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LeanPool.CIVAxisymmetric.Reduction.AveragedClassical

Rotation covariance and the averaged classical solution (sec:reduction:core) #

The forced Navier–Stokes system eq:nse:forced is covariant under the rigid rotations Q_φ of CIV.rotZ: if (u, p, f) is a classical solution on the unit cylinder then so is the rotated triple (ℛ_φ u, p ∘ Q_φ⁻¹, ℛ_φ f) (isClassicalSolutionOn_rotField). Design note R8 records the reduction this feeds: since an axisymmetric u is fixed by every ℛ_φ, averaging the rotated triples in φ over [0, 2π] replaces (u, p, f) by (u, 𝒫p, 𝒫f), again a classical solution (isClassicalSolutionOn_angularMean), with an axisymmetric, C²-bounded force when the original force was C²-bounded (forceC2Bounded_angularMean).

The derivative of the rotated field #

The derivative of rotField with respect to the space variable.

rotField at a fixed angle is C¹ on the unit cylinder whenever u is.

The spatial partial derivative of a scalar field composed with a rotation of the point is the corresponding partial derivative of the field at the rotated point, in the rotated direction. Unconditional: no regularity hypothesis on g is needed.

The time derivative of the rotated field #

The spatial derivatives of the rotated field #

A spatial partial derivative of rotField, component 0.

A spatial partial derivative of rotField, component 1.

The Laplacian of a rotated scalar field #

Differentiability, at a general fixed direction w (not necessarily a basis vector), of the once-differentiated slice of a C² field.

The second directional derivative of a C² scalar field, in directions v (outer) and w (inner). Diagonal values at basis vectors recover spatialSecondPartial (hessAt_eq_spatialSecondPartial).

Equations
Instances For
    theorem CIV.hessAt_add_left (g : CKN.Foundation.Parabolic.ParabolicPoint → ℝ) (t : ℝ) (x v1 v2 w : CKN.Foundation.Parabolic.Vec3) :
    hessAt g t x (v1 + v2) w = hessAt g t x v1 w + hessAt g t x v2 w

    The Laplacian (sum of second Cartesian partial derivatives) of a C² scalar field composed with a rotation of the point is the Laplacian of the field at the rotated point: the trace of the Hessian is invariant under the orthogonal map rotZ.

    ContDiffOn of a component of u composed with a rotation of the point.

    The convective and divergence terms of the rotated system #

    Rotation covariance of the Navier–Stokes equations #

    The Navier–Stokes equations are covariant under rigid rotations of the spatial coordinates (sec:reduction:core, design note R8). For any angle φ, if (u, p, f) solves the forced Navier–Stokes equations on the unit cylinder, then the rotated triple (ℛ_φ u, p ∘ Q_φ⁻¹, ℛ_φ f) also solves them.

    The averaged classical solution #

    The angular mean of a C^n scalar field on the unit cylinder is C^n there.

    For a C¹ scalar field, a spatial partial derivative of the angular mean is the angular mean of the corresponding spatial partial derivatives of the rotated fields: the derivative passes under the angular integral.

    A component of the angular mean of a C^∞ vector field is the angular mean of the corresponding component of the rotated fields.

    Pointwise agreement of two scalar fields on the unit cylinder transports a spatial partial derivative.

    The angular mean of a classical solution with axisymmetric velocity is again a classical solution, with pressure and force replaced by their angular means (sec:reduction:core, design note R8). Since the velocity is fixed by every rotation, only the pressure and force terms of the momentum equation change under averaging; the momentum and divergence equations themselves are linear in (p, f) with u fixed, so they survive averaging over φ.

    Corollaries #