Longitudinal Ray Transform

In mathematics the longitudinal ray transform (LRT) is a generalization of the X-ray transform to symmetric tensor fields
V.A. Sharafutdinov, Integral Geometry of Tensor Fields, VSP 1994,. Chapter
on-line version
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Let $f_$ be the components of a symmetric rank-m tesnor field ($m\ge$) on Euclidean space $\mathbf^n$ ($n \ge 2$). For a unit vector $\xi, , \xi, =1$ and a point $x \in \mathbf^n$ the longitudinal ray transform is defined as
:$g(x, \xi):= If(x, \xi)= \int\limits_^\infty f_(x+ s \xi) \xi_ \cdots \xi_\, \mathrms$
where summation over repeated indices is implied. The transform has a null-space, assuming the components are smooth and decay at infinity any $f= dg$, the symmetrized derivative of a rank m-1 tensor field $g$, satisfies $If=0$. More generally the Saint-Venant tensor $Wf$ can be recovered uniquely by an explicit formula. For lines that pass through a curve similar results can be obtained to the case of the complete data case of all lines

Applications of the LRT include Bragg edge neutron tomography of strain, and Doppler tomography of velocity vector fields.T. Schuster, An efficient method for three-dimensional vector tomography: convergence and
implementation, Inverse problems, 17 (2001), 739-766

References

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Integral geometry