- John's equation
John's equation is an ultrahyperbolic
partial differential equation satisfied by theX-ray transform of a function. It is named afterFritz John .Given a function with compact support the "X-ray transform" is the integral over all lines in . We will parameterise the lines by pairs of points on each line and define "u" as the ray transform where:then "u" satisfies John's equation: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:where , such that thequadratic form :can be reduced by a linear change of variables to the form :Unlike the wave equation and other hyperbolic partial differential equations, 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
* Fritz John, The ultrahyperbolic differential equation with four independent variables, Duke Math. J. 4, no. 2 (1938), 300–322
* S K Patch, Consistency conditions upon 3D CT data and the wave equation, Phys. Med. Biol. 47 No 15 (7 August 2002) 2637-2650 doi|10.1088/0031-9155/47/15/306
Wikimedia Foundation. 2010.