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Rays and Waves    251


               write the wavefunction in terms of a slowly varying amplitude and a
               rapidly oscillating phase, i.e.,


                                                  i
                                ( r, t) = A( r, t) exp  	( r, t)    (8.38)
                                                  ¯ h

               Notice that the phase was chosen to be proportional to the inverse
               of ¯h. Therefore, like k for the Helmholtz case, ¯h −1  plays the role of
               the large asymptotic parameter. The resulting approximate results are
               then valid within the so-called semiclassical regime, i.e., when ¯h is
               small compared to all other quantities (or variations of quantities) in
               theproblemunderstudythatpresentthesameunits(action=length×
               mass × speed).
                 After substitution of Eq. (8.38) and reordering, Eq. (8.37) can be
               written as

                                                         2
                  ∂	   |∇	| 2          ∂ A  2∇ A·∇	 + A∇ 	      2  2
                     +      + V  − i¯h    +                  − ¯h ∇ A = 0
                  ∂t    2m             ∂t         2m
                                                                    (8.39)
               Again, we face a decision between two approaches:
                  1. Assume that ¯h is very small, and expand A in a Debye series.
                  2. Assume that both A and 	 are real, and separate the real and
                    imaginary parts of Eq. (8.39).
                 As before, let us consider approach 1 first.


               8.5.1 Semiclassical Mechanics
               We start by setting the leading term in Eq. (8.39) to zero. This leads to
               the equation

                                    ∂	   |∇	| 2
                                       +      + V = 0               (8.40)
                                    ∂t    2m
               This is the equation for the action in classical mechanics. Like the
               eikonal equation, it can be solved parameterically. We start by pa-
               rameterizing the position as   =   R(t,   1 ,   2 ,   3 ). We then define the
                                        r
               momentum P and the Hamiltonian H, respectively, as the spatial and

               (minus the) temporal derivatives of the action
                                      P =∇	(   R, t)                (8.41)

                                            ∂
                                      H =−    (   R, t)             (8.42)
                                            ∂t
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