Page 244 - Phase Space Optics Fundamentals and Applications
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Radiometry, Wave Optics, and Spatial Coherence     225


                 The stationary phase approximation is carried out on the phase
               function

                                                               2
                                                          2
                    
( p, q) = px + qy + mz = px + qy + z  1 − p − q .  (7.25)
                 The direction cosines ( p, q) are chosen to make the first partial
               derivatives of 
( p, q) equal to zero. These values are substituted in
               the second partial derivatives of the phase function, and the higher-
               order terms are neglected. This approximated phase function is used
               in the evaluation of the double integral of Eq. (7.24). Alternatively, it
               is simpler to substitute the values of ( p, q) in the formula given in
                            2
               Born and Wolf, Eq. (20) of Section 3 on double integrals, contained in
               Appendix III, entitled “Asymptotic Approximations to Integrals.”
               This procedure leads to the following expression for the diffracted
               field. 6
                            −i z exp (ikr)
                   (x, y, z) =
                               r    r

                                                  2      xx s + yy s
                            ×      (x s ,y s , 0) exp −i         dx s dy s
                                                         r
                               A
                                                                    (7.26)

                 The form of this expression suggests that we can rewrite it in the
               form

                  ( r,  ) =  (r, p, q,  )
                          −i  exp (ikr)
                       =    m
                                  r

                                                2
                         ×       (x s ,y s , 0) exp −i  ( px s + qy s ) dx s dy s (7.27)

                             A
                 Here, we have used the direction cosines p = x/r, q = y/r, and
               m = z/r.
                 The diffracted field on a hemisphere is simply the spatial Fourier
               transform of the field distribution in the aperture as long as the dis-
               tance r to the observation point satisfies the far-field condition
                                              2 2
                                            2m a
                                       r >>                         (7.28)

                 In this expression m = z/r = cos   which is the third direction co-
               sine. The symbol a is the radius of the aperture. The z axis is perpen-
               dicular to the aperture plane and   is measured from the z axis.
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