OAI/Analysis/CircleDomains/Sobolev/CoordinateEstimates.lean
13 declarations, 0 contain sorry, 0 declared as axioms
Actual coordinate energies on the completed surface
The metric trace estimate controls the sum of the actual scalar coordinate energies. Exact agreement near the retained core then gives localized estimates against the original domain, even though the original coordinates need not extend into the filled holes.
- def
OAI.CircleDomainRigidity.FiniteTransfer.gradientEnergyline 23 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.gradientEnergy_nonnegline 26 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.gradientEnergy_sphericalline 30 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.coordinateGram_energy_eq_sumline 38 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.gradientEnergy_le_coordinateGramline 44 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.continuousOn_matrixEnergy_localline 51 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.continuousOn_gradientEnergyline 68 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.integrableOn_gradientEnergyline 96 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.integrable_gradientEnergy_spherical_of_memLpline 104 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.integral_coordinateGram_eq_sumline 118Source documentation
Integrating the trace really gives the sum of all transferred coordinate energies.
theorem integral_coordinateGram_eq_sum {Ω Q K : Set (ℝ × ℝ)} (hΩ : IsOpen Ω) (hQ : IsCompact Q) (hQΩ : Q ⊆ Ω) (f : ℕ → (ℝ × ℝ) → ℝ) (hf : ∀ i, ContDiffOn ℝ ∞ (f i) Ω) (n : ℕ) {g : (ℝ × ℝ) → PlanarMetric} (hg : Continuous g) (hPD : ∀ z, (g z).PosDef) : (∫ z in Q \ K, matrixEnergy (coordinateGram f n z) (g z)) = ∑ i ∈ range n, ∫ z in Q \ K, gradientEnergy (f i) g z := by …Mentions: OAI.CircleDomainRigidity.FiniteTransfer.PlanarMetric, OAI.CircleDomainRigidity.FiniteTransfer.matrixEnergy, OAI.CircleDomainRigidity.FiniteTransfer.coordinateGram, OAI.CircleDomainRigidity.FiniteTransfer.gradientEnergy
- theorem
OAI.CircleDomainRigidity.FiniteTransfer.localized_energy_lt_sourceline 130Source documentation
Compare localized energy to the original domain, without evaluating or integrating an original coordinate in the added holes.
theorem localized_energy_lt_source {X : Type*} [MeasurableSpace X] {μ : Measure X} {Q G K E : Set X} (hQ : MeasurableSet Q) (hG : MeasurableSet G) (hK : MeasurableSet K) (hE : MeasurableSet E) (hEK : E ⊆ K) (hQKG : Q ∩ K ⊆ G) {f u T : X → ℝ} (hf : IntegrableOn f Q μ) (hu : IntegrableOn u G μ) (hT : IntegrableOn T (Q \ K) μ) (hu0 : ∀ x ∈ G, 0 ≤ u x) (hcore : ∀ x ∈ Q ∩ K, f x = u x) (htail : ∀ x ∈ Q \ K, f x ≤ T x) {ε : ℝ} (hε : (∫ x in Q \ K, T x ∂μ) < ε) : (∫ x in Q \ E, f x ∂μ) < (∫ x in G \ E, u x ∂μ) + ε := by … - theorem
OAI.CircleDomainRigidity.FiniteTransfer.integrableOn_coordinateGram_energyline 158 - theorem
OAI.CircleDomainRigidity.FiniteTransfer.localized_coordinate_energy_ltline 169Source documentation
The localized estimate for each actual transferred coordinate. The original right-hand side is integrated only over its original domain.
theorem localized_coordinate_energy_lt {Ω Q G K : Set (ℝ × ℝ)} (hΩ : IsOpen Ω) (hQ : IsCompact Q) (hQΩ : Q ⊆ Ω) (hG : MeasurableSet G) (hK : IsClosed K) (hQKG : Q ∩ K ⊆ G) (f u : ℕ → (ℝ × ℝ) → ℝ) (hf : ∀ i, ContDiffOn ℝ ∞ (f i) Ω) {n : ℕ} (hu : ∀ i < n, IntegrableOn (gradientEnergy (u i) (fun z => sphericalMetricFactor z • 1)) G) (hretain : ∀ᶠ z in 𝓝ˢ K, ∀ i < n, f i z = u i z) {g : (ℝ × ℝ) → PlanarMetric} (hg : Continuous g) (hPD : ∀ z, (g z).PosDef) (hmetric : ∀ᶠ z in 𝓝ˢ K, g z = sphericalMetricFactor z • 1) {ε : ℝ} (henergy : (∫ z in Q \ K, matrixEnergy (coordinateGram f n z) (g z)) < ε) {i : ℕ} (hi : i < n) {E : Set (ℝ × ℝ)} (hE : MeasurableSet E) (hEK : E ⊆ K) : (∫ z in Q \ E, gradientEnergy (f i) g z) < …Mentions: OAI.CircleDomainRigidity.FiniteTransfer.gradientEnergy, OAI.CircleDomainRigidity.FiniteTransfer.sphericalMetricFactor, OAI.CircleDomainRigidity.FiniteTransfer.PlanarMetric, OAI.CircleDomainRigidity.FiniteTransfer.matrixEnergy, OAI.CircleDomainRigidity.FiniteTransfer.coordinateGram