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John's equation
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John's equation : ウィキペディア英語版
John's equation
John's equation is an ultrahyperbolic partial differential equation satisfied by the X-ray transform of a function. It is named after Fritz John.
Given a function f\colon\mathbb^n \rightarrow \mathbb with compact support the ''X-ray transform'' is the integral over all lines in \mathbb^n. We will parameterise the lines by pairs of points x,y \in \mathbb^n, x \ne y on each line and define ''u'' as the ray transform where
: u(x,y) = \int\limits_^ f( x + t(y-x) ) dt.
Such functions ''u'' are characterized by John's equations
: \frac - \frac=0
which is proved by Fritz John for dimension three and by Kurusa for higher dimensions.
In three-dimensional x-ray computerized tomography John's equation can be solved to fill in missing data, for example where the data is obtained from a point source traversing a curve, typically a helix.
More generally an ''ultrahyperbolic'' partial differential equation (a term coined by Richard Courant) is a second order partial differential equation of the form
: \sum\limits_^ a_\frac +
\sum\limits_^ b_i\frac + cu =0
where n \ge 2, such that the quadratic form
: \sum\limits_^ a_ \xi_i \xi_j
can be reduced by a linear change of variables to the form
: \sum\limits_^ \xi_i^2 - \sum\limits_^ \xi_i^2.
It is not possible to arbitrarily specify the value of the solution on a non-characteristic hypersurface. John's paper however does give examples of manifolds on which an arbitrary specification of ''u'' can be extended to a solution.
==References==

*
* Á. Kurusa, A characterization of the Radon transform's range by a system of PDEs, J. Math. Anal. Appl., 161(1991), 218--226.
* S K Patch, Consistency conditions upon 3D CT data and the wave equation, Phys. Med. Biol. 47 No 15 (7 August 2002) 2637-2650

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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