Quadratic initial-point remainder for the flow's second variation.
theorem
AVenhance.Infra.Flow.ThirdSpatialRemainder.gronwallBound_zero_scale_thirdSpatialRemainder
(L a c d : ℝ)
:
theorem
AVenhance.Infra.Flow.ThirdSpatialRemainder.thirdRemainder_linearFlow_bound_on_Ico
(A : ℝ → Homogenization.Vec 2 →L[ℝ] Homogenization.Vec 2)
(M : ℝ)
(hM₀ : 0 ≤ M)
(hA : ∀ (q : ℝ), ‖A q‖ ≤ M)
{V : ℝ → Homogenization.Vec 2 → ℝ → Homogenization.Vec 2}
(hV : IsFlow (fun (q : ℝ) (v : Homogenization.Vec 2) => (A q) v) V)
(s t : ℝ)
(_hst : s ≤ t)
(v : Homogenization.Vec 2)
(q : ℝ)
:
theorem
AVenhance.Infra.Flow.exists_flow_secondVariation_quadratic_remainder_all_times_of_le
{b : ℝ → Homogenization.Vec 2 → Homogenization.Vec 2}
(hb : SmoothPeriodicField b)
{X : ℝ → Homogenization.Vec 2 → ℝ → Homogenization.Vec 2}
(hX : IsFlow b X)
(x : Homogenization.Vec 2)
(s t : ℝ)
(hst : s ≤ t)
:
On a forward interval, the selected third variation is the linear term in the initial-point Taylor expansion of the second variation, with a uniform quadratic remainder.