Ergodic estimates after a periodic volume-preserving flow #
theorem
AVenhance.Infra.Ergodic.FlowAverages.zPeriodic_comp_flow
{d : ℕ}
{f : Homogenization.Vec d → ℝ}
(hf : IsZPeriodic f)
(X : PeriodicVolumePreservingDiffeomorphism d)
:
IsZPeriodic fun (x : Homogenization.Vec d) => f (X.toFun x)
theorem
AVenhance.Infra.Ergodic.FlowAverages.zPeriodic_square
{d : ℕ}
{f : Homogenization.Vec d → ℝ}
(hf : IsZPeriodic f)
:
IsZPeriodic fun (x : Homogenization.Vec d) => f x ^ 2
theorem
AVenhance.Infra.Ergodic.cellAverage_flow_mul_sub_le_of_composedCoordinateAnalyticL1Bounds
{d N : ℕ}
(hd : 0 < d)
(hN : 0 < N)
(X : PeriodicVolumePreservingDiffeomorphism d)
{f : Homogenization.Vec d → ℝ}
(hf : ContDiff ℝ (↑⊤) f)
(hper : IsZPeriodic f)
(Cf r : ℝ)
(hCf : 0 ≤ Cf)
(hr : 0 < r)
(hderivComp : HasCoordinateAnalyticL1Bounds (fun (x : Homogenization.Vec d) => ↑(f (X.toFun x))) Cf r)
{g : Homogenization.Vec d → ℝ}
(hg : MeasureTheory.LocallyIntegrable g MeasureTheory.volume)
(hfast : IsFastPeriodic N g)
(hNr : 1 ≤ r * ↑N)
:
Flow version of the basic L¹ covariance estimate. The derivative premise
is placed on f ∘ X, which is the function to which the Fourier estimate is
applied. Deriving it from averaged derivative bounds on f requires a
separate quantitative composition theorem.