Spectral Deformations and
Soliton
Equations
117
A
further degeneration
K
+
0
finally yields
V(z)
=
0
and
y2
=
(-z)~.
(4.8)
This point of view has been adopted in [48] and [49] and the general
n-soliton potentials have been derived from the Its-Matveev formula
by
a
singularization of
K,
where all compact spectral bands degen-
erate into
a
single point
2
[E2(j4),
E2j-11
-
-Kj,
1
I
j
5
12,
K1
>
K2
>
*-.
>
K,,
E2n
=
0
(4.9)
(see (3.3)).
Here we shall
in
a
sense reverse the above point of view. Instead
of starting with
a
finite-gap potential such as (4.1) and degenerating
compact spectral bands into single points (such
as
in (4.4) with the
result (4.5)-(4.7)), we shall start with
a
finite-gap potential
VO
and
insert eigenvalues into its spectral gaps. In the context of the above
example this amounts to starting with
V&)
=
0,
y2
=
--z
(4.10)
and inserting the eigenvalue
-tc2
into the spectral gap
po
=
(-oo,O)
of
Vo
to arrive at
VI(X)
=
-2K~[COSh(Kx)]-2,
y2
=
(-62
-
-z)+).
(4.11)
The spectral deformations described
so
far were clearly non-isospec-
tral. In addition we will also discuss various isospectral deformations
of potentials below.
In
short, these isospectral deformations either
“insert eigenvalues” at points where there were already eigenvalues
or
they formally insert eigenvalues with certain “defects” such as
zero
or
infinite norming constants. In either case no new eigenvalue
is actually inserted and the deformation is isospectral.
A
systematic
and detailed approach to these ideas can be found in (251-[27].
We start with the single commutation method
or
Crum-Darboux
method [11]-[14],
[18],
[19], [3G],
[Gl].
Assume that
VO
E
Lioc
(IR)
is
real-valued and that the differential expression
(4.12)