Attenuated Radon transform Created 2026-10-06 Updated 2026-10-14
The integral of a source over a directed line, weighted by exponential absorption between each source point and a detector. For line coordinates and a detector at the negative end, it is . The integrating factor of a transport equation derives the weight. Reversing the detector direction changes the weight for spatially varying attenuation, so the two directed measurements need not coincide. Setting recovers the Radon transform.
Computed tomography Created 2026-10-14 Updated 2026-10-20
Transmission measurements determine line integrals of an absorption coefficient after taking the logarithm of incident intensity divided by transmitted intensity. Under the ideal straight-ray model, these measurements are a Radon transform; filtered backprojection reconstructs a planar slice. Angular coverage, calibration and noise control matter because differentiating measured projections amplifies high frequencies. In contrast, single-photon emission computed tomography reconstructs an emitting source through a possibly attenuating medium.
Filtered backprojection 2026-10-14
The Radon transform records line integrals of a planar density. Apply the transverse Hilbert transform and a derivative to each projection, then average the filtered values over all lines through the reconstruction point. With , the filter has Fourier multiplier . The Fourier inversion theorem, or the jump of the complexified transport Cauchy kernel, proves the displayed formula. The factor is when directions are integrated over a half-circle. The growing Fourier multiplier explains amplification of measurement noise and the need for regularization of an inverse problem.
Define the Radon transform and its transverse Hilbert transform by
Use the signed Cauchy boundary operators and . Thus and are the complementary idempotent projections; itself carries the signed lower-boundary convention. The PDF defines the outside limit but omits the definition of the inside limit in its displayed formula. We take , as required by that formula.
As , apply the Sokhotski–Plemelj formula to the kernel from part (b):
The principal value contribution is . The delta contribution is the same from either side and equals
Since for the inside limit, the resulting boundary value is
The outside limit similarly has in place of . Naming the signed convention explicitly prevents a sign error from treating as a positive projection.
In ideal computed tomography, the unknown is an absorption coefficient . Along a straight ray the transmitted intensity satisfies , so
Thus calibrated transmission measurements supply the Radon transform of the slice. The inversion above reconstructs the coefficient by filtered backprojection: filter each projection in its transverse variable and then accumulate it over the rays through each image point. This turns a collection of line-integral measurements into a spatial map, which is the key usefulness of the result.
The ideal derivation assumes known ray geometry, sufficiently complete angular sampling and a straight-ray attenuation model. The ramp Fourier multiplier grows at high frequency, so measurement noise is amplified. Practical reconstruction therefore uses discretization and regularization of an inverse problem, for example a window on the ramp filter. Limited angles or missing detector positions cannot be treated as if they were complete noiseless Radon transform data.
Keep the coordinates and operator from part (a). The attenuation is known, and the source is to be reconstructed. Put and . The directed forward attenuated Radon transform, for a detector at the positive end of the line, is
This weight accounts for absorption from each emission point to the detector. It is also derived by solving the real transport equation with zero incoming intensity: its outgoing limit is . In particular reversing the line direction generally changes the measurement. The pair reconstructs from full directed data and known ; it does not infer both unknown functions from the same data.
We must specify the sign convention for the projectors. Use the Hilbert transform and the signed Cauchy boundary operators
Then , and the positive idempotent projectors are and . This is the signed boundary-value convention in the given limits of . To express everything with ordinary complementary projectors, one may instead write , . The given limits become
Both depend on the transverse coordinate and direction but are constant along .
The equation supplies an integrating factor:
where is the inverse of unattenuated complex transport, normalized to vanish at spatial infinity. To see the normalization and analyticity rather than assume them, let . The complexified transport Cauchy kernel is
In the rotated coordinates, . The identity and the Jacobian prove with exactly this normalization. The denominator cannot vanish for nonzero real off the unit circle. The kernel is analytic separately inside and outside that circle, is at zero and at infinity. Thus and the displayed have the corresponding spectral behavior for the smooth decaying data. In particular at infinity and is bounded, indeed , at zero.
The limiting unattenuated inverse on any smooth decaying input is
One may verify this directly in the rotated Fourier variables: has multiplier , so its inverse has a pole at . As , the positive transverse frequencies have the negative tail primitive and the negative transverse frequencies have the positive past primitive; for these allocations reverse. Splitting with the Fourier projectors yields exactly the two formulas above. Applying them to reproduces the assumed limits of and checks the signs.
Now apply the same limiting inverse to . Because are independent of , its line integral is , while its tail is . Hence
The unknown incomplete line integral cancels in their difference. All remaining quantities are obtained from the measurements and known attenuation:
Each projection acts in at fixed , before evaluating and . Pulling a transverse-dependent exponential outside a projector would be incorrect.
The sectionally analytic therefore solves an additive Riemann-Hilbert problem on the counterclockwise unit circle, with the plus value inside. The normalized Cauchy integral formula is
The Sokhotski–Plemelj theorem gives its jump; boundedness at zero and decay at infinity make it unique by the Liouville theorem. Its expansion at infinity is
Substitute into the original equation. The part contributes at order one, the reciprocal derivative and vanish at that order. This derives the projection formula for inverse attenuated Radon transform:
Together with the boxed forward transform this is the requested pair. The derivation uses no small-attenuation approximation. For smooth compactly supported data the operations above are justified directly; sufficient integrable decay permits the same limiting construction.
As a normalization check, set . Then , and . Since the line transform is independent of and , the formula reduces to
the full-angle inverse Radon transform. For the radial Gaussian , and , so the reconstructed value at the origin is , checking the factor.
In single-photon emission computed tomography, represents the internal emission density, the known absorption coefficient and the directed detector counts. Each path integral weights a source point by its survival probability to the detector. Thus the attenuated Radon transform is the forward measurement model and its derived inverse reconstructs the emission distribution, providing the mathematical basis of SPECT.
Let be the Radon transform
Taking the large-radius limit in the Kirchhoff formula, with fixed for the outgoing limit and fixed for the incoming limit, gives the radiation fields
Indeed, the expanding spheres converge after multiplication by to the planes and , respectively.
The Radon transforms of smooth compactly supported functions are smooth. If the data are supported in a ball of radius , these transforms vanish for . Hence both radiation fields are well-defined smooth functions of compact support in the null-time variable.
Tomography 2026-10-14
Tomography reconstructs an interior distribution from measurements along multiple lines or paths through it. A linear unattenuated model is the Radon transform; absorption changes it to an attenuated Radon transform.