Distribution theory may often be used to find solutions of inhomogeneous linear partial differential equations by the technique of Green’s functions. We give here two important standard examples.
Poisson’s equation
To solve an inhomogeneous equation such as Poisson’s equation
we seek a solution to the distributional equation
A solution of Poisson’s equation Eq. (12.15) is then
for
To solve, set
By Fourier’s theorem
which implies that
But
so
Substituting in Eq. (12.16) gives
and
The integration in -space is best performed using polar coordinates with the -axis pointing along the direction (see Fig. 12.2). Then
and
Figure 12.2 Change to polar coordinates in -space.
This results in
on making use of the well-known definite integra
Hence
and a solution of Poisson’s equation Eq. (12.15) is
where the integral is taken over all of the space, . For a point charge, the solution reduces to the standard coulomb solution
Green’s function for the wave equation
To solve the inhomogeneous wave equation
it is best to adopt a relativistic 4-vector notation, setting . The wave equation can then be written as in Section 9.4,
where and range from 1 to , is the diagonal metric tensor having diagonal components and the argument in the last term is shorthand for ).
Again we look for a solution of the equation
Every Green’s function generates a solution of Eq. (12.19),
for
Show that the general solution of the inhomogeneous wave equation Eq. (12.19) has the form where
Set
where , and
and . Writing the four-dimensional function as a Fourier transform we have
whence
Figure 12.3 Green’s function for the three-dimensional wave equation
where . The Fourier transform expression of the Green’s function is thus
To evaluate this integral set
whence and
Deform the path in the complex to avoid the pole singularities at as shown in Fig. 12.3 – convince yourself, however, that this has no effect on satisfying Eq. (12.20).
For the contour is completed in a counterclockwise sense by the upper half semi circle and
For we complete the contour with the lower semicircle in a clockwise direction; no poles are enclosed and the integral vanishes. Hence
where is the Heaviside step function.
This particular contour gives rise to a Green’s function that vanishes for ; that is, for . It is therefore called the outgoing wave condition or retarded Green’s function, for a source switched on at only affects field points at later times. Ifthe contour had been chosen to lie above the poles, then the ingoing wave condition or advanced Green’s function would have resulted.
To complete the calculation of , use polar coodinates in -space with the -axis paralle to . This gives
The last step follows because the whole expression vanishes for on account of the factor, while for we have . Hence the Green’s function may be written
which is non-vanishing only on the future light cone of
The solution of the inhomogeneous wave equation Eq. (12.19) generated by this Green’s function is
where means evaluated at the retarded time
Problems
Show that the Green’s function for the time-independent Klein–Gordon equation
can be expressed as the Fourier integra
Evaluate this integral and show that it results in
Find the solution corresponding to a point source
Show that the Green’s function for the one-dimensional diffusion equation,
is given by
and write out the corresponding solution of the inhomogeneous equation
Do the same for the two- and three-dimensional diffusion equations