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In a subsequent chapter we shall study the inhomogeneous Helmholtz wave
equation
It is amusing that the solution to this equation exhibits a property
which is readily expressed in terms of a Dirichlet kernel and more
generally in terms of a Fourier series. This property is so useful,
physically fundamental, and deducible with so little effort that it is
worthwhile to give a quick derivation.
The property pertains to the field amplitude
when the
inhomogeneity (``source'') of the wave equation is concentrated at,
say,
sources
In that case, the governing Helmholtz equation is
![$\displaystyle \left[ \frac{\partial ^2}{\partial x ^2} +\frac{\partial ^2}{\par...
...t] \psi (x,y,z)= -\sum^N_{n=-N} A_n~\delta (x-x_n) \delta (y-y_n)\delta (z-z_n)$](img575.png) |
(23) |
One can readily show that the solution to this inhomogeneous wave equation
is
Each term in this solution is proportional to the
strength of each corresponding localized source of the wave equation.
The quantity
is the distance between
, the point where the field is observed,
and
, the location of the
th source point.
We now consider the circumstance where this distance is large. More
precisely, we assume that if the sources are distributed along, say, the
-axis,
and the amplitude is observed at, say,
so that the distance is
then ``large distance'' means that
is so large that
For such distances the solution has the form
 |
(24) |
The long distance assumption can be strengthened by demanding that both
 |
(25) |
be satisfied. This strengthened assumption is called the ``Fraunhofer
approximation''.
Under this approximation the third contribution to the phase in the
exponential of the solution, Eq.(2.4), is so
small that this contribution can also be neglected.
As a consequence the solution assumes the perspicuous form
 |
(26) |
Suppose the
sources are equally spaced and hence are located at
In that case the solution is a
-term Fourier series whose
coefficients are the source strengths
in Eq.(
):
 |
(27) |
We thus have proved the following fundamental
Theorem 21.1 (Fraunhofer-Kirchhoff)
At sufficiently large distances expressed by Eq.(
2.5), the solution to the inhomogeneous Helmholtz wave equation,
Eq.(
2.3), has the Fourier form
Eq.(
2.6)
whose spectral coefficients are the strengths of the inhomogeneities
in that wave equation. If these inhomogeneities are equally spaced, then the
solution is a Fourier series, Eq.(
2.7).
When all the sources have equal strength, say
, then the solution
is proportional to the Dirichlet kernel,
 |
(28) |
which varies with
in a way given in Fig. 2.1.
For the sake of completeness it is necessary to point out that the
Fraunhofer approximation can always be
satisfied by having the separation between the ``observation'' point
and the finite source region be large enough. If it is not satisfied,
i.e., if
 |
(29) |
then the third contribution to the phase of the solution,
Eq.(2.4), cannot be neglected. This less
stringent assumption is called the ``Fresnel
approximation''.
Exercise 21.1 (SHIFTED INTEGRATION LIMITS)
Suppose that

is an integrable function of period

. Show that
where

is any real number.
Next: Dirichlet Kernel: Fountainhead of
Up: Three Applications
Previous: Three Applications
Contents
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Ulrich Gerlach
2007-04-05