Terminal heat tails and backward stress #
All derivatives and integrals are actual analytic operations. The backward stress is defined independently of the separate global moment condition that identifies it with an axis-based stress primitive.
Radial-viscosity terms left after cancelling the heat equation for K.
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The exact backward integration-by-parts identity. Integrability and the vanishing boundary at infinity are explicit local-tail hypotheses.
The backward stress controls the positive radial boundary term.
A precise version of the time-integral lower comparison. The extra
coefficient comparison is distinct from mere monotonicity of K.
The heat carrier with the manuscript's arbitrary fixed normalization.
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- NavierStokes.TerminalStress.heatAmplitude C a t r = C * NavierStokes.RadialHeatProfile.radialProfile a (1 - t) r
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Product expansion of the actual heat equation. No formal jet variables occur.
Physical point: an abbreviation for SimilarityProfile.PhysicalPoint.
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Physical profile: an abbreviation for SimilarityProfile.PhysicalProfile.
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Radius point, given by (t, (r ^ 2 / 2, z)).
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Radial slice, given by G (radiusPoint t r z).
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- NavierStokes.TerminalStress.radialSlice G t z r = G (NavierStokes.TerminalStress.radiusPoint t r z)
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The actual cylindrical angular radial Laplacian of r F.
The displayed terminal angular residual, before axial viscosity, is an
identity of actual time and radial derivatives of K f_o.
The angular heat carrier expressed in the regular coordinate s.
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- NavierStokes.TerminalStress.physicalHeat C a p = C * NavierStokes.RadialHeatProfile.spatialProfile a (1 - p.1) p.2.1
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The regular Cartesian swirl coefficient: the physical angular velocity is r F.
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- NavierStokes.TerminalStress.swirlCoefficient C h f p = NavierStokes.TerminalStress.physicalHeat C (1 + h) p * NavierStokes.TerminalStress.flattening h f p / √(2 * p.2.1)
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Transfer from regular Cartesian swirl derivatives to the actual radial operator.
Leading residual, constructed using heatAmplitude.
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Canonical pressure, normalized at infinity, in the regular coordinate.
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The radial pressure balance is derived from the defining improper integral. Joint pressure differentiability is a separate analytic regularity hypothesis.
Residual coefficient, given by partialT F p - 2 * p.2.1 * partialS (partialS F) p - 4 * partialS F p - partialZ (partialZ F) p.
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The actual Cartesian residual of a purely angular velocity.
Exact axial viscosity retained in the terminal physical residual.
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Terminal velocity, given by AxisymmetricResidual.velocity (fun _ => 0) (swirlCoefficient C h f) (fun _ => 0).
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Terminal pressure, given by AxisymmetricResidual.pressure (canonicalPressure (swirlCoefficient C h f)).
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Full terminal residual, with canonical radial balance and the omitted axial-viscosity term displayed. The pressure's joint differentiability and the tail-integral hypotheses are explicit and do not impose a residual identity.
A backward stress solves the actual radial divergence equation without any hypothesis about its integral over the whole radius.
The missing global matching condition is exactly the zero total weighted residual. It is not part of the definition of either stress primitive.
Time denominator, given by SimilarityProfile.q h (t, (0, z)) * CoordinateAlgebra.L h (SimilarityProfile.eta h (t, (0, z))).
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Time residual, given by heatAmplitude C (1 + h) t r * deriv f (Real.log (SimilarityProfile.X h (radiusPoint t r z))) / timeDenominator h t z.
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The actual logarithmic time term is a positive weight times ∂r f_o.
On a finite remaining radius interval, positivity and decreasing K
give a concrete time-weight comparison for the mass lower bound.
Terminal stress, given by backwardStress (fun u => leadingResidual C h f t u z) r.
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- NavierStokes.TerminalStress.terminalStress C h f t z r = NavierStokes.TerminalStress.backwardStress (fun (u : ℝ) => NavierStokes.TerminalStress.leadingResidual C h f t u z) r
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Backward formula instantiated with the actual heat carrier and actual logarithmic flattening factor. The integrability and boundary conditions are ordinary conditions on these functions, not assumed stress identities.
A plateau at infinity automatically removes the radial boundary term, irrespective of the behavior of the heat carrier there.
In particular, the actual outgoing taper gives the zero boundary at infinity.
The actual terminal taper and its Gaussian edge #
Taper factor, given by (taperDenominator δ)⁻¹.
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The actual outgoing taper has the precise exp(-4/δ²) deficit.
Taper slope factor, given by d.rho * (8 * taperFactor δ + δ ^ 3 * deriv taperFactor δ).
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The actual taper derivative has a smooth positive limiting coefficient
after division by the edge factor exp(-4/δ²) δ⁻³.
The boundary term and actual backward integrals after the edge change of variables.
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- NavierStokes.TerminalStress.edgeStress c b a y = NavierStokes.FlatCutoff.edge c y.2 / y.2 ^ 3 * b y + NavierStokes.ParametricFlatFactor.primitive c 3 a y
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Normalized edge stress, given by b y + y.2 ^ 3 * ParametricFlatFactor.factor c 3 a y.
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- NavierStokes.TerminalStress.normalizedEdgeStress c b a y = b y + y.2 ^ 3 * NavierStokes.ParametricFlatFactor.factor c 3 a y