Chapter 3 solution and estimate vocabulary #
Solution carriers and estimate right-hand sides for the pinned CoarseGraining
development. The coefficient, Besov and cube geometry primitives are separated
into DomainGeometry so clients can import that foundation independently.
Normalized integral over an arbitrary measurable set, written as a total quantity so theorem statements do not need side hypotheses merely to parse.
Equations
Instances For
Normalized L² square over a set.
Equations
- HCPolySupport.Book.Ch03.normalizedL2SqOnSet V u = HCPolySupport.Book.Ch03.normalizedSetAverage V fun (x : HCPolySupport.Vec d) => u x ^ 2
Instances For
Localized coefficient energy for an H¹ function, using the symmetric part
of the public coefficient representative.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The global coefficient-energy norm of a Chapter 2 solution on a cube.
Equations
Instances For
Weak public formulation of - div(a grad u) = div g on a cube, in the
codebase's RHS sign convention.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Forced cube solution for the public Chapter 3.2 estimates.
- toH1 : H1Function (Ch02.cubeDomain Q).carrier
The Sobolev function satisfying the forced weak equation on the cube.
- weakSolution : IsForcedEquation Q a self.toH1 g
Instances For
Zero-trace forced solution used by the auxiliary Dirichlet estimate.
- toH10 : H10Function (Ch02.cubeDomain Q).carrier
The zero-trace Sobolev function satisfying the forced weak equation on the cube.
- weakSolution : IsForcedEquation Q a self.toH10.toH1Function g
Instances For
Boundary-patch forced solution for the RHS Caccioppoli estimate.
- toH1 : H1Function (Ch02.cubeDomain Q).carrier
The forced Sobolev solution whose trace vanishes on the specified boundary patch.
- weakSolution : IsForcedEquation Q a self.toH1 g
- zeroTraceOnBoundaryPatch : Ch01.LocalizedZeroTraceFunctionOn (Ch02.cubeDomain Q).carrier (openCubeAtScale x (Q.scale - 1)) self.toH1.toFun
Instances For
Dirichlet forced solution with boundary datum h, formalizing
v - h ∈ H¹₀(Q).
- toH1 : H1Function (Ch02.cubeDomain Q).carrier
The Sobolev solution of the forced Dirichlet problem on the cube.
- boundaryData : H1Function (Ch02.cubeDomain Q).carrier
Sobolev boundary datum whose difference from the solution has zero trace.
- weakSolution : IsForcedEquation Q a self.toH1 g
- zeroTraceDifference : ∃ (w : H10Function (Ch02.cubeDomain Q).carrier), w.toFun =ᵐ[volumeMeasureOn (Ch02.cubeDomain Q).carrier] fun (x : Vec d) => self.toH1.toFun x - self.boundaryData.toFun x
Instances For
Mean-zero Neumann weak formulation for the public energy consequence.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Mean-zero Neumann solution of the forced problem on a cube.
The forcing is centered, matching the variational Neumann statement in the notes. The sign follows the codebase's RHS convention.
- toH1MeanZero : H1MeanZeroFunction (Ch02.cubeDomain Q).carrier
The mean-zero Sobolev solution tested against mean-zero functions with centered forcing.
- weakSolution : IsMeanZeroNeumannForcedEquation Q a self.toH1MeanZero fun (x : Vec d) => g x - cubeAverageVec Q g
Instances For
Coefficient-energy norm of an arbitrary public H¹ function on a cube.
Equations
Instances For
Energy norm of a forced cube solution.
Equations
Instances For
Energy norm of a zero-trace forced solution.
Equations
Instances For
Energy norm of boundary-patch forced Caccioppoli data.
Equations
Instances For
Parent-cube L² size of boundary-patch forced Caccioppoli data.
Equations
Instances For
Energy norm of a Dirichlet forced solution.
Equations
Instances For
Gradient of the boundary datum in a Dirichlet forced solution.
Instances For
Energy norm of a mean-zero Neumann forced solution.
Equations
Instances For
Gradient field of a cube solution.
Equations
Instances For
Gradient field of a forced cube solution.
Equations
Instances For
Flux field a ∇u of a cube solution.
Equations
- HCPolySupport.Book.Ch03.solutionFluxField Q a u x = HCPolySupport.matVecMul ((a.coeffOn Q).toCoeffField x) (u.toH1.grad x)
Instances For
Flux field a ∇u of a forced cube solution.
Equations
- HCPolySupport.Book.Ch03.forcedSolutionFluxField Q a u x = HCPolySupport.matVecMul ((a.coeffOn Q).toCoeffField x) (u.toH1.grad x)
Instances For
A constant symmetric uniformly elliptic comparison matrix.
