The process of a system exploring its state space, leading to equilibration.Mixing in physics refers to the process by which a system explores its available states and eventually reaches equilibrium. It is a central concept in statistical mechanics and dynamical systems theory. A system is said to be mixing if, over time, any subset of its possible states becomes uniformly distributed throughout the entire state space. This is stronger than mere ergodicity: while ergodic systems visit all states, mixing ensures that correlations between initial and final states decay rapidly, so the system 'forgets' its starting conditions.
The concept of mixing was formalized in the early 20th century by mathematicians and physicists working on the foundations of statistical mechanics, particularly in the context of ergodic theory. Key contributions came from John von Neumann and George David Birkhoff in the 1930s.
Imagine stirring cream into coffee: initially, the cream forms localized blobs, but after enough stirring, it becomes uniformly distributed. Mathematically, mixing is described by the decay of correlation functions — quantities that measure how much the state at time t depends on the initial state. In chaotic systems, mixing occurs because nearby trajectories diverge exponentially, causing information about the initial state to be lost. In quantum systems, mixing can be studied through the entanglement spectrum, which reveals how information spreads across different parts of the system.
Mixing is crucial in chemical engineering for designing reactors and mixers, in environmental science for understanding pollutant dispersion in porous media, and in quantum computing for understanding decoherence and thermalization.
The 'quantum Mpemba effect' — where a quantum system cools faster when it starts hotter — was recently observed in experiments with trapped ions, and it is intimately connected to how mixing occurs in quantum systems.

