Coarse-graining support: Support.Sobolev.Foundations.CubeNeumannW22CZ.WeakInteriorDQ.SqCutoffH10 #
Imported from the Apache-2.0 CoarseGraining development at commit
c7ddd76c08ade64fed1b8d2ca51be14dfee8deb4.
The squared-cutoff forward difference quotient η² D_i^+ u is an ambient
zero-trace test when the cutoff is supported in a shift-safe interior set.
The squared-cutoff forward quotient is genuinely supported in the ambient domain when the cutoff support lies in an interior subset.
Chosen ambient H¹₀(U) representative of η² D_i^+ u.
Equations
- HCPolySupport.WeakPoissonEquationOn.sqCutoffForwardDifferenceQuotientToH10 u hV hVU step i hVshift hη hη_compact hη_sub = Classical.choose ⋯
Instances For
Coordinatewise gradient identification between the chosen ambient
H¹₀(U) representative of η²D_i^+u and the explicit ambient H¹
localized product representative.
Vector-valued gradient identification for the chosen ambient H¹₀(U)
representative of η²D_i^+u.
The whole-space backward quotient bound specialized to the squared-cutoff forward difference quotient test.
The squared-cutoff direct test is controlled by the explicit product-rule
gradient of η²D_i^+u.
The shifted factor η(x-h e_i)² D_i^- u(x) is an ambient zero-trace
test. It is the translated companion to
memH10_sqCutoffForwardDifferenceQuotient, with the backward quotient living
on the translated interior set V + h e_i.
Ambient H¹ representative of the shifted term
η(x-h e_i)² D_i^- u(x), localized on the translated interior set
V + h e_i.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Pairing against the shifted localized gradient is supported in the translated interior set.
Transport the shifted localized-gradient pairing from U back to the
interior set V.
Explicit ambient H¹ representative of the direct test
D_i^-(η² D_i^+u).
Equations
- One or more equations did not get rendered due to their size.
Instances For
The direct difference-quotient test D_i^-(η²D_i^+u) is genuinely
supported in the ambient domain.
The direct weak-equation test D_i^- (η² D_i^+ u) is ambient zero-trace.
This is the key admissibility bridge for the direct difference-quotient
energy estimate: the original weak equation can be tested against a difference
quotient of the cutoff-weighted forward quotient, so the forcing remains f
rather than D_i^+ f.
Chosen H¹₀(U) representative of the direct difference-quotient test
D_i^- (η² D_i^+ u).
Equations
- HCPolySupport.WeakPoissonEquationOn.backwardDifferenceQuotientSqCutoffForwardDifferenceQuotientToH10 u hV hVU step i hVshift hη hη_compact hη_sub = Classical.choose ⋯
Instances For
Coordinatewise gradient identification between the chosen H¹₀
representative of D_i^-(η² D_i^+u) and the explicit ambient H¹
representative built from localized shifted pieces.
Vector-valued gradient identification for the direct difference-quotient test.
Integral-square form of the specialized direct-test quotient bound.
Original weak equation tested against the direct difference-quotient test.
The right-hand side contains the undifferentiated forcing f; the next stage
is to identify the left-hand side by finite-difference summation by parts.
Original weak equation tested against the direct difference-quotient test,
with the left-hand side rewritten using the explicit ambient H¹
representative of that test.