- matrix : Mat d
The symmetric elliptic matrix used to compare the variable-coefficient flux.
- isSymm : Matrix.IsSymm self.matrix
- lam : ℝ
The positive lower ellipticity bound for the comparison matrix.
- Lam : ℝ
The upper ellipticity bound for the comparison matrix.
- elliptic : IsEllipticMatrix self.lam self.Lam self.matrix
Instances For
The factor |a0|^{1/2} in the flux-response estimate.
Equations
Instances For
The factor |a0| in the inhomogeneous flux-response estimate.
Equations
Instances For
Flux defect (a - a0)∇u against a constant comparison matrix.
Equations
- HCPolySupport.Book.Ch03.solutionFluxDefectField Q a a0 u x = HCPolySupport.matVecMul ((a.coeffOn Q).toCoeffField x - a0.matrix) (u.toH1.grad x)
Instances For
Flux defect (a - a0)∇u for a forced solution.
Equations
- HCPolySupport.Book.Ch03.forcedSolutionFluxDefectField Q a a0 u x = HCPolySupport.matVecMul ((a.coeffOn Q).toCoeffField x - a0.matrix) (u.toH1.grad x)
Instances For
Constant-coefficient weak formulation of - div(a0 grad u) = div g on a
cube, in the codebase's RHS sign convention.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Constant-coefficient part a0(∇u - ∇v) in the homogenization comparison.
Equations
- HCPolySupport.Book.Ch03.homogenizationComparisonConstantGradientField a0 u v x = HCPolySupport.matVecMul a0.matrix (u.grad x - v.grad x)
Instances For
Flux difference a∇u - a0∇v in the homogenization comparison.
Equations
- HCPolySupport.Book.Ch03.homogenizationComparisonFluxField Q a a0 u v x = HCPolySupport.matVecMul ((a.coeffOn Q).toCoeffField x) (u.grad x) - HCPolySupport.matVecMul a0.matrix (v.grad x)
Instances For
Local flux defect (a - a0)G, using the coefficient representative on the
cube where the norm is evaluated.
Equations
- HCPolySupport.Book.Ch03.homogenizationComparisonFluxDefectFromGradient Q a a0 G x = HCPolySupport.matVecMul ((a.coeffOn Q).toCoeffField x - a0.matrix) (G x)
Instances For
Local flux defect (a - a0)∇u on a cube.
Equations
Instances For
Data for the duality lemma: a pair satisfying
div(a∇u - a0∇v) = 0 and u - v ∈ H¹₀(Q).
- u : H1Function (Ch02.cubeDomain Q).carrier
The Sobolev function contributing the variable-coefficient flux to the duality comparison.
- v : H1Function (Ch02.cubeDomain Q).carrier
The Sobolev comparison function contributing the constant-coefficient flux and sharing the trace of
u. - fluxComparisonSolenoidal : IsSolenoidalOn (Ch02.cubeDomain Q).carrier (homogenizationComparisonFluxField Q a a0 self.u self.v)
- zeroTraceDifference : ∃ (w : H10Function (Ch02.cubeDomain Q).carrier), w.toFun =ᵐ[volumeMeasureOn (Ch02.cubeDomain Q).carrier] fun (x : Vec d) => self.u.toFun x - self.v.toFun x
Instances For
Data for the general coarse-graining theorem: two solutions with the same right-hand side and zero-trace difference.
- u : H1Function (Ch02.cubeDomain Q).carrier
The variable-coefficient solution with forcing
gin the coarse-graining comparison. - v : H1Function (Ch02.cubeDomain Q).carrier
The constant-coefficient solution with forcing
gand the same trace asu. - uWeakSolution : IsForcedEquation Q a self.u g
- vWeakSolution : IsConstantCoeffForcedEquation Q a0 self.v g
- zeroTraceDifference : ∃ (w : H10Function (Ch02.cubeDomain Q).carrier), w.toFun =ᵐ[volumeMeasureOn (Ch02.cubeDomain Q).carrier] fun (x : Vec d) => self.u.toFun x - self.v.toFun x
Instances For
Left-hand side in the Section 3.3 comparison estimates, using the concrete/circ negative Besov seminorm from the deterministic splitting arguments.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Localized ℓ² average of the concrete/circ flux-defect negative Besov
seminorms over descendants at depth j = m - n. If the parent cube has scale
m = Q.scale, then the manuscript lower scale is n = Q.scale - (j : ℤ),
which may be negative.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Public localized boundary data for the boundary Caccioppoli theorem.
