John's equation

From HandWiki

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:ℝn→ℝ with compact support the X-ray transform is the integral over all lines in ℝn. We will parameterise the lines by pairs of points x,y∈ℝn, x≠y on each line and define u as the ray transform where

u(x,y)=∫−∞∞f(x+t(y−x))dt.

Such functions u are characterized by John's equations

∂2u∂xi∂yj−∂2u∂yi∂xj=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

∑i,j=12naij∂2u∂xi∂xj+∑i=12nbi∂u∂xi+cu=0

where n≥2, such that the quadratic form

∑i,j=12naijξiξj

can be reduced by a linear change of variables to the form

∑i=1nξi2−∑i=n+12nξi2.

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