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.
For , put and , with . Dividing by this accumulated homogeneous growth gives and . A telescoping series then proves
This is the discrete counterpart of the integrating factor for a first-order linear differential equation.