The zero-trace condition is scalar and localized: every smooth cutoff supported
in the boundary window x + cu_{m-1} turns u into an admissible H¹₀ test
function on the parent cube. This is the Lean form of the note's Sobolev trace
condition u = 0 on (∂cu_m) ∩ (x + cu_{m-1}); it deliberately does not use a
gradient-only potential condition, since gradients cannot see constants.
- toH1 : H1Function (Ch02.cubeDomain Q).carrier
The Sobolev function with an a-harmonic gradient and zero trace on the boundary patch.
- isHarmonic : IsAHarmonicGradient (a.coeffOn Q).toCoeffField (Ch02.cubeDomain Q).carrier self.toH1.grad
- zeroTraceOnBoundaryPatch : Ch01.LocalizedZeroTraceFunctionOn (Ch02.cubeDomain Q).carrier (openCubeAtScale x (Q.scale - 1)) self.toH1.toFun
Instances For
Localized energy of boundary Caccioppoli data on the core patch.
Equations
Instances For
Parent-cube L² size for boundary Caccioppoli data.
Equations
Instances For
Localized energy of an interior solution on the core patch.
Equations
Instances For
Parent-cube oscillation L² square for the interior Caccioppoli estimate.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The Caccioppoli prefactor in
e.coarse.grained.Caccioppoli.*.deterministic.theory, excluding the final
L² square.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Boundary Caccioppoli right-hand side.
Equations
Instances For
Interior Caccioppoli right-hand side.
Equations
Instances For
The factor c_{s,q}^{-1/q}, with value 1 at q = infinity.
Equations
Instances For
The lower-ellipticity factor \lambda_{s,q}^{-1/2}.
Equations
- HCPolySupport.Book.Ch03.poincareLowerEllipticityFactor Q a s q = (HCPolySupport.Book.Ch02.lambdaSq Q s q a).rpow (-(1 / 2))
Instances For
The upper-ellipticity factor \Lambda_{s,q}^{1/2}.
Equations
- HCPolySupport.Book.Ch03.poincareUpperEllipticityFactor Q a s q = (HCPolySupport.Book.Ch02.LambdaSq Q s q a).rpow (1 / 2)
Instances For
Right-hand side in the gradient coarse Poincare estimate.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the flux coarse Poincare estimate.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the coarse flux-response estimate.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the coarse Poincare estimate with forcing.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the auxiliary zero-Dirichlet energy estimate.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Common prefactor in the boundary Caccioppoli estimate with forcing.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Boundary Caccioppoli right-hand side with forcing.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the weak flux estimate with forcing.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the coarse flux-response estimate with forcing.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the Dirichlet energy estimate with forcing and boundary data.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the mean-zero Neumann energy estimate with forcing.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Truncated homogenization error
\mathcal E_{s,\infty,1}(Q,n; a, a0), encoded by descendant depth
j = m - n. Equivalently, the manuscript scale is
n = Q.scale - (j : ℤ), so negative n are represented by sufficiently large
natural depths j.
This is the Ch3.3 localized envelope: the supremum of the Ch2 one-cube
homogenization error over the depth-j descendants of the parent cube.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Right-hand side in the duality estimate from local flux defect to global comparison.
Equations
- HCPolySupport.Book.Ch03.dualityFromFluxDefectRHS C Q a a0 s j u = C * s⁻¹ * HCPolySupport.Book.Ch03.localizedHomogenizationFluxDefectAverage Q a a0 s j u
Instances For
Note-facing two-exponent replacement RHS for the duality estimate.
The comparison field is measured at exponent s, while the localized
flux-defect average is measured at the independent lower exponent t.
The scalar prefactor is the displayed manuscript loss
s^{-1} t^{-2} (1/2 - t)^{-1}.
Equations
Instances For
The depth factor 3^{s(m-n)/2} in the Section 3.3 coarse-graining bound.
Equations
- HCPolySupport.Book.Ch03.coarseGrainingDepthHalfWeight s j = Real.rpow 3 (s / 2 * ↑j)
Instances For
The depth factor 3^{s(m-n)} in the Section 3.3 coarse-graining bound.
Equations
- HCPolySupport.Book.Ch03.coarseGrainingDepthWeight s j = Real.rpow 3 (s * ↑j)
Instances For
The inverse depth factor 3^{-s(m-n)} used by scale-separated forcing.
Equations
Instances For
Scale-separated local flux-defect RHS in the repaired general
coarse-graining estimate. The flux-response quantities are measured at
exponent r, while the force is measured at the stronger exponent r₂.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Note-facing RHS with an independent stronger force exponent r₂. The
comparison is measured at exponent s, the flux response at r, and the
forcing at r₂.
Equations
- One or more equations did not get rendered due to their size.