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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 k-space. 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 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