Coarse-graining support: Support.Book.Ch03.Theorems.PublicInternalBridges.H1Transport #
Imported from the Apache-2.0 CoarseGraining development at commit
c7ddd76c08ade64fed1b8d2ca51be14dfee8deb4.
Public H1 transport bridges for Chapter 3 #
This file transports public H1, H10, mean-zero, and zero-trace data to the deterministic half-open cube setting used by Chapter 3 engines.
View a public open-domain H¹ function as an H¹ function on the
half-open triadic cube used by the deterministic layer.
Equations
Instances For
Promote a mean-zero H¹ witness on an open triadic cube to the
corresponding half-open cube.
Equations
- HCPolySupport.Book.Ch03.H1MeanZeroFunction.toCubeSet u = { toH1Function := u.toH1Function.toCubeSet, meanZero := ⋯ }
Instances For
Restrict a mean-zero H¹ witness on a half-open triadic cube to its open
realization.
Equations
- HCPolySupport.Book.Ch03.H1MeanZeroFunction.toOpenCubeSet u = { toH1Function := u.toH1Function.toOpenCubeSet, meanZero := ⋯ }
Instances For
View a public open-domain mean-zero H¹ function as a mean-zero H¹
function on the half-open triadic cube used by the deterministic layer.
Equations
Instances For
View a public open-domain H¹₀ function as an H¹₀ function on the
half-open triadic cube used by the deterministic layer.
Equations
Instances For
Chosen public zero-trace representative for the Dirichlet boundary
condition v - h ∈ H¹₀(Q).
Equations
Instances For
The chosen public zero-trace representative, transported to the deterministic half-open cube.
Equations
Instances For
Zero-trace public test functions provide the deterministic zero-trace-potential predicate on the corresponding half-open cube.
Weak partial derivatives are unique even when the underlying scalar representatives agree only a.e. on the open domain.
On an open domain, two H¹ representatives with a.e.-equal values have
a.e.-equal weak gradients.
Coefficient-energy split for a public Dirichlet solution:
∇v = ∇(v - h) + ∇h on the deterministic cube, with the zero-trace
representative chosen from the public boundary condition.
The public value-level zero-trace difference u - v ∈ H¹₀ supplies the
deterministic zero-trace-potential predicate for the gradient difference.