25.7 WKB METHODS
one function and the same function may need different expansions for
different values of argz.
Finally in this subsection we note that, although the form of equation (25.42) may
appear rather restrictive, in that it contains no term iny′, the results obtained so
far can be applied to an equation such as
d^2 y
dz^2
+P(z)
dy
dz
+Q(z)y=0. (25.56)
To make this possible, a change of either the dependent or the independent
variable is made. For the former we write
Y(z)=y(z)exp
(
1
2
∫z
P(u)du
)
⇒
d^2 Y
dz^2
+
(
Q−
1
4
P^2 −
1
2
dP
dz
)
Y=0,
whilst for the latter we introduce a new independent variableζdefined by
dζ
dz
=exp
(
−
∫z
P(u)du
)
⇒
d^2 y
dζ^2
+Q
(
dz
dζ
) 2
y=0.
In either case, equation (25.56) is reduced to the form of (25.42), though it
will be clear that the two sets of WKB solutions (which are, of course, only
approximations) will not be the same.
25.7.4 The Stokes phenomenon
As we saw in subsection 25.7.2, the combination of WKB solutions of a differential
equation required to reproduce the asymptotic form of the accurate solutiony(z)
of the same equation, varies according to the region of thez-plane in whichzlies.
We now consider this behaviour, known as the Stokes phenomenon, in a little
more detail.
Lety 1 (z)andy 2 (z) be the two WKB solutions of a second-order differential
equation. Then any solutionY(z) of the same equation can be written asymptot-
ically as
Y(z)∼A 1 y 1 (z)+A 2 y 2 (z), (25.57)
where, although we will be considering (abrupt) changes in them, we will continue
to refer toA 1 andA 2 as constants, as they are within any one region. In order to
produce the required change in the linear combination, as we pass over a Stokes
line from one region of thez-plane to another, one of the constants must change
(relative to the other) as the border between the regions is crossed.
At first sight, this may seem impossible without causing a discernible discon-
tinuity in the representation ofY(z). However, we must recall that the WKB
solutions are approximations, and that, as they contain a phase integral, for
certain values of argzthe phaseφ(z) will be purely imaginary and the factors