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LeanPool.ViscositySolutionTheory.AleksandrovDifferentiability.Analysis.Directional.LineScalar

Ported for Lean Pool: imports relocated and code adapted to Lean/Mathlib v4.34.0.

Scalar estimates along affine lines #

This file records zero-direction cases and transport wrappers for scalar quadratic estimates on line restrictions.

Every point is good for the zero-direction scalar estimate set.

Every point is good for the zero-direction scalar quotient-estimate set.

Affine ambient functions have scalar line-estimate data in every direction and at every base point.

Affine ambient functions have scalar line-estimate data with the ambient slope projected onto the line direction and zero quadratic coefficient.

For affine ambient functions, every point is good for every scalar directional-line estimate.

theorem AleksandrovDifferentiability.compatibleDirectionalSliceEstimateAt_inner_add_const {E : Type u_1} [NormedAddCommGroup E] [InnerProductSpace ℝ E] {ι : Type u_2} (D : Finset ι) (v : ι → E) (p : E) (c : ℝ) (x : E) :
CompatibleDirectionalSliceEstimateAt D v (fun (y : E) => inner ℝ p y + c) x

Affine ambient functions carry compatible finite slice data for every finite direction list. The compatible ambient slope is the affine slope and all quadratic coefficients are zero.

Symmetric compatible finite slice data for affine ambient functions.

For affine ambient functions, every point carries compatible finite slice data.

For affine ambient functions, every point carries symmetric compatible finite slice data.

Nonzero scalar rescaling of a direction does not change the scalar directional-line good set.

The fixed-direction scalar estimate good set is contained in its punctured normalized quotient version.

On ℝ, scalar quadratic estimate data at a point gives scalar estimate data on the restriction to any real affine line through that point.

A scalar estimate for the unit real-line restriction through x is exactly a scalar estimate at x.

On the real line, scalar quadratic estimate data at a point supplies compatible finite slice data for any finite family of real directions: every line slope is obtained from the same ambient scalar first-order coefficient.

On the real line, the ordinary scalar-estimate good set is contained in every directional line scalar-estimate good set.

Normalizing a nonzero direction by the inverse of its norm gives a unit direction.