Endpoint extensions of the actual summed slow base #
At nonzero axial coordinate the stable coordinate extension has positive q. The original cutoff schedule therefore gives a locally finite series on an open neighborhood crossing t = 1. No new summation or cutoff choice is made.
For velocity and pressure, the nonzero-axial extension combines with the proved heat exterior on the central plane. The forward-integral potential is only extended at nonzero axial coordinate here; a central-plane gauge correction is a separate construction.
The same coefficient series evaluated at the actual stable coordinate extension, including the original leading power.
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Cartesian profile extension, given by profileExtension a h b f (AxisymmetricFields.profilePoint z.1 z.2).
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One neighborhood and one finite index work for every coefficient family. In particular the seven bundled fields keep the same schedule.
Stream extension, given by profileExtension a h (-CoordinateAlgebra.A h) (bundleComponent C d 0).
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Swirl extension, given by profileExtension a h (1 / 2 - CoordinateAlgebra.A h) (bundleComponent C d 1).
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Potential extension, given by AxisymmetricFields.potential (streamExtension a h C d) (swirlExtension a h C d).
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Velocity extension, given by SpatialCurl.spatialCurl (potentialExtension a h C d).
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Pressure extension, given by cartesianProfileExtension a h (-2 * CoordinateAlgebra.A h) (bundleComponent C d 2).
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The original forward-integral potential extends at every nonzero axial endpoint, with exactly the original cutoff schedule.
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Velocity nonzero axial, bundling value, domain, isOpen, mem and the required
compatibility proofs.
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Pressure nonzero axial, bundling value, domain, isOpen, mem and the required
compatibility proofs.
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The fixed physical radial anchor used for the exact gauge correction.
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This is the literal anchored-potential formula. Equality of its curl with the original velocity is proved in the separate gauge module.
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Anchored potential extension, constructed using AxisymmetricFields.potential.
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The exact anchored potential also extends at every nonzero axial endpoint. In particular the subtracted gauge uses the same sum and schedule.
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Convert a genuine locally smooth closed-side continuation into an ambient smooth extension. A local bump and the already proved joint Taylor--Borel extension are the actual construction.
For the actual repaired scheme, velocity and pressure have ambient smooth continuations at every nonzero point of the terminal slice.
The original potential of the actual entrance-aligned base extends at nonzero axial coordinate, with its selected scale sequence unchanged.
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- NavierStokes.SlowBaseEndpoint.finalPotentialNonzeroAxial H v upper B hx = NavierStokes.SlowBaseEndpoint.potentialNonzeroAxial ⋯ ⋯ ⋯ ⋯ W.axis.normalization hx
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Final velocity nonzero axial, constructed using velocityNonzeroAxial.
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- NavierStokes.SlowBaseEndpoint.finalVelocityNonzeroAxial H v upper B hx = NavierStokes.SlowBaseEndpoint.velocityNonzeroAxial ⋯ ⋯ ⋯ ⋯ W.axis.normalization hx
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Final pressure nonzero axial, constructed using pressureNonzeroAxial.
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- NavierStokes.SlowBaseEndpoint.finalPressureNonzeroAxial H v upper B hx = NavierStokes.SlowBaseEndpoint.pressureNonzeroAxial ⋯ ⋯ ⋯ ⋯ W.axis.normalization hx
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Final anchored potential nonzero axial, constructed using anchoredPotentialNonzeroAxial.
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This includes the central plane and the spatial axis away from zero. The inputs are the actual finite profile witnesses, not endpoint assumptions.
The already constructed finite profile gives actual endpoint extensions for the selected slow base without another profile input.