Imagine a square grid. Each cell is independently open with some probability p, or blocked with probability 1 − p. Water (or fire, or disease) flows only through open cells. The question is ancient and deceptively simple: will a path of open cells connect the top of the grid to the bottom?
For small p the grid is mostly blocked; a spanning path never forms. For large p it is mostly open; a path almost surely exists. In between there is a critical probability p_c where the behaviour flips with startling sharpness — the mathematical signature of a phase transition.
Percolation was introduced by Simon Broadbent and John Hammersley in 1957 to model the random flow of gas through carbon used in gas masks. It has since become one of the central models of statistical mechanics, probability theory, and the study of critical phenomena — the same mathematical skeleton that describes magnets losing their magnetism at the Curie temperature, or the spread of an epidemic reaching a tipping point.
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