Trilinear identities at a fixed time #
For slices u ∈ L² ∩ L⁵ and v ∈ L² ∩ L^{10/3} with square-integrable weak
gradients of vanishing trace, the self-transport form of u vanishes, and the
sum of the two convection pairings equals the relative convection form
∑ₖ uₖ ∑ⱼ (vⱼ - uⱼ)(∂ⱼ vₖ - ∂ⱼ uₖ). These reduce the cross-testing identity
to the relative energy inequality of lem:pv-serrin-uniqueness.
theorem
ESS.serrin_prod_memLp
{f g : CKN.Foundation.Parabolic.Vec3 → ℝ}
{p q r : ℝ}
(hp : 0 < p)
(hq : 0 < q)
(hr : 0 < r)
(h : p⁻¹ + q⁻¹ = r⁻¹)
(hf : MeasureTheory.MemLp f (ENNReal.ofReal p) MeasureTheory.volume)
(hg : MeasureTheory.MemLp g (ENNReal.ofReal q) MeasureTheory.volume)
:
MeasureTheory.MemLp (fun (x : CKN.Foundation.Parabolic.Vec3) => f x * g x) (ENNReal.ofReal r) MeasureTheory.volume
structure
ESS.SerrinSlice
(w : CKN.Foundation.Parabolic.Vec3 → CKN.Foundation.Parabolic.Vec3)
(Dw : CKN.Foundation.Parabolic.Vec3 → Fin 3 → CKN.Foundation.Parabolic.Vec3)
:
The slice facts used in the trilinear identities.
- mem2 : MeasureTheory.MemLp w 2 MeasureTheory.volume
- grad2 : MeasureTheory.MemLp Dw 2 MeasureTheory.volume
- grad (i : Fin 3) : CKN.HasWeakGradientOn Set.univ (fun (x : CKN.Vec 3) => w x i) fun (x : CKN.Vec 3) => Dw x i
- trace : ∀ᵐ (x : CKN.Foundation.Parabolic.Vec3), ∑ j : Fin 3, Dw x j j = 0
Instances For
theorem
ESS.serrin_slice_self_transport
{u : CKN.Foundation.Parabolic.Vec3 → CKN.Foundation.Parabolic.Vec3}
{Du : CKN.Foundation.Parabolic.Vec3 → Fin 3 → CKN.Foundation.Parabolic.Vec3}
(hu : SerrinSlice u Du)
(hu5 : MeasureTheory.MemLp u (ENNReal.ofReal 5) MeasureTheory.volume)
:
The self-transport form of an L⁵ slice vanishes.
theorem
ESS.serrin_slice_relative
{u v : CKN.Foundation.Parabolic.Vec3 → CKN.Foundation.Parabolic.Vec3}
{Du Dv : CKN.Foundation.Parabolic.Vec3 → Fin 3 → CKN.Foundation.Parabolic.Vec3}
(hu : SerrinSlice u Du)
(hu5 : MeasureTheory.MemLp u (ENNReal.ofReal 5) MeasureTheory.volume)
(hv : SerrinSlice v Dv)
(hv103 : MeasureTheory.MemLp v (ENNReal.ofReal (10 / 3)) MeasureTheory.volume)
:
The sum of the two convection pairings minus the relative convection form integrates to zero.