infinite repulsion, modelled by a hard core of radius equal to the range of this repulsive interaction.

  4. 4.

    In three dimensions a percolating path no longer makes a border and the front will extend over a whole range of concentrations. However, its foremost part will still be spontaneously localised in the region where p = p c .

  5. 5.

    A cellular automaton is a model in which time, space but also state variables take only discrete values. Such a model is therefore particularly suitable for numerical studies. Typically, particles are moved from site to site according to very simple probabilistic rules. Cellular automata are used to study many transport phenomena, for example reaction-diffusion phenomena or those encountered in hydrodynamics and population dynamics [8]. In the context of self-organised criticality, sandpiles, forest fires and traffic flow are numerically studied using this type of simulation [20].

  6. 6.

    We do not discuss here the reliability of observations or how real the phenomenon the model intends to reproduce and explain actually is.

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Lesne, A., Laguës, M. (2012). Self-Organised Criticality. In: Scale Invariance. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-15123-1_10

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