6.2 Brief Historical Notes 241
linear operators and a determinant of arbitrary order whose elements are
defined as integrals.
The verifications given in Sections 6.7 and 6.8 of the non-Wronskian
solutions of both the KdV and KP equations apply purely determinantal
methods and are essentially those published by Vein and Dale in 1987.
6.2.7 The Benjamin–Ono Equation
The Benjamin–Ono (BO) equation is a nonlinear integro-differential equa-
tion which arises in the theory of internalwaves in astratified fluid of great
depth and in the propagation of nonlinear Rossbywaves in arotating fluid.
It can be expressed in the form
ut+4uux+H{uxx}=0,
whereH{f(x)}denotes the Hilbert transform off(x) defined as
H{f(x)}=
1
π
P
∫
∞
−∞
f(y)
y−x
dy
and wherePdenotes the principal value.
In a paper published in 1988, Matsuno introduced a complex substitution
into the BO equation which transformed it into a more manageable form,
namely
2 AxA
∗
x=A
∗
(Axx+ωAt)+A(Axx+ωAt)
∗
(ω
2
=−1),
whereA
∗
is the complex conjugate ofA, and found a solution in which
Ais a determinant of arbitrary order whose diagonal elements are linear
inxandtand whose nondiagonal elements contain a sequence of distinct
arbitrary constants.
6.2.8 The Einstein and Ernst Equations
In the particular case in which a relativistic gravitational field is axially
symmetric, the Einstein equations can be expressed in the form
∂
∂ρ
(
ρ
∂P
∂ρ
P
− 1
)
+
∂
∂z
(
ρ
∂P
∂z
P
− 1
)
=0,
where the matrixPis defined as
P=
1
φ
[
1 ψ
ψφ
2
+ψ
2
]
. (6.2.6)
φis the gravitational potential and is real andψis either real, in which
case it is the twist potential, or it is purely imaginary, in which case it has
no physical significance. (ρ, z) are cylindrical polar coordinates, the angular
coordinate being absent as the system is axially symmetric.