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228 Inverse scattering transform for the KdV equation
S (k, 0) =
{κ
j
, C
j
(0)}
N
#
j=1
,ρ(k, 0) ≡
b(k, 0)
a(k, 0)
,
where κ
j
, j = 1, 2,...,N
#
, are the locations of the zeros of a(k, 0) and C
j
(0),
j = 1, 2,...,N
#
, are often called the associated “normalization constants” that
were also defined above.
Next we determine the time evolution of the scattering data using equations
(9.39)–(9.40). This yields the scattering data at any time t:
S (k, t) =
{κ
j
, C
j
(t)}
N
#
j=1
,ρ(k, t) ≡
b(k, t)
a(k, t)
.
For the inverse problem, at time t, we solve either the integral equations for
N(x, t) and reconstruct u(x, t)via(9.34)–(9.36) or solve the Gel’fand–Levitan–
Marchenko equations for K(x, y, t) and reconstruct u(x, t)via(9.42)–(9.44).
This method is conceptually analogous to the Fourier transform method for
solving linear equations (discussed in Chapter 2), except however the step
of solving the inverse scattering problem requires one to solve a linear inte-
gral equation (i.e., a Riemann–Hilbert boundary value problem) that adds
complications. Schematically the solution is given by
u(x, 0)
direct scattering
−−−−−−−−−−−→ S (k, 0) =
{κ
n
, C
j
(0)}
N
#
j=1
,ρ(k, 0), a(k, 0)
⏐
⏐
⏐
⏐
⏐
*
t: time evolution
u(x, t)
inverse scattering
←−−−−−−−−−−−− S (k, t) =
{κ
n
, C
j
(t)}
N
#
j=1
,ρ(k, t), a(k, t)
In the analogy of IST to the Fourier transform method for linear partial dif-
ferential equations, the direct scattering problem and the scattering data play
the role of the Fourier transform and the inverse scattering problem the inverse
Fourier transform.
9.7 Soliton solutions of the KdV equation
In this section we will describe how the inverse scattering method can be used
to find soliton solutions of the Korteweg–de Vries equation (9.3).
9.7.1 The Riemann–Hilbert method
Pure soliton solutions may be obtained from (9.34)–(9.36) in the case when
ρ(k, t) = 0 on the real k-axis. This is usually called a reflectionless potential.
We assume a special form for ρ(k; t), namely