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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 internal waves in a stratified fluid of great
          depth and in the propagation of nonlinear Rossby waves in a rotating fluid.
          It can be expressed in the form
                               u t +4uu x + H{u xx } =0,
          where H{f(x)} denotes the Hilbert transform of f(x) defined as

                                        1  ,  ∞  f(y)
                             H{f(x)} =   P           dy
                                        π       y − x
                                            −
          and where P denotes 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
                 2A x A = A (A xx + ωA t )+ A(A xx + ωA t ) ∗  (ω = −1),
                      ∗
                           ∗
                      x
                 ∗
          where A is the complex conjugate of A, and found a solution in which
          A is a determinant of arbitrary order whose diagonal elements are linear
          in x and t and 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
                         ∂  	  ∂P  −1  
  ∂  	  ∂P  −1
                             ρ   P     +      ρ   P    =0,
                         ∂ρ    ∂ρ        ∂z    ∂z
          where the matrix P is defined as

                                    1   1     ψ
                                P =         2    2  .                (6.2.6)
                                    φ ψ    φ + ψ
          φ is the gravitational potential and is real and ψ is 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.
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