Actual natural profiles in the original radial variable #
This module reconstructs the unscaled natural profiles from the actual smooth solutions of the coefficient-space problem. Derivative identities refer to ordinary derivatives of the reconstructed real functions.
The actual fixed coefficients of the natural-axis problem #
The pressure comes from its proved holomorphic integral extension. A common complex neighborhood is chosen by compactness and nonvanishing of the two actual denominators. Every fixed field is then embedded in the same complete space of compatible coefficient functions.
The fixed real natural-axis data #
The small parameters are quantitative. The unique zero of H is proved,
not postulated. The pressure is an input with explicit real smoothness,
negativity, and derivative-sign hypotheses; its construction and complex
analytic estimates are separate results.
The pressure datum from a nonnegative weighted schedule #
The clock weights and bounded exponents are fixed input functions. Regularity of the pressure is deduced from the integral, not assumed as an input.
Sufficient hypotheses on the fixed clock data. No pressure derivatives occur here.
- integrable : MeasureTheory.Integrable g MeasureTheory.volume
- measurable : Measurable a
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Complex kernel, given by Complex.exp ((-2 * (a : ℂ)) * Complex.log (1 + z ^ 2)).
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- NavierStokes.PressureDatum.complexKernel a z = Complex.exp (-2 * ↑a * Complex.log (1 + z ^ 2))
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Complex kernel derivative, given by complexKernel a z * ((-2 * (a : ℂ)) * ((1 + z ^ 2)⁻¹ * (2 * z))).
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Compactness of the bounded exponent interval supplies the dominating constant.
Complex pressure, given by -(1 / 2 : ℂ) * ∫ y, (g y : ℂ) * complexKernel (a y) z.
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- NavierStokes.PressureDatum.complexPressure g a z = -(1 / 2) * ∫ (y : ℝ), ↑(g y) * NavierStokes.PressureDatum.complexKernel (a y) z
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Holomorphic extension is proved by dominated differentiation on the strip.
Smoothness follows from the proved complex extension, for every finite order at once.
An arbitrary measurable positive prefix contributes its exact constant-exponent mass.
L, given by 1 - 2 * h * η ^ 2.
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W, given by 1 - 4 * d η - 2 * D h * η * U j η.
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- NavierStokes.NaturalAxisData.W h j η = 1 - 4 * NavierStokes.NaturalAxisData.d η - 2 * NavierStokes.NaturalAxisData.D h * η * NavierStokes.NaturalAxisData.U j η
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Chi, given by (H h j η) ^ 2 / ((H h j η) ^ 2 + σ ^ 2).
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- NavierStokes.NaturalAxisData.chi h j σ η = NavierStokes.NaturalAxisData.H h j η ^ 2 / (NavierStokes.NaturalAxisData.H h j η ^ 2 + σ ^ 2)
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The proof gives 2.991, stronger than the manuscript's 2.8.
Real pressure hypotheses provided by the separately constructed datum. The derivative-sign condition is weak, so zero derivative is permitted.
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A quantitative version of the crucial nonzero-root assertion: pressure at most minus one is already sufficient.
The true fixed data have a unique negative root at which Z is bounded
strictly away from zero. No root property is an input hypothesis.
On the actual compact low-Z set, H² has a strictly positive uniform
minimum. The threshold is the explicit choice δ_* = j/10.
Construct the cutoff scale after the root-separation proof. The proof
chooses σ_* = sqrt(m)/20 from the actual compact minimum bound.
The requested fixed positive choices, with no input separation premise.
The actual integral pressure datum satisfies the real axis hypotheses.
The ideal-prefix amplitude B ≥ 2 suffices uniformly on [-1,1].
End-to-end real cutoff construction from the actual weighted pressure integral and its ideal prefix, rather than assumed pressure conclusions.
Uniform analytic input for the natural-axis coefficient space #
The hypotheses concern one common complex neighborhood of the entire real parameter interval. Cauchy's integral formula supplies bounds on actual derivatives; the derivative bounds are not hypotheses of the construction.
A uniform complex value bound, with holomorphy on a neighborhood of the same closed tube. No derivative estimates occur in this predicate.
- analytic : AnalyticOnNhd ℂ f (closedTube I ρ)
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Cauchy's estimate for every genuine complex derivative, derived from the circle-integral coefficients and the factorial derivative identity.
The real part of a genuine complex jet, evaluated on the real axis.
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- NavierStokes.AnalyticCoefficientBounds.realJet f m x = (iteratedDeriv m f ↑x).re
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The real-axis jets really are the ordinary iterated real derivatives.
The Cauchy bound fits the exact degree-zero manuscript weight.
A coefficient family concentrated at radial degree zero.
