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The Clapp Circuit A variation of the Colpitts oscillator makes use of series resonance, instead of parallel resonance, in the tuned circuit Otherwise, the circuit is basically the same as the parallel-tuned Colpitts oscillator Figure 24-15 is a schematic diagram of a series-tuned Colpitts oscillator circuit that uses an NPN bipolar transistor This circuit is also known as a Clapp oscillator Its frequency won t change much when high-quality components are used The Clapp oscillator is a reliable circuit It isn t hard to get it to oscillate and keep it going Another advantage of the Clapp circuit is that it allows the use of a variable capacitor for frequency control, while accomplishing feedback through a capacitive voltage divider Getting the Output In the Hartley, Colpitts, and Clapp oscillators just described and shown in Figs 24-13 through 24-15, the output is taken from the emitter or source, not from the collector or drain There s a reason for this The output of an oscillator can be taken from the collector or drain, just as is done in a common emitter or common-source amplifier to get maximum gain But in an oscillator, stabil-

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Consider a stationary vehicle that is nominally level and at rest at 45 degrees north latitude This results in eigenvalues of 00 00 72722 10 5 j 00 12915 10 3 j 00 ( s + e sin( )) j 00 11886 10 3 j 00 ( s e sin( )) j where j = 1 The close proximity of the second two eigenvalue pairs results in solutions containing an oscillation (approximately) at the Schuler frequency g (1191) s = Re with amplitude modulated2 (approximately) at the Foucault frequency f = e sin( ) (1192)

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The period of the Schuler oscillation is 844 minutes At the latitude of the simulation, the period of the Foucault beat is 339 hrs Figure 113 shows the response of the error state of the stationary INS with F de ned by eqn (1190) when the initial state error is 10 m of s north velocity error The initial north velocity error directly causes east tilt error due to error in the calculation of the Earth relative navigation frame angular rate; east velocity error due to error in Coriolis compensation; and, latitude error by direct integration All ve of the error states that are plotted attain a steady-state oscillation that is dominated by the Foucault modulated Schuler oscillation Due to the simulation occurring at latitude 45 degrees north, the north tilt and azimuth errors have equal magnitudes In general, the F matrix (fourth column, fth and seventh rows) of eqn (1190) indicates that the east velocity error will cause the azimuth error to be greater than the north tilt error by a factor of tan( ) The solution of the reduced error model from this same initial condition was considered in eqn (1185) The response for the reduced order system of eqn (1185) matches the full system response of Figure 113 well for approximately one hour, including the predicted peak errors for the north position and east tilt errors Figure 114 displays the error trajectory for the case of a one degree initial tilt about the east axis The east tilt error directly causes error in the gravity and earth rate compensation, which results in azimuth, north tilt and north velocity errors As predicted by eqn (1186), the initial rate of north position error is g 0 t2 m This estimate is valid for the rst 2 several minutes

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ity is more important than gain The stability of an oscillator is better when the output is taken from the emitter or source, as compared with taking it from the collector or drain Variations in the load impedance are less likely to affect the frequency of oscillation, and a sudden decrease in load impedance is less likely to cause the circuit to stop oscillating To prevent the output signal from being short-circuited to ground, an RF choke (RFC) is connected in series with the emitter or source in the Colpitts and Clapp oscillator circuits The choke lets dc pass while blocking ac (just the opposite of a blocking capacitor) Typical values for RF chokes range from about 100 H at high frequencies, such as 15 MHz, to 10 mH at low frequencies, such as 150 kHz

0 -1000 2000 0 -2000 001 0 -001 001 0 -001 001 0 -001

Figure 113: Numeric solution of eqn (1188) with F from eqn (1190) showing the error response for a stationary INS initialized with 10 m of north s velocity error

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