Genuine smooth profile histories #
The histories are actual integrals of jointly smooth profiles. Their parameter derivatives and radial identities are derived from differentiation under the integral and the fundamental theorem of calculus, rather than supplied as independent history data.
Exact radial stress identities #
This file verifies the algebra and radial calculus in equations (6)--(9) of the candidate manuscript. Parameter derivatives are supplied as independent radial functions, with their requisite radial derivative identities stated explicitly. No existence of the candidate profiles or estimates for them is asserted.
The axial scaling exponent from the manuscript.
Equations
- NavierStokes.StressAlgebra.axialExponent h = 1 / 2 - h
Instances For
The velocity scaling exponent from the manuscript.
Equations
- NavierStokes.StressAlgebra.velocityExponent h = 1 / 2 + h
Instances For
H S_q, with radial derivatives written explicitly instead of logarithms.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The angular integration-by-parts cancellation, as an exact polynomial identity.
The axial integration-by-parts cancellation, including both pressure identities.
Genuine radial differentiation of the angular primitive. The moment hypotheses
are precisely I_x = H, (I_η)_x = H_η, J_x = UH, and
(J_η)_x = U_ηH + UH_η.
Genuine radial differentiation of the axial primitive. In addition to the
moment identities this uses x P_x = E²/2 and its η derivative.
Data for the angular integrated identity on a specified closed radial interval. The fields are differential and initial conditions, not an assumed integral identity.
W of
AngularMomentData, of typeℝ → ℝ.Wx of
AngularMomentData, of typeℝ → ℝ.H of
AngularMomentData, of typeℝ → ℝ.Hx of
AngularMomentData, of typeℝ → ℝ.Hη of
AngularMomentData, of typeℝ → ℝ.U of
AngularMomentData, of typeℝ → ℝ.Uη of
AngularMomentData, of typeℝ → ℝ.I of
AngularMomentData, of typeℝ → ℝ.Iη of
AngularMomentData, of typeℝ → ℝ.J of
AngularMomentData, of typeℝ → ℝ.Jη of
AngularMomentData, of typeℝ → ℝ.
Instances For
The first integral formula in the proof of Lemma 3.3, derived by the fundamental theorem of calculus from explicit differential moment conditions.
Differential and initial data required for the axial integrated identity.
W of
AxialMomentData, of typeℝ → ℝ.Wx of
AxialMomentData, of typeℝ → ℝ.U of
AxialMomentData, of typeℝ → ℝ.Ux of
AxialMomentData, of typeℝ → ℝ.Uη of
AxialMomentData, of typeℝ → ℝ.E of
AxialMomentData, of typeℝ → ℝ.Eη of
AxialMomentData, of typeℝ → ℝ.P of
AxialMomentData, of typeℝ → ℝ.Px of
AxialMomentData, of typeℝ → ℝ.Pη of
AxialMomentData, of typeℝ → ℝ.Pηx of
AxialMomentData, of typeℝ → ℝ.M of
AxialMomentData, of typeℝ → ℝ.Mη of
AxialMomentData, of typeℝ → ℝ.Parameter
SofAxialMomentData, of typeℝ → ℝ.Sη of
AxialMomentData, of typeℝ → ℝ.
Instances For
The second integral formula in Lemma 3.3, including its pressure terms.
The angular formula (9) after division by the regular integrating factor.
The left side is the regular primitive definition of Q_s.
The axial formula (9) after division by its regular integrating factor.
The left side is the regular primitive definition of N_s.
The source written with logarithmic derivatives agrees with H S_q.
Its use for actual logarithms requires the usual nonvanishing profile conditions.
Multiplying (6)'s angular lag equation by its integrating factor gives the
primitive equation. This equivalence uses genuine derivatives of H and Q.
The axial lag equation's integrating factor is x.
The angular stress-free substitution from (7) yields exactly the radial
second-order expression in (8). Here φx and φxx denote radial derivatives.
The angular coefficient of (7), with its radial viscous primitive exposed.
This verifies the sign of the subtraction of a = 1 - 2 dot(E)/E.
Point: an abbreviation for ℝ × ℝ.
Equations
Instances For
An open profile domain containing every radial segment from the axis to one of its points. Open rectangles centered radially at zero are examples.
Carrier of
RadialDomain, of typeSet Point.
Instances For
A concrete open rectangle meeting the axis. Positivity of R is needed only to make it nonempty, not for the radial stability proof.
Equations
Instances For
The derivative of the compact parameter integral is the integral of the genuine parameter derivative. Joint smoothness supplies the local majorant.
The history has its defining integrand as genuine radial derivative.
Parameter differentiation commutes with the regular average, including at X=0.
The parameter derivative of a history is the actual history of the parameter derivative; no history derivative is assumed.
Mixed radial/parameter differentiation of an actual history.
Eη, defined pointwise by Real.sqrt (2 * p.1) * parameterPartial P.f p.
Instances For
Transport density, defined pointwise by P.U p * P.H p.
Equations
- P.transportDensity p = P.U p * P.H p
Instances For
Equations
Instances For
Equations
Instances For
J, given by primitive P.transportDensity.
Equations
Instances For
S, given by primitive P.energyDensity.
Equations
Instances For
Equations
Instances For
Pressure, defined pointwise by P.pressure0 p.2 + primitive (fun q => P.f q ^ 2) p.
Equations
- P.pressure p = P.pressure0 p.2 + NavierStokes.ProfileHistories.primitive (fun (q : NavierStokes.ProfileHistories.Point) => P.f q ^ 2) p
Instances For
W, defined pointwise by 1 - 2 * axialExponent h * p.2 * P.Ubar p - coordinateFactor p.2 * average (parameterPartial P.U) p.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The key identity used in both integrations by parts is derived from FTC.
Every field and every derivative in the angular stress data is obtained from the actual profiles and the actual integral histories.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The axial data also use the pressure constructed by integrating f².
Equations
- One or more equations did not get rendered due to their size.
Instances For
Angular source, defined pointwise by StressAlgebra.angularSource h p.2 p.1 (P.W h p) (P.U p) (P.H p) (radialPartial P.H p) (parameterPartial P.H p).
Equations
- One or more equations did not get rendered due to their size.
Instances For
Axial source as an element of Field.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The printed Q_s is the regular primitive divided by its integrating factor.
Equations
- P.angularLag h p = NavierStokes.ProfileHistories.primitive (P.angularSource h) p / (p.1 * P.H p)
Instances For
The printed N_s is the regular primitive divided by X.
Equations
- P.axialLag h p = NavierStokes.ProfileHistories.primitive (P.axialSource h) p / p.1
Instances For
Equation (9), angular row, for actual smooth profile histories.
Equation (9), axial row, with constructed pressure and actual histories.
The angular differential equation (6), with logarithmic slopes as ratios of genuine derivatives.
The axial differential equation (6), with the actual primitive-defined N_s.
The angular row of (6) with actual logarithms, not surrogate slope data.
The axial row of (6), with the pressure derivative proved from its integral.