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We can assume, without loss of generality, that the incident wave-function
is characterized by a wave-vector
which is aligned parallel to the
-axis.
The scattered wave-function is characterized by a wave-vector
which has the same magnitude as
, but, in general, points
in a different direction. The direction of
is specified
by the polar angle
(i.e., the angle subtended between the
two wave-vectors), and an azimuthal angle
about the
-axis.
Equations (1248) and (1249) strongly suggest that for a spherically symmetric
scattering potential [i.e.,
] the scattering amplitude
is a function of
only: i.e.,
 |
(1261) |
It follows that neither the incident wave-function,
 |
(1262) |
nor the large-
form of the total wave-function,
![\begin{displaymath}
\psi({\bf r}) = \sqrt{n}
\left[ \exp(\,{\rm i}\,k\,r\cos\theta) + \frac{\exp(\,{\rm i}\,k\,r)\, f(\theta)}
{r} \right],
\end{displaymath}](img2793.png) |
(1263) |
depend on the azimuthal angle
.
Outside the range of the scattering potential, both
and
satisfy the free space Schrödinger equation
 |
(1264) |
What is the most general solution to this equation in spherical polar
coordinates which does not depend on the azimuthal angle
?
Separation of variables yields
 |
(1265) |
since the Legendre functions
form a complete
set in
-space. The Legendre functions are related to the
spherical harmonics, introduced in Sect. 8, via
 |
(1266) |
Equations (1264) and (1265) can be combined to give
![\begin{displaymath}
r^2\,\frac{d^2 R_l}{dr^2} + 2\,r \,\frac{dR_l}{dr} + [k^2 \,r^2 -
l\,(l+1)]R_l = 0.
\end{displaymath}](img2798.png) |
(1267) |
The two independent solutions to this equation are the
spherical Bessel functions,
and
, introduced in Sect. 9.3.
Recall that
Note that the
are well-behaved in the limit
, whereas the
become singular.
The asymptotic behaviour of these functions in the limit
is
We can write
 |
(1272) |
where the
are constants. Note there are no
functions in
this expression, because they are not well-behaved as
.
The Legendre functions are orthonormal,
 |
(1273) |
so we can invert the above expansion to give
 |
(1274) |
It is well-known that
 |
(1275) |
where
[see M. Abramowitz and I.A. Stegun, Handbook of mathematical functions, (Dover, New York NY, 1965),
Eq. 10.1.14]. Thus,
 |
(1276) |
giving
 |
(1277) |
The above expression tells us how to decompose
the incident plane-wave into
a series of spherical waves. These waves are usually termed ``partial waves''.
The most general expression for the total wave-function outside the
scattering region is
![\begin{displaymath}
\psi({\bf r}) = \sqrt{n}\sum_l\left[
A_l\,j_l(k\,r) + B_l\,y_l(k\,r)\right] P_l(\cos\theta),
\end{displaymath}](img2810.png) |
(1278) |
where the
and
are constants.
Note that the
functions are allowed to appear
in this expansion, because
its region of validity does not include the origin. In the large-
limit, the total wave-function reduces to
![\begin{displaymath}
\psi ({\bf r} ) \simeq \sqrt{n} \sum_l\left[A_l\,
\frac{\sin...
..._l\,\frac{\cos(k\,r -l\,\pi/2)}{k\,r}
\right] P_l(\cos\theta),
\end{displaymath}](img2813.png) |
(1279) |
where use has been made of Eqs. (1270) and (1271). The above expression can also
be written
 |
(1280) |
where the sine and cosine functions have been combined to give a
sine function which is phase-shifted by
. Note that
and
.
Equation (1280) yields
![\begin{displaymath}
\psi({\bf r}) \simeq \sqrt{n} \sum_l C_l\left[
\frac{{\rm e}...
...\pi/2+ \delta_l)} }{2\,{\rm i}\,k\,r} \right] P_l(\cos\theta),
\end{displaymath}](img2818.png) |
(1281) |
which contains both incoming and outgoing spherical waves. What is the
source of the incoming waves? Obviously, they must be part of
the large-
asymptotic expansion of the incident wave-function. In fact,
it is easily seen from Eqs. (1270) and (1277)
that
![\begin{displaymath}
\psi_0({\bf r}) \simeq \sqrt{n} \sum_l {\rm i}^{\,l}\,
(2l+1...
...\,(k\,r - l\,\pi/2)}}{2\,{\rm i}\,k\,r} \right]P_l(\cos\theta)
\end{displaymath}](img2819.png) |
(1282) |
in the large-
limit. Now, Eqs. (1262) and (1263) give
 |
(1283) |
Note that the right-hand side consists of an outgoing spherical
wave only. This implies that the coefficients of the incoming spherical waves
in the large-
expansions of
and
must be the same. It follows from Eqs. (1281) and (1282) that
![\begin{displaymath}
C_l = (2\,l+1)\,\exp[\,{\rm i}\,(\delta_l + l\,\pi/2)].
\end{displaymath}](img2821.png) |
(1284) |
Thus, Eqs. (1281)-(1283) yield
 |
(1285) |
Clearly, determining the scattering amplitude
via a decomposition into
partial waves (i.e., spherical waves) is equivalent to determining
the phase-shifts
.
Now, the differential scattering cross-section
is simply
the modulus squared of the scattering amplitude
[see Eq. (1245)]. The
total cross-section is thus given by
where
. It follows that
 |
(1287) |
where use has been made of Eq. (1273).
Next: Determination of phase-shifts
Up: Scattering theory
Previous: The Born approximation
Contents
Richard Fitzpatrick
2006-12-12