A Fredholm equation is an integral equation in which the term containing the kernel function has constants as integration limits. A closely related form is the Volterra integral equation which has variable integral limits. An inhomogeneous Fredholm equation of the first kind is written as and the problem is, given the continuous kernel function and the function, to find the function. An important case of these types of equation is the case when the kernel is a function only of the difference of its arguments, namely, and the limits of integration are ±∞, then the right hand side of the equation can be rewritten as a convolution of the functions and and therefore, formally, the solution is given by where and are the direct and inverse Fourier transforms, respectively. This case would not be typically included under the umbrella of Fredholm integral equations, a name that is usually reserved for when the integral operator defines a compact operator.
Equation of the second kind
An inhomogeneous Fredholm equation of the second kind is given as Given the kernel , and the function , the problem is typically to find the function . A standard approach to solving this is to use iteration, amounting to the resolvent formalism; written as a series, the solution is known as the Liouville–Neumann series.
General theory
The general theory underlying the Fredholm equations is known as Fredholm theory. One of the principal results is that the kernel yields a compact operator. Compactness may be shown by invoking equicontinuity. As an operator, it has a spectral theory that can be understood in terms of a discrete spectrum of eigenvalues that tend to 0.
Applications
Fredholm equations arise naturally in the theory ofsignal processing, for example as the famous spectral concentration problem popularized by David Slepian. The operators involved are the same as linear filters. They also commonly arise in linear forward modeling and inverse problems. In physics, the solution of such integral equations allows for experimental spectra to be related to various underlying distributions, for instance the mass distribution of polymers in a polymeric melt, or the distribution of relaxation times in the system. In addition, Fredholm integral equations also arise in fluid mechanics problems involving hydrodynamic interactions near finite-sized elastic interfaces.