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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,
|
(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
|
(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
|
(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
|
(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
|
(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
|
(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
|
(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