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A bounded holomorphic function supplies an actual degree-zero element of the compatible coefficient Banach space.
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The normalized axis exponential, defined on the whole complex plane but bounded using the common complex neighborhood.
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- NavierStokes.AnalyticCoefficientBounds.normalizedExp F Λ C z = Complex.exp (↑Λ * F z) / ↑C
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One lower bound on C supplies all derivative bounds simultaneously.
The upper bound on Re F is imposed on the complex tube, not just its real axis.
Supremum over a fixed compact complex set, used for the literal
normalization threshold exp(Λ sup Re F).
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A compact wider complex neighborhood is enough: every radius-ρ
closed disc about a real parameter must lie inside it.
Uniform degree-zero data for every admissible pair (Λ,C).
The element is constructed from compatible actual derivatives, and its
norm bound depends only on the two radii.
The compact-neighborhood form uses exactly C ≥ exp(Λ sup Re F).
The order is: fix I, ε, ρ, K, F, then choose Λ and any sufficiently
large C; the coefficient norm threshold remains the same.
An actual holomorphic primitive on a convex open set #
The primitive is the radial segment integral. Its derivative is proved by differentiating under a uniformly dominated integral on a compact local product, then applying the real fundamental theorem of calculus along the segment. No disk containing the entire domain and no assumed primitive are required.
The same derivative integrand is the real derivative of t*g(t*z).
The normalized exponential built from the actual segment primitive.
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Normalization is constant in the spatial variable, so the differential equation is valid for any normalization scalar.
The actual logarithmic derivative of the nonvanishing normalized exponential is the prescribed scaled holomorphic gradient.
A fixed, slightly enlarged real parameter interval.
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- NavierStokes.NaturalAxisCoefficients.window = { left := -11 / 10, right := 11 / 10, nondegenerate := NavierStokes.NaturalAxisCoefficients.window._proof_1 }
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Complex U, given by 4 * z + (j : ℂ).
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- NavierStokes.NaturalAxisCoefficients.complexU j z = 4 * z + ↑j
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Denominator, given by complexH h j z ^ 2 + (σ : ℂ) ^ 2.
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- NavierStokes.NaturalAxisCoefficients.denominator h j σ z = NavierStokes.NaturalAxisCoefficients.complexH h j z ^ 2 + ↑σ ^ 2
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Complex gradient, given by -complexL h z * complexH h j z / denominator h j σ z.
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Real gradient, given by -NaturalAxisData.L h x * NaturalAxisData.H h j x / (NaturalAxisData.H h j x ^ 2 + σ ^ 2).
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- NavierStokes.NaturalAxisCoefficients.realGradient h j σ x = -NavierStokes.NaturalAxisData.L h x * NavierStokes.NaturalAxisData.H h j x / (NavierStokes.NaturalAxisData.H h j x ^ 2 + σ ^ 2)
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The open region where all fixed rational expressions and pressure are analytic.
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Complex field used in natural axis coefficients.
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- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.one = fun (x : ℂ) => 1
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.eta = fun (z : ℂ) => z
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.d = NavierStokes.NaturalAxisCoefficients.complexD
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.inverseL = fun (z : ℂ) => (NavierStokes.NaturalAxisCoefficients.complexL h z)⁻¹
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.uStar = NavierStokes.NaturalAxisCoefficients.complexU j
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.uStarEta = fun (x : ℂ) => 4
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.wStar = NavierStokes.NaturalAxisCoefficients.complexW h j
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.hStar = NavierStokes.NaturalAxisCoefficients.complexH h j
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.zStar = NavierStokes.NaturalAxisCoefficients.complexZ h j P
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.chi = NavierStokes.NaturalAxisCoefficients.complexChi h j σ
- NavierStokes.NaturalAxisCoefficients.complexField h j σ P NavierStokes.NaturalAxisCoefficients.Field.gradient = NavierStokes.NaturalAxisCoefficients.complexGradient h j σ
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Real field used in natural axis coefficients.
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- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.one = fun (x : ℝ) => 1
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.eta = fun (x : ℝ) => x
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.d = NavierStokes.NaturalAxisData.d
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.inverseL = fun (x : ℝ) => (NavierStokes.NaturalAxisData.L h x)⁻¹
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.uStar = NavierStokes.NaturalAxisData.U j
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.uStarEta = fun (x : ℝ) => 4
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.wStar = NavierStokes.NaturalAxisData.W h j
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.hStar = NavierStokes.NaturalAxisData.H h j
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.zStar = NavierStokes.NaturalAxisData.Z h j P
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.chi = NavierStokes.NaturalAxisData.chi h j σ
- NavierStokes.NaturalAxisCoefficients.realField h j σ P NavierStokes.NaturalAxisCoefficients.Field.gradient = NavierStokes.NaturalAxisCoefficients.realGradient h j σ
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One compact complex neighborhood for the whole finite family.
