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Let us test out this scheme using a particularly simple example. Consider
scattering by a hard sphere, for which the potential is infinite
for
, and zero for
. It follows that
is
zero in the region
, which implies that
for all
.
Thus,
 |
(1298) |
for all
. Equation (1291) thus gives
 |
(1299) |
Consider the
partial wave, which is usually referred to as the
-wave.
Equation (1299) yields
 |
(1300) |
where use has been made of Eqs. (1268) and (1269). It follows that
 |
(1301) |
The
-wave radial wave function
is [see Eq. (1289)]
The corresponding radial wave-function for the incident wave
takes the form [see Eq. (1277)]
 |
(1303) |
Thus, the actual
radial wave-function is similar to the
incident
wave-function, except that it is phase-shifted by
.
Let us examine the low and high energy asymptotic limits of
.
Low energy implies that
. In this regime, the spherical Bessel functions
reduce to:
where
. It follows that
![\begin{displaymath}
\tan\delta_l = \frac{-(k\,a)^{2\,l+1}}{(2\,l+1) \,[(2\,l-1)!!]^{\,2}}.
\end{displaymath}](img2864.png) |
(1306) |
It is clear that we can neglect
, with
, with respect to
. In other words, at low energy only
-wave scattering
(i.e., spherically symmetric scattering) is important. It follows
from Eqs. (1245), (1285), and (1301) that
 |
(1307) |
for
. Note that the total cross-section
 |
(1308) |
is four times the geometric cross-section
(i.e., the cross-section for classical particles bouncing off a
hard sphere of radius
).
However,
low energy scattering implies relatively long wave-lengths, so we would not
expect to obtain the classical result in this limit.
Consider the high energy limit
. At high energies, all partial
waves up to
contribute significantly to
the scattering cross-section. It follows from Eq. (1287) that
 |
(1309) |
With so many
values contributing, it is legitimate to replace
by its average value
. Thus,
 |
(1310) |
This is twice the classical result, which is somewhat surprizing,
since we might expect to obtain the classical result in the short
wave-length limit. For hard sphere scattering, incident waves with
impact parameters less than
must be deflected. However, in order to
produce a ``shadow'' behind the sphere, there must also be some scattering
in the forward direction in order to produce
destructive interference with the incident plane-wave. In fact, the
interference is not completely destructive, and the shadow has a bright
spot (the so-called ``Poisson spot'') in the forward direction. The effective cross-section associated with
this bright spot is
which, when combined with the
cross-section for classical reflection,
, gives the actual
cross-section of
.
Next: Low energy scattering
Up: Scattering theory
Previous: Determination of phase-shifts
Contents
Richard Fitzpatrick
2006-12-12