The physical residual of a scaled graph pullback #
This file keeps the cylindrical angle separate from the lifted slow and fast variables. Every differential operator is an actual Frechet derivative.
The complete real graph-coordinate residual, including the quadratic transport term and the cylindrical connection terms.
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Repeating the genuine derivative differentiates the target direction field as well. In particular this includes the radial-profile derivative.
Differential data used by the generic pullback calculation below. The explicit physical graph later supplies every field of this structure.
- source_open : IsOpen Ω
- target_open : IsOpen U
- smooth : ContDiffOn ℝ (↑⊤) Γ Ω
- mapsTo : Set.MapsTo Γ Ω U
- radial_smooth : ContDiffOn ℝ (↑⊤) Vr U
- angular_smooth : ContDiffOn ℝ (↑⊤) Vθ U
- axial_smooth : ContDiffOn ℝ (↑⊤) Vz U
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Plane: an abbreviation for ℝ × ℝ.
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Lift: an abbreviation for ℝ × (Plane × Plane).
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Numerical and directional data of one fixed chart.
- radialScale : ℝ
Radial scale of
ScaledGraph, of typeℝ. - velocityScale : ℝ
Velocity scale of
ScaledGraph, of typeℝ. - epsilon : ℝ
Epsilon of
ScaledGraph, of typeℝ. - exponent : ℝ
Exponent of
ScaledGraph, of typeℝ. - frequency : ℝ
Frequency of
ScaledGraph, of typeℝ. - fastCoefficient : ℝ
Fast coefficient of
ScaledGraph, of typeℝ. - radialVector : Plane
Radial vector of
ScaledGraph, of typePlane. - temporalVector : Plane
Temporal vector of
ScaledGraph, of typePlane.
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Map as an element of Cylinder.
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Radius, given by x.1.1.
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Radial, given by ((1, ((0, 0), (G.frequency * GraphCalculus.radialSpeed G.exponent x.1.1) • G.radialVector)), 0).
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Angular, given by (0, 1).
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Temporal, given by ((0, ((0, -G.epsilon), G.fastCoefficient • G.temporalVector)), 0).
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Forward physical time produces minus the slow-time direction.
Source, given by {p | 0 < p.2 0} ∩ G.map ⁻¹' U.
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Physical cylindrical velocity obtained from the actual graph.
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- G.velocity a p = NavierStokes.AxisymmetricResidual.pack (G.velocityScale * a (G.map p) 0) (G.velocityScale * a (G.map p) 1) (G.velocityScale * a (G.map p) 2)
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Pressure, defined pointwise by G.velocityScale ^ 2 * p (G.map z).
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Identification with the viscosity-one Cartesian PDE. The representation premises concern only field values on a neighborhood.
One arbitrary integer-cover chart; the index is not constrained to the native band index.
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The exact power multiplying the physical viscosity-one residual.
The actual linear-plus-quadratic correction expression #
Complex increment as an element of ℝ.
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The base equation supplies only the fixed base residual. All linear, quadratic, pressure, and viscous increment terms are derived above.
The absolute graph before choosing a band or an integer covering.
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Matching consists of the literal coefficient and direction data at one band, with no assumption about a residual or a differential operator.
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Base components, given by ![c.base.radial n x.1, c.base.angular n x.1, c.base.axial n x.1].
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Increment components, given by ![s.mean.radial n x.1 + s.oscillation n x 0, s.mean.angular n x.1 + s.oscillation n x 1, s.mean.axial n x.1 + s.oscillation n x 2].
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Exact total-field residual for the actual correction state. The only base premise is its independently verified fixed pressure/virtual-stress equation, and the base error is included once.
The actual correction-state residual is the scaled Cartesian
Navier--Stokes residual on the physical graph. The cover index k is free.
The base pressure is fixed separately because a correction state stores only
pressure increments.