A convex open outer neighborhood and compact inner neighborhood. The inner radius can be used for both the fixed fields and an analytic primitive.
Compactness and finiteness give one common value bound for all inputs.
An arbitrary finite complex bound is reduced to the unit-bound Cauchy constructor.
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- NavierStokes.NaturalAxisCoefficients.boundedAxisElement hε hερ hB hf hb = B • ⋯.toAxisSpace hε hερ
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A finite family of actual degree-zero fields, all using the same positive parameter radius and the same finite norm bound.
- epsilon : ℝ
Epsilon of
CoefficientFamily, of typeℝ. - elements : Field → ↥(AxisCoefficientSpace.AxisSpace window self.epsilon)
Elements of
CoefficientFamily, of typeField → AxisSpace window epsilon. - bound : ℝ
Bound of
CoefficientFamily, of typeℝ.
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The coefficient family and the open convex domain for its primitive can be chosen together, with an explicit strict gap between the two radii.
Axis data, bundling A, D, h, one and the required compatibility proofs.
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The actual normalized logarithmic phase, as a complex segment integral.
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Real phase, given by x * ∫ t in (0 : ℝ)..1, realGradient h j σ (t * x).
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- NavierStokes.NaturalAxisCoefficients.realPhase h j σ x = x * ∫ (t : ℝ) in 0..1, NavierStokes.NaturalAxisCoefficients.realGradient h j σ (t * x)
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The fixed coefficient family and its actual analytic phase on one common compact neighborhood. No primitive or coefficient record is assumed by the existence theorem below.
- coefficients : CoefficientFamily h j σ P
Coefficients of
AnalyticInputs, of typeCoefficientFamily h j σ P. - radius : ℝ
Radius of
AnalyticInputs, of typeℝ. Compact set of
AnalyticInputs, of typeSet ℂ.- isCompact : IsCompact self.compactSet
- covers (x : ℝ) : x ∈ window.interval → Metric.closedBall (↑x) self.radius ⊆ self.compactSet
- phase_analytic : AnalyticOnNhd ℂ (axisPhase h j σ) self.compactSet
- phase_derivative (z : ℂ) : z ∈ self.compactSet → HasDerivAt (axisPhase h j σ) (complexGradient h j σ z) z
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Real amplitude, given by Real.exp (Λ * realPhase h j σ x) / C.
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- NavierStokes.NaturalAxisCoefficients.realAmplitude h j σ Λ C x = Real.exp (Λ * NavierStokes.NaturalAxisCoefficients.realPhase h j σ x) / C
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Normalization threshold, given by Real.exp (Λ * realPartSup (axisPhase h j σ) d.compactSet).
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Amplitude bound, given by radiusLoss (d.coefficients.epsilon / d.radius).
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The actual φ*/C belongs to exactly the same coefficient space as
all fixed data, uniformly for every allowed large parameter and normalization.
End-to-end fixed analytic input construction from the actual pressure integral and ideal prefix, including the normalized amplitude source.
Pullback, given by F (rescalePoint Λ p).
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The fixed polynomial and pressure fields, interpreted as real functions.
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Replace all coefficient evaluations by their proved concrete values.
The natural transport coefficient recovered from the true radial average.
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- NavierStokes.NaturalProfile.transportW h V p = 1 - 2 * NavierStokes.NaturalAxisData.D h * p.2 * V p - NavierStokes.NaturalAxisData.d p.2 * NavierStokes.NaturalAxisBridge.partialEta V p
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Transport H, given by NaturalAxisData.D h * p.2 + NaturalAxisData.d p.2 * U p.
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- NavierStokes.NaturalProfile.transportH h U p = NavierStokes.NaturalAxisData.D h * p.2 + NavierStokes.NaturalAxisData.d p.2 * U p
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The actual unscaled system, with all derivatives taken on real functions.
