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We can assume, without loss of generality, that the incident wavefunction
is characterized by a wavevector
which is aligned parallel to the
-axis.
The scattered wavefunction is characterized by a wavevector
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 wavevectors), and an azimuthal angle
about the
-axis.
Equations (1269) and (1270) strongly suggest that for a spherically symmetric
scattering potential [i.e.,
] the scattering amplitude
is a function of
only: i.e.,
 |
(1282) |
It follows that neither the incident wavefunction,
 |
(1283) |
nor the large-
form of the total wavefunction,
![\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}](img2906.png) |
(1284) |
depend on the azimuthal angle
.
Outside the range of the scattering potential, both
and
satisfy the free space Schrödinger equation
 |
(1285) |
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
 |
(1286) |
since the Legendre functions
form a complete
set in
-space. The Legendre functions are related to the
spherical harmonics, introduced in Cha. 8, via
 |
(1287) |
Equations (1285) and (1286) 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}](img2911.png) |
(1288) |
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
 |
(1293) |
where the
are constants. Note there are no
functions in
this expression, because they are not well-behaved as
.
The Legendre functions are orthonormal,
 |
(1294) |
so we can invert the above expansion to give
 |
(1295) |
It is well-known that
 |
(1296) |
where
[see M. Abramowitz and I.A. Stegun, Handbook of mathematical functions, (Dover, New York NY, 1965),
Eq. 10.1.14]. Thus,
 |
(1297) |
giving
 |
(1298) |
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 wavefunction 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}](img2923.png) |
(1299) |
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 wavefunction 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}](img2926.png) |
(1300) |
where use has been made of Eqs. (1291) and (1292). The above expression can also
be written
 |
(1301) |
where the sine and cosine functions have been combined to give a
sine function which is phase-shifted by
. Note that
and
.
Equation (1301) 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}](img2931.png) |
(1302) |
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 wavefunction. In fact,
it is easily seen from Eqs. (1291) and (1298)
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}](img2932.png) |
(1303) |
in the large-
limit. Now, Eqs. (1283) and (1284) give
 |
(1304) |
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. (1302) and (1303) that
![\begin{displaymath}
C_l = (2 l+1) \exp[ {\rm i} (\delta_l + l \pi/2)].
\end{displaymath}](img2934.png) |
(1305) |
Thus, Eqs. (1302)-(1304) yield
 |
(1306) |
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. (1266)]. The
total cross-section is thus given by
where
. It follows that
 |
(1308) |
where use has been made of Eq. (1294).
Next: Determination of Phase-Shifts
Up: Scattering Theory
Previous: Born Approximation
Richard Fitzpatrick
2010-07-20