Physical power-coordinate pullback of the weighted radial inverse #
The power coordinate is U = R^d on a fixed positive annulus. Smooth positive
regularizations below the annulus make every source and output a genuine
globally defined smooth function. They agree with the prescribed power maps
where the source or the output can be nonzero.
Uniform flat-weight estimates for radial primitives #
The initial coordinate is additive distance from the left endpoint of a fixed
interval (0,L). The constants in the estimates are independent of the point
approaching either endpoint and of any auxiliary shifts in the source.
Zeta, given by edge cL x * edge cR (L - x).
Equations
- NavierStokes.WeightedRadialPrimitive.zeta cL cR L x = NavierStokes.FlatCutoff.edge cL x * NavierStokes.FlatCutoff.edge cR (L - x)
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Weight, given by zeta cL cR L x / delta L x ^ m.
Equations
- NavierStokes.WeightedRadialPrimitive.weight cL cR L m x = NavierStokes.WeightedRadialPrimitive.zeta cL cR L x / NavierStokes.WeightedRadialPrimitive.delta L x ^ m
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Single-edge monotonicity is proved from the exponential formula.
Compactness of the actual transformed improper integral gives one constant for the primitive, uniformly down to the flat endpoint.
Whole majorant, given by `singleWeight cL 0 x + singleWeight cL m x + (singleWeight cR 0 (L
- x) + singleWeight cR m (L - x))`.
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The left inverse estimate is uniform at the endpoint, with no loss of the polynomial edge exponent. It applies to arbitrary Banach-valued sources.
Reflection gives the corresponding endpoint-uniform right inverse bound.
Uniform total and partial mass bounds on the finite shell. Endpoint values of the source are immaterial to this Lebesgue-integral statement.
Compact primitive, given by intervalIntegral f 0 x volume - χ x • intervalIntegral f 0 L volume.
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The actual compactified primitive preserves the same two-edge weighted envelope. The cutoff is only required to have two plateaus and remain bounded; no monotonicity of the weight or inverse estimate is assumed.
Pullback to logarithmic edge distances on a fixed positive annulus #
Exp pullback, given by expCoordinate a s • f (expCoordinate a s).
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Actual change of variables, including the radial integration Jacobian.
Left logarithmic-edge estimate in the original positive radial variable. The extra constant is only the fixed upper radial endpoint b.
Right logarithmic-edge estimate in the original positive radial variable.
The entire weighted source has uniformly bounded mass on the positive annulus. This also bounds every interior subinterval.
Log compact primitive, given by intervalIntegral f a X volume - χ (logPosition a X) • intervalIntegral f a b volume.
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The compactified primitive preserves the explicit logarithmic two-edge weight uniformly on the whole positive annulus.
Physical cutoffs and auxiliary shifts #
Radial compact primitive, given by intervalIntegral f a X volume - χ X • intervalIntegral f a b volume.
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Any fixed pair of interior physical plateau thresholds gives positive logarithmic collars. This derives the collars from the endpoints.
The cutoff can be specified directly in the physical radial coordinate. No logarithmic cutoff regularity or assumed inverse bound is required.
A source slice along the actual affine shifted radial characteristic.
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Auxiliary translation does not change a radial bound that is uniform in the auxiliary variable. Constants are independent of M, v, and the base point.
The actual transport operator #
A uniform weighted inverse bound for the manuscript's actual shifted, compactified transport primitive. All shifts are quantified after the constant.
The cutoff itself is the explicit smooth transition constructed in
TransportPrimitive; there is no cutoff-existence hypothesis.
The uncorrected past primitive obeys the left weighted estimate uniformly in every auxiliary shift.
The future primitive obeys the right weighted estimate.
A common bound for past and total mass, uniform in every shift and in the point in the annulus. It is used only on a compact interior collar.
A smooth scalar radial cutoff has bounded actual Fréchet jets on the entire strip, including its unbounded auxiliary directions.
