The actual zero-endpoint transverse displacement inverse #
We use the derivative of the physical displacement as the Hilbert-space variable. Terminal integration supplies the displacement. Its initial trace and its moving normal component are bounded linear constraints, hence define a closed Hilbert subspace. The kinetic energy is exactly the squared norm on this space; no norm equivalence or pre-existing differential inverse is assumed.
This constructs the weak transverse inverse in source lines 172--184. The
coordinate identity η = F R ξ and strong coordinate evolution require the
separate frame and regularity arguments; they are not assumed in this file.
Recovering the source's transverse coordinates #
The moving plane with normal (F⁻¹)* m₀ is exactly the image under F of
the fixed plane m₀⊥. Orthogonal projection gives a bounded coordinate map,
and on the moving plane its reconstruction is the identity. These are
coefficient identities, not assumptions about a differential inverse.
The fixed reference transverse plane.
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The actual pulled-back normal used by the packet construction.
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Bounded recovery of fixed-plane coordinates from a physical displacement.
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Moving tangency is exactly fixed-plane membership after applying F⁻¹.
Reconstructing a tangent displacement from its recovered coordinates is exact.
The coordinate map is a left inverse to F restricted to the reference plane.
The coordinate map has the expected polynomial bound from the inverse frame.
Any orthonormal identification with the fixed plane gives the source's R⊥ coordinates.
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The full source reconstruction η = F R⊥ ξ follows from moving tangency.
Passing to an orthonormal coordinate basis has no extra norm cost.
Applying a continuous inverse-frame path produces actual continuous transverse coordinates, not separate incompatible pointwise choices.
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The recovered continuous coordinates reconstruct every tangent displacement.
Zero endpoint displacements give zero endpoint coordinates.
Pointwise coordinate control only pays the actual inverse-frame norm.
Derivatives of actual zero-endpoint displacements tangent to the moving plane.
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The two endpoint and moving tangency conditions are closed constraints.
Closedness supplies completeness for the actual displacement-derivative space.
The zero initial trace is exactly the zero-mean condition on the time derivative.
Every genuine absolutely continuous zero-endpoint transverse path with an L² derivative belongs to this Hilbert model. Thus the test space is not an assumed family of already solved displacements.
The actual terminal primitive restricted to the transverse derivative space.
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The sharp time Poincaré bound holds on the actual transverse space.
A convenient polynomial operator bound for the terminal primitive.
The actual transverse forcing-to-derivative map, constructed from the primitive and the given time-dependent Hessian.
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The continuous displacement is constructed by integrating its solved derivative.
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The solved displacement vanishes at the initial endpoint.
The solved displacement vanishes at the terminal endpoint.
The solved displacement belongs to the actual moving transverse plane.
The derivative of the constructed displacement is the solved L² field, as an actual almost-everywhere derivative of its continuous real-time representative.
The actual weak transverse displacement equation, tested against every zero-endpoint displacement in the same moving plane.
The constructed weak inverse is unique in the actual transverse displacement space.
The solved derivative has a polynomial finite-time bound, with no exponential in H.
Zero forcing has zero displacement, the pointwise-in-label support preservation property.
The inverse preserves sign, hence oddness in a parameter with unchanged coefficients.
A zero angle mean of the forcing gives a zero angle mean of the displacement. The measure can be the normalized periodic angle measure; coefficients are fixed in this parameter.
Existence and uniqueness follow from the actual sharp time primitive estimate, the pointwise potential bound, and closed transverse constraints.
The actual weak inverse has the source's form η = F R⊥ ξ, with continuous
coordinates and both endpoint conditions. The frame is prescribed coefficient
data; neither a displacement nor a differential inverse is supplied.