Charles R. Wilson, John V. Olson and Dan Osborne
Geophysical Institute, University of Alaska Fairbanks
The calibration constant is a dimensionless number that depends on the ambient
atmospheric pressure. When the value of the ambient pressure is multiplied by the
calibrator calibration constant, one obtains the peak-to-peak calibration sinusoid signal
amplitude. The average values of the calibration constants of the UAF calibrator units # 2
and # 3 were found to be:
Unit # 2: Cal. Const. = 1.328E (-5)
Unit # 3: Cal. Const. = 1.331E (-5)
Stastical studies were made with the UAF calibrators to determine the repeatability of
measurements under both laboratory and field conditions at several different frequencies.
The results were consistent to within 5% across all microphones.
Dynamical calibrations were also made of the French MB-2000 sensor, over the frequency range from 0.02 to 1.5 Hz, with the UAF calibrator using an adaptor especially designed for this purpose. The results will be shown.
Finally, experiments were performed using the step-impulse function of the UAF calibrator in order to assess whether the step-impulse could be used in the field to determine the system response function. Impulse responses for both the Chaparral # 5 and the MB-2000 sensors were measured. The purpose of these experiments is to determine if the impulse-mode function can be used in the field with the UAF calibrator to assess the system response function.