Ewald sphere 2026-10-14
With , elastic scattering into a propagating wavevector samples Fourier transfer . These transfers satisfy the displayed shifted sphere relation. This reciprocal-space construction appears in crystallographic diffraction and the Fourier diffraction theorem.
Let , and use the same two-dimensional Fourier transform for at a fixed depth. For propagating modes, and . Fourier transforming the angular spectrum in the previous part gives
The factor cancels against the change of transverse spectral variables . Hence the recoverable samples satisfy
Equivalently, in terms of the requested two-dimensional transform of ,
This is the Fourier diffraction theorem. It recovers Fourier samples on the two hemispheres of a shifted Ewald sphere, since the outgoing wavevector has length and the Fourier transfer is .
For a general three-dimensional , this is not enough to recover at every depth or reconstruct uniquely. At a fixed transverse frequency, the two planes supply only two longitudinal Fourier samples. Additional incident directions, frequencies or prior constraints are required. Thus the inverse problem as worded yields the boxed sampling relation, rather than a unique unconstrained volumetric solution.
An explicit nullspace makes this obstruction stronger than a dimension count. For any real smooth with compact support in , take the Born non-scattering contrasts at one incident direction
Its Fourier transform is . On the sampled sphere, , so this polynomial factor vanishes. Nonzero real compactly supported contrasts can therefore give identical propagating data to zero contrast in this linear approximation. Their amplitude can be made small enough to keep and remain in the weak-scattering regime. In fact the associated Born field is . Applying gives the source , while compact support makes this field zero on both exterior measurement planes. Thus this example also defeats recovery from their evanescent components.
The nullspace in the Fourier diffraction theorem already prevents uniqueness, and the rapid decay of evanescent high-frequency information prevents stable recovery. Both make this an ill-posed inverse problem.
Let be the linear Born approximation operators mapping a real contrast supported in a known region to the measured fields on the two observation planes. For data , a suitable Tikhonov reconstruction from two-plane scattering data minimizes
A Sobolev norm penalty can instead express a smoothness preference. Reality, known support and can be imposed as constraints. For the unconstrained complex Hilbert-space problem with the displayed quadratic penalty, write and . Its Tikhonov normal equation is
Tikhonov regularization selects a stable preferred estimate; it does not establish that the original two-plane data uniquely determine the true contrast.