A geometric drift function is -integrable (Meyn-Tweedie Thm 14.3.7)
ProvedMarkovChainCLT.integrable_of_geoDriftConditionLet be a Harris ergodic Markov chain with transition kernel and invariant probability distribution . Suppose a measurable function satisfies the geometric drift condition towards a measurable small set : is integrable under every and, for some and some ,
Then is -integrable:
This is Theorem 14.3.7 of Meyn and Tweedie (1993), quoted in the source's Remark 1 as "if (5) holds then ". It is the step that turns the drift function of a geometrically ergodic chain into a -integrable rate constant, which is the standing side condition under which the source's Theorem 2(ii) bounds the strong mixing coefficients by the total-variation rate.
Formalization Note Harris ergodicity is the mission's total-variation encoding (HarrisErgodic), which gives the invariance of and the -irreducibility that Meyn and Tweedie assume; the drift condition is the platform's GeoDriftCondition, whose integrability conjunct rules out the vacuous reading of a non-integrable . The -algebra of the state space is assumed countably generated (MeasurableSpace.CountablyGenerated X), the standing assumption of Meyn and Tweedie (1993, Section 3.1) on which the existence of small sets (their Theorem 5.2.2) rests; the mission's Theorem 1(i) milestone carries the same hypothesis.
import Definitions.Def_MarkovErgodicity import Definitions.Def_MarkovDriftMinorization open MeasureTheory ProbabilityTheory Filter open scoped ENNReal NNReal Topology ProbabilityTheory
theorem MarkovChainCLT.integrable_of_geoDriftCondition {X : Type*} [MeasurableSpace X]
[MeasurableSpace.CountablyGenerated X]
(P : Kernel X X) [IsMarkovKernel P] (π : Measure X) [IsProbabilityMeasure π]
(hP : HarrisErgodic P π)
(V : X → ℝ) (hV : Measurable V) (hV1 : ∀ x, 1 ≤ V x)
(C : Set X) (hC : MeasurableSet C) (hsmall : IsSmallSet P C)
(d b : ℝ) (hd : 0 < d) (hdrift : GeoDriftCondition P V d b C) :
Integrable V π := by sorry