Page 160 - Tunable Lasers Handbook
P. 160

140     Charles Freed

                   in  1984 [11 I] and  1985 [76], respectively. Here I can only give a few glimpses
                   into some of the findings.
                      In [76.111,112] we find anomalous blue shifts of CO,  absorptions with pres-
                   sure that were in the range of 40 to 90 kHz/Torr for the 626, 636, 828, and 838
                   CO,  isotopic species (see Table 1 of  [78] or [ 11 11). Figure 19 shows a sample of
                   the plots of typical pressure shift data sequences, all “blue” shifts, one for each of
                   the four  CO,  isotopic species that  were measured. Because  the CO,  pressures
                   used  in  the frequency  stabilization cells were  typically in  the  50 k- 15 mTorr
                   range, the implication is that there is a systematic 3.6 k 2.2 kHz frequency shift
                   that we chose to ignore when generating the predicted [37] absolute frequencies.
                   Our decision not to take into account pressure shift was based on the considera-
                   tions that follow.
                      The anomalous blue pressure shifts we measured could not be explained by
                   any of the theories that we explored [ 11 21 or that were suggested to us because
                   all of  them predict  red pressure  shifts. The pressure  shifts we  measured were
                   very small and necessitated the improvement of our experimental apparatus and
                   measurement technique well beyond what was available when most of our data
                   were gathered for the database given in Bradley et ill. [37].
                      Consistent and reproducible pressure shifts were only obtained after we ini-
                   tiated a new measurement technique in order to eliminate frequency-offset errors
                   caused by the nonzero slope of the power-versus-frequency characteristics of the
                   lasers over the frequency range of  the nonlinear saturation resonance dip. This
                   nonzero power slope is a universal problem in most stabilization schemes used
                   with lasers. Furthermore, this so-called “instrumental” frequency shift has a qua-
                   dratic dependence on pressure and may  easily dominate over the true pressure
                   shift at stabilization cell pressures greater than  about 60 mTorr. Moreover, the
                   sense of this “instrumental” frequency shift can be either red or blue, depending
                   on the adjustment of  the grating position in the CO, - laser as illustrated by  the
                   data shown in Fig. 20.
                      Figure  21  shows the  block  diagram  of  the  two-channel  line-center-stabi-
                   lized CO,  heterodyne laser system we used in our experiments for the purpose
                   of  determining  pressure  shift. This system  is  an expanded  version  of the  one
                   previously described in Fig. 13 and Sec. 8.
                      Comparison of  Figs. 21 and  13 will indicate the addition of  a power  slope
                   detection channel consisting of a relatively large AuGe detector (in order to detect
                   a portion of the entire combined beam cross section) and a phase-sensitive lock-in
                   amplifier. The power  slope signal is already present in the saturated absorption-
                   stabilized system shown in Fig. 21 since the PZT is dithered to recover the first
                   derivative of the 4.3-pm fluorescence signal. By synchronously detecting the laser
                   power output at 9 or  10 pm with an additional detector [a 0.3-cm-diameter gold-
                   doped germanium  detector in  our system), the slope of  the laser power can be
                   measured with a large degree of reliability. In our system the asymmetry in the res-
                   onant dip originates from the net  dispersive profile, and is the  sum total of  the
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