StoppedMomentsDatum #
Ported from scottnarmstrong/Superdiffusion at 7f20476385d4af418f110303085ad0740c9eba46. Module imports, support namespace and local option directives adapted for Lean Pool.
The linear and quadratic observables of the displacement bounds #
The two Dirichlet problems behind Steps 1 and 3 of the superdiffusive displacement bounds are
posed on the origin cube openCubeSet (originCube d m) with the boundary data
ell_e (x) = e ⬝ x , quad_e (x) = (e ⬝ x)^2 ,
and, for the second one, the right-hand side -2 sigma, written as the divergence of the
field g(x) = -2 sigma (e ⬝ x) e. The homogenized solutions are the data themselves: ell_e
is harmonic, and quad_e satisfies -sigma * Laplacian quad_e = -2 sigma (e ⬝ e), which is
exactly the divergence of g.
This file records the calculus these two data need in order to be fed to the renormalization of the generator, and reads its conclusion at each of them.
- Gradients:
ell_ehas the constant gradiente, andquad_ehas the gradient2 (e ⬝ x) e. - Hölder data: a field of the form
x ↦ (c (e ⬝ x)) ehas1/2-Hölder seminorm at most|c| ‖e‖ (sum of |e_i|) 3^{m/2}on a cube of side3^m, and is bounded there by|c| ‖e‖ (sum of |e_i|) 3^m / 2. The constant gradientehas vanishing seminorm and is bounded by‖e‖. - Homogenized solutions: the two data solve the constant-coefficient problems with the stated forcings. For the linear datum this is one integration by parts against a zero-trace test function; for the quadratic datum the two sides of the weak equation agree pointwise.
Reading the renormalization estimate at these data then gives, on the cube of side 3^m,
|u - ell_e| <= 3^m * EB * ‖e‖ ,
|u - quad_e| <= (3^m)^2 * 5 * EB * ‖e‖ * (sum of |e_i|) ,
almost everywhere, the two displays e.u.minus.v.mean and e.u.minus.v.second of the source.
The effective diffusivity cancels in the second: the field g carries the factor 2 sigma
and the estimate divides by sigma.
Main definitions #
affineObservable,affineGradient—e ⬝ xand its gradient.quadraticObservable,quadraticGradient—(e ⬝ x)^2and its gradient.quadraticForcing— the field-2 sigma (e ⬝ x) e.vecCoordSum— the sum of the absolute values of the coordinates.
Main results #
hasGradientOn_affineObservable,hasGradientOn_quadraticObservable.holderSeminormBoundOn_affineGradient,holderSeminormBoundOn_smulAffineField.isDirichletSolutionOn_homogenized_affine,isDirichletSolutionOn_homogenized_quadratic.ae_abs_sub_affineObservable_le,ae_abs_sub_quadraticObservable_le.
References #
- ABK26, Steps 1 and 3 of the superdiffusive displacement bounds of Section 5.4.
1. The observables #
The linear observable x ↦ e ⬝ x.
Equations
Instances For
The gradient of the linear observable: the constant field e.
Equations
Instances For
The quadratic observable x ↦ (e ⬝ x)^2.
Equations
Instances For
The gradient of the quadratic observable: x ↦ 2 (e ⬝ x) e.
Equations
- Algsuperdiff.Section5.Provider.quadraticGradient e x = (2 * HCPolySupport.vecDot e x) • e
Instances For
The field whose divergence is the constant right-hand side of the quadratic problem:
g(x) = -2 sigma (e ⬝ x) e.
Equations
- Algsuperdiff.Section5.Provider.quadraticForcing sigma e x = (-(2 * sigma) * HCPolySupport.vecDot e x) • e
Instances For
The pairing against a fixed vector is bounded by the coordinate sum times the supremum norm.
2. The gradients #
The gradient of the linear observable.
The gradient of the quadratic observable.
3. The geometry of the origin cube #
The supremum norm on the origin cube of scale m is below half the side length.
The diameter of the origin cube of scale m in the supremum norm.
4. The Hölder data #
The constant gradient has vanishing Hölder seminorm.
The vanishing field has vanishing Hölder seminorm.
The Hölder seminorm of a field proportional to (e ⬝ x) e on the origin cube.
The uniform bound for a field proportional to (e ⬝ x) e on the origin cube.
5. The homogenized solutions #
The linear observable solves the homogenized problem with vanishing forcing. The constant-coefficient equation for a constant gradient tests to zero against any zero-trace function, by one integration by parts.
The quadratic observable solves the homogenized problem with the stated forcing. Here the two sides of the weak equation agree pointwise: the forcing field is exactly minus the effective diffusivity times the gradient of the observable.
6. Reading the renormalization estimate at the two data #
The renormalization estimate at the linear datum. With vanishing forcing, vanishing
Hölder seminorm of the constant gradient, and the uniform gradient bound ‖e‖, the estimate
reads |u - ell_e| <= 3^m EB ‖e‖.
The renormalization estimate at the quadratic datum. The effective diffusivity
cancels: the forcing field carries the factor 2 sigma and the estimate divides by sigma.
The estimate reads |u - quad_e| <= 5 (3^m)^2 EB ‖e‖ (sum of |e_i|).