Integrated tangential balances from actual radial differential expressions #
All moments below are actual Bochner integrals. Compact radial support supplies
the boundary cancellations, and parameter derivatives pass under integrals by
the dominated differentiation theorem in TransportPrimitive.
Smooth compact radial families and their moments #
Radial moment, given by moment n (fun r => F (r, p)).
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- NavierStokes.IntegratedMeanBalances.radialMoment n F p = NavierStokes.IntegratedMeanBalances.moment n fun (r : ℝ) => F (r, p)
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Parameter partial, given by fderiv ℝ F x (0, v).
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Actual torus averages annihilate the lift derivatives #
Torus average, given by ∫ y in (0 : ℝ)..1, torusInner F (p, y).
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Fixed partial, given by fderiv ℝ F q v.
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- NavierStokes.IntegratedMeanBalances.fixedPartial v F q = (fderiv ℝ F q) v
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Slow partial, given by fixedPartial ((v, 0), 0) F.
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Torus partial, given by fixedPartial ((0, v.2), v.1) F.
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Both parameter-integral interchanges are proved from joint smoothness on the compact torus coordinate square.
Graph partial, given by slowPartial v F q + a q.1.1 * torusPartial w F q.
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Graph lift terms integrate to zero; only the genuine slow derivative remains.
The averaged chart balances and their exact weighted integrals #
Mean parameter: an abbreviation for ℝ × ℝ.
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Joint smoothness and a common compact radial shell are genuine input regularity conditions on the pointwise fields, not conditions on their moments.
- supported : RadialAlias.RadiallySupported a b F
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The angular line of (32), after the actual torus average. Coordinates are
(R,(T,Z)); ε is constant on a chart. The supplied fluxes are full averages
of the pointwise products in (32), and the last radial divergence is the virtual stress.
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- One or more equations did not get rendered due to their size.
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The axial line of (32), with pressure retained inside the axial flux.
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- One or more equations did not get rendered due to their size.
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The first identity in (34), derived from the pointwise angular balance.
The second tangential integral, before eliminating the pressure moment.
Pressure total, given by radialMoment 0 gr.
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Pressure coefficient, given by radialMoment 2 ρ p / 2.
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Axial defect, given by radialMoment 1 axialFlux p - (1 / 2 : ℝ) * radialMoment 2 gr p.
Equations
- NavierStokes.IntegratedMeanBalances.axialDefect axialFlux gr p = NavierStokes.IntegratedMeanBalances.radialMoment 1 axialFlux p - 1 / 2 * NavierStokes.IntegratedMeanBalances.radialMoment 2 gr p
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The pressure coefficient stays inside the actual axial derivative, exactly as in (34); it may vary with both slow parameters.
Restriction to the physical positive radial half-line #
The actual pressure primitive (33), without a supplied derivative identity #
Exact moment of the constructed compact pressure, including its normalized mean correction. The derivative used in the proof is a theorem of the actual physical transport integral, not an assumption here.
Reconstructed mean pressure, given by PressureStream.torusAverage (PressureStream.meanPressure d a b M hab v f).
Equations
- NavierStokes.IntegratedMeanBalances.reconstructedMeanPressure d a b M hab v f = NavierStokes.PressureStream.torusAverage (NavierStokes.PressureStream.meanPressure d a b M hab v f)
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Averaged radial source, given by PressureStream.torusAverage f.
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Normalized mean density, given by PressureStream.rho a b hab x.1.
Equations
- NavierStokes.IntegratedMeanBalances.normalizedMeanDensity a b hab x = NavierStokes.PressureStream.rho a b hab x.1
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The second identity of (34) with pressure supplied by the actual compact primitive (33). No pressure moment or pressure derivative identity is assumed.