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62   Chapter Four

        At a location in the system where we know the data of all three rays,
        we can determine the scaling constants by a simultaneous solution of
        Eqs. 4.20 and 4.21, and get

                           A   ( y u   u y )/(u y   y u )           (4.22)
                                 3  2   3 2  2 1    2  1
                           B   ( u y   y u )/(u y   y u )           (4.23)
                                 3 1   3  1  2 1    2  1
        Typically, the axial and principal rays are chosen as rays 1 and 2. The
        third ray is often defined in object space, although it may be defined any-
        where in the system where the data of all three rays are known. The
        scaling factors A and B are calculated from Eqs. 4.22 and 4.23. Then,
        after putting these values for A and B into Eqs. 4.20 and 4.21, the data
        of ray 3 in image space can be found by inserting the image space data
        of rays 1 and 2 into the resulting equations. (Assuming that the data of
        ray 3 in image space is what is desired.)



        Focal length determination
        For example, if we have the raytrace data for the axial ray #1 and
        oblique ray #2 and define ray 3 as having u   0 and y   1 in object
                                                 3          3
        space, Eqs. 4.20 and 4.21 can give us the final ray height and slope  in
        image space for ray 3. Then, with the primed data (y′ and u′) indicat-
        ing the values in image space, we get:
                    efl   1/u ′   (y u   u y )/(u u ′   u u ′)      (4.24)
                             3       1  2  1 2   1  2   2  1
                   bfl   y ′ /u ′    (u y ′   u y ′)/(u u ′  u u ′)  (4.25)
                           3   3      2  1    1 2   1  2  1  1
        If we reverse the whole process and set u ′   0 and y ′ = 1, we can get
                                               3         3
        the (normally negative) front focal length
                      ffl   y /u    ( u ′y )/(u u ′   u u ′)        (4.26)
                              3  3        2  1  1  2   2  1


        Formula for two specific rays
        The above formulas are perfectly general. If we select certain rays to
        trace, a simplified expression can often be derived. For example, the
        OSLO reference manual gives the following variation on this scheme:
        If we start ray #1 at the foot of the object, and have it strike the first
        surface at y 1 ≡ y 3 , and if we start ray #2 at height h on the object and
        send it through the center of the first surface, then the ray coordinates
        in object space (i.e., at the object) are:
          for ray #1:  y 1   0 and u 1   y 3 /s,
          for ray #2:  y 2   h and u 2   h/s
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