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DefinitionDefinition: AI-adaptedProof: Not applicablePipeline-generatedverified 2026-10-22 (gpt-6.1-sol)
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Stationary path entropy for a finite-state jump process

Definition

Let E be a finite nonempty state set, let qxy≥0 be finite time-homogeneous transition rates for distinct x,y∈E, and let Q be their row generator. Let π be a strictly positive probability row vector with πQ=0; the forward-equation theorem shows that this is a stationary law when used initially. Assume symmetric support: qxy>0 if and only if qyx>0. For a sample path on a finite interval [0,T] with successive jump states x0,x1,…,xn, define its stationary path entropy by

ST:=∑j=1nlog⁡(πxj−1qxj−1xjπxjqxjxj−1).

The bounded-rate path-density lemma shows that the process is nonexplosive on every finite horizon. It also gives zero density to every finite path sequence containing a transition x→y with qxy=0. Since there are countably many finite state sequences, the union of those path strata is null. Hence almost surely the path has finitely many jumps and every jump uses a positive-rate edge. Define ST by the displayed sum on this full-probability set, and set ST=0 on its null complement, including paths with infinitely many jumps. Every logarithm on the full-probability set is defined because πx>0 and symmetric support makes both rates in each jump ratio positive. Its Borel preimages are countable unions of measurable path strata indexed by jump number and finite state sequence, together with the null-complement convention, so ST is a real random variable. The empty sum for a path with no jumps is 0. The quantity ST is dimensionless and depends only on the ordered jump states, not on their times. Detailed balance with respect to π means πxqxy=πyqyx for every pair x≠y; under this condition each jump contribution is zero, but no detailed-balance condition is part of this definition.

Remarks

ST is a mathematical log-likelihood-ratio statistic for paths. It is not automatically the physical entropy change of a reservoir or system. A thermodynamic interpretation requires additional physical assumptions, such as a specified relation between each forward/reverse rate ratio and the corresponding reservoir entropy transfer; if a model identifies kBST with an entropy change, its units are J/K.

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