Self-organization in physics
There are several broad classes of physical processes that can be described as self-organization. Such examples from physics include:
- structural (order-disorder, first-order) phase transitions, such as
- spontaneous magnetization, crystallization (see crystal growth, and liquid crystal, in the classical domain and
- the laser, superconductivity and Bose-Einstein condensation, in the quantum domain (but with macroscopic manifestations).
- stationary thermodynamic systems away from equilibrium. The theory of dissipative structures was developed to unify the understanding of these phenomena, which include
- turbulence and convection (e.g., Bénard cells) in fluid dynamics,
- structure formation in astrophysics and cosmology (including star formation, galaxy formation)
- reaction-diffusion systems, such as oscillating chemical reactions.
- second-order phase transitions, associated with "critical points" at which the system exhibits scale-invariant structures (see fractal). Examples of these include:
- critical opalescence of fluids at the critical point
- percolation in random media
- self-organizing dynamical systems: complex systems made up of small, simple units connected to each other usually exhibit self-organization.
- The theory of self-organized criticality (SOC) claims that whenever such a system is open or dissipative, it exhibits critical (scale-invariant) behaviour similar to the static systems associated with second-order phase transitions.
- Examples include avalanches, earthquakes, forest fires, traffic jams, blackoutss in electric networks, size of cities, size of companies, mass extinctions. The theory of SOC has been more or less successfully applied to at least these systems.
- This is related to the self-organization of cellular automata.
It is sometimes debated whether static systems deserve the label of "self-organizing".