Self-Organised Criticality

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Self-Organised Criticality (SOC) is a generic concept, applicable to a host of complex systems [1]. A system is said to be in this state when it is at an attractive critical point at which it behaves as in a phase transition (i.e., the spatial and temporal scales are scale-invariant, or nearly so).

In magnetically confined plasmas, this state is thought to be responsible for the global transport phenomena of profile consistency, the Bohm scaling of confinement (in L-mode) [2], and power degradation. Profile consistency is the observation that profiles tend to have roughly the same shape, regardless of the power and location of the applied heating. [3] Power degradation shows up in global transport scaling laws, and implies a sub-linear scaling of the plasma energy content with the injected power.

The basic explanation for these phenomena is self-regulation of the profiles by turbulence. [4] The strong temperature and density gradients in fusion-grade plasmas provide free energy that may drive turbulence. The turbulence then enhances transport locally, leading to a local reduction of gradients and a consequential damping of the turbulence amplitude. This feedback could be responsible for keeping the gradients below a critical value. Considered locally, the former is a description of a simple marginal state. But the interaction of such feedback mechanisms at various radial locations would lead to avalanche behaviour and a true (scale-free) self-organised state.

Indeed, there is direct evidence for avalanching behaviour in numerical simulations [5], but experimental evidence is scarce. [6] However, some indirect evidence exists. Typically, such evidence involves the detection of long-range correlations in fluctuations. [7]

Evidence for critical gradients is much more abundant. [8] [9] However, the existence of a critical gradient by itself does not prove the system is in a SOC state.

References