- f_smooth : ContDiffOn ℝ (↑⊤) f (domain Λ)
- U_smooth : ContDiffOn ℝ (↑⊤) U (domain Λ)
- average_smooth : ContDiffOn ℝ (↑⊤) V (domain Λ)
- pressure_smooth : ContDiffOn ℝ (↑⊤) Pr (domain Λ)
- U_axis (η : ℝ) : η ∈ Set.Ioo NaturalAxisCoefficients.window.left NaturalAxisCoefficients.window.right → U (0, η) = NaturalAxisData.U j η
- average_axis (η : ℝ) : η ∈ Set.Ioo NaturalAxisCoefficients.window.left NaturalAxisCoefficients.window.right → V (0, η) = NaturalAxisData.U j η
- angular_equation (p : ℝ × ℝ) : p ∈ domain Λ → 2 * NaturalAxisData.L h p.2 * NaturalAxisBridge.radialDifferential 2 f p = transportW h V p * (p.1 * NaturalAxisBridge.partialY f p + f p) + h * (1 - 2 * p.2 * U p) * f p + transportH h U p * NaturalAxisBridge.partialEta f p
- axial_equation (p : ℝ × ℝ) : p ∈ domain Λ → 2 * NaturalAxisData.L h p.2 * NaturalAxisBridge.radialDifferential 1 U p = transportW h V p * (p.1 * NaturalAxisBridge.partialY U p) + NaturalAxisData.A h * (1 - 2 * p.2 * U p) * U p + transportH h U p * NaturalAxisBridge.partialEta U p + NaturalAxisData.d p.2 * NaturalAxisBridge.partialEta Pr p - 4 * NaturalAxisData.A h * p.2 * Pr p - 2 * p.2 * p.1 * NaturalAxisBridge.partialY Pr p
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Reconstruction preserves the full differential and integral system.
Profile error constant, constructed using errorConstant.
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The functions and estimates obtained from one actual coefficient-space fixed point. All unscaled functions are explicit expressions in these fields.
Phi of
ProfileFamily, of typeℝ × ℝ → ℝ.U of
ProfileFamily, of typeℝ × ℝ → ℝ.Average of
ProfileFamily, of typeℝ × ℝ → ℝ.Pressure field of
ProfileFamily, of typeℝ × ℝ → ℝ.- natural : IsNaturalSolution h j Λ P0 (NaturalAxisCoefficients.realAmplitude h j σ Λ C) (angularProfile (NaturalAxisCoefficients.realAmplitude h j σ Λ C) Λ self.phi) (affineProfile (NaturalAxisData.U j) (1 / Λ) Λ self.u) (affineProfile (NaturalAxisData.U j) (1 / Λ) Λ self.average) (affineProfile P0 (1 / Λ) Λ self.pressure)
- mixed_error : NaturalAxisBridge.UniformMixedError NaturalAxisCoefficients.window d.coefficients.epsilon (profileErrorConstant d / (2 * Λ)) self.phi self.u (AxisEvaluation.profile NaturalAxisCoefficients.window d.coefficients.epsilon (NaturalAxisBridge.referenceCoefficients NaturalAxisCoefficients.window ⋯ (d.coefficients.elements NaturalAxisCoefficients.Field.chi) d.coefficients.axisData).1) (AxisEvaluation.profile NaturalAxisCoefficients.window d.coefficients.epsilon (NaturalAxisBridge.referenceCoefficients NaturalAxisCoefficients.window ⋯ (d.coefficients.elements NaturalAxisCoefficients.Field.chi) d.coefficients.axisData).2)
- slope (η : ℝ) : η ∈ Set.Ioo NaturalAxisCoefficients.window.left NaturalAxisCoefficients.window.right → 99 / 100 ≤ NaturalAxisData.chi h j σ η → 23 / 10 < -2 * (4 / Λ) * NaturalAxisBridge.partialY (angularProfile (NaturalAxisCoefficients.realAmplitude h j σ Λ C) Λ self.phi) (4 / Λ, η) / angularProfile (NaturalAxisCoefficients.realAmplitude h j σ Λ C) Λ self.phi (4 / Λ, η)
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F, given by angularProfile (realAmplitude h j σ Λ C) Λ F.phi.
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U, given by affineProfile (NaturalAxisData.U j) (1 / Λ) Λ F.u.
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- F.U = NavierStokes.NaturalProfile.affineProfile (NavierStokes.NaturalAxisData.U j) (1 / Λ) Λ F.u
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Ubar, given by affineProfile (NaturalAxisData.U j) (1 / Λ) Λ F.average.
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- F.Ubar = NavierStokes.NaturalProfile.affineProfile (NavierStokes.NaturalAxisData.U j) (1 / Λ) Λ F.average
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Pi, given by affineProfile P0 (1 / Λ) Λ F.pressure.
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- F.Pi = NavierStokes.NaturalProfile.affineProfile P0 (1 / Λ) Λ F.pressure
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The scale threshold is uniform over every normalization above the actual compact-domain exponential threshold.
The pressure integral and ideal prefix yield actual unscaled natural profiles after selecting the cutoff and common analytic coefficient radius.
A direct existence theorem for the unscaled real functions. The cutoff, analytic input family, large scale, and normalization are all constructed from the stated pressure assumptions.