On an open left logarithmic collar, every actual derivative of the compactified operator equals the corresponding derivative of the past integral.
On an open right logarithmic collar the compactified operator equals the negative future integral, including all its actual derivatives.
Every finite prefix of actual Fréchet derivatives of the compactified transport inverse preserves the same flat radial envelope. The estimate is uniform in the shift and in all auxiliary variables.
The manuscript's all-jet mean class on a concrete annulus #
A concrete StripData: the radial domain and both weights are explicit;
the only inputs beyond the annulus are the positive band scales.
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On the concrete strip, the library majorant is exactly a band amplitude times the explicit logarithmic radial weight.
The concrete compactified shifted inverse preserves the all-jet mean
class M_α on the explicit logarithmic annulus. Both radial support and global
smoothness of the input are named hypotheses; neither the inverse estimate nor
smoothness of the output is assumed. The bandwise shifts may be arbitrary.
The full supported-mean conclusion includes global smoothness and the original radial support, as required by the smooth zero-extension convention.
A globally smooth positive radius, identical to the radius above 2ℓ.
Equations
- NavierStokes.RadialPullback.positiveRadius ℓ x = ℓ + (x - ℓ) * ((x - ℓ) / ℓ).smoothTransition
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Inverse chart, given by (positiveRadius (a ^ d / 4) U) ^ d⁻¹.
Equations
- NavierStokes.RadialPullback.inverseChart d a U = NavierStokes.RadialPullback.positiveRadius (a ^ d / 4) U ^ d⁻¹
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Normalize source, given by sourceMultiplier d a z.1 • g (liftChart (inverseChart d a) z).
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Physical graph derivative, given by fderiv ℝ F z (1, (radialJacobian d z.1 * M) • v).
Equations
- NavierStokes.RadialPullback.physicalGraphDeriv d M v F z = (fderiv ℝ F z) (1, (NavierStokes.RadialPullback.radialJacobian d z.1 * M) • v)
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The physical radial graph derivative is the transformed transport derivative multiplied by the actual power-coordinate Jacobian.
Pure auxiliary derivatives are unchanged by the radial coordinate map.
The positive power substitution includes the actual radial Jacobian.
After source normalization, the Jacobian cancels exactly, including the auxiliary shift in the transformed coordinate.
The total transformed integral has exactly the original physical radial measure. In particular no Jacobian remains when taking a torus mean later.
Physical compact, given by pullback d a (TransportPrimitive.compactIntegral (TransportPrimitive.interiorCutoff (a ^ d) (b ^ d)) M v (normalizeSource d a g)).
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The pulled-back operator is the physical shifted radial integral, with the original source g and no uncancelled Jacobian.
Physical alias as an element of V.
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Physical cutoff, given by TransportPrimitive.interiorCutoff (a ^ d) (b ^ d) (powerChart d a R).
Equations
- NavierStokes.RadialPullback.physicalCutoff d a b R = NavierStokes.TransportPrimitive.interiorCutoff (a ^ d) (b ^ d) (NavierStokes.RadialPullback.powerChart d a R)
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Exact inverse identity in the physical radial graph coordinate, including the compactification alias and the source normalization.
Global physical inverse identity. Below the positive annulus, the source, the output derivative, and the alias all vanish by their proved support.
Exact exponential weight and controlled inverse-edge powers #
Uniform genuine finite jets under fixed radial maps #
Positive-order derivatives of a radial coordinate change are independent of the auxiliary base point. This follows from translation identities.
A fixed radial coordinate map has a finite-order composition constant, uniform on the full auxiliary strip, for actual multilinear derivative norms.
Multiplication by a fixed smooth radial coefficient has a finite-order constant, with all product-rule terms retained.
Weighted source normalization #
The complete physical inverse preserves the original exponential weight and the same finite inverse-edge degree. All constants precede the arbitrary transport shift, source, amplitude, and evaluation point.
The physical/chart inverse maps the concrete all-jet mean class to itself. The input and output weights are exactly the same logarithmic exponential.