Airborne Gravity 2010 - Geoscience Australia

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Airborne Gravity 2010 Figure 3. Bouguer gravity anomaly values for the helicopter-mounted AIRGrav survey of the Podolsky Mineral Exploration Project (300 m resolution gravity data). Horizontal gravity components Six passes along a repeat line of about 95 km length were flown with the AIRGrav system installed in a Cessna Grand Caravan close to Alexandria, Ontario, with three passes made in each direction,. The test successfully demonstrated that the three spatial components of the gravity vector, or equivalently, the deflection of the gravity vector can be measured with high repeatability using the AIRGrav system and that the measured horizontal components agree well with geoid models of the highest order available. Data were processed using the enhanced procedure to extract the three gravity components, using AIRGrav data recorded at a 128 Hz rate and GPS data recorded using two aircraft receivers on different antennas, and a reference GPS ground station. Ambiguity between the orientations of the Inertial Navigation System (INS) and the Earth reference frames was resolved by relating the AIRGrav data to CGG05 model data. Bias and drift for the data acquired on each pass were removed using a simple linear fit to the CGG05 reference data. The mean value of the standard deviation of the agreement of the AIRGrav East component data with the mean AIRGrav data for the six repeat lines was 0.286 mGal whilst the value of this statistic for the North component data was 0.344 mGal. Profiles of the East component data for the six repeat lines are shown in Figure 4. The corrected mean AIRGrav East component data were compared to the East component gravity data calculated from two geoid models, the Canadian Gravimetric Geoid 2005 (CGG05; Huang and Véronneau, 2005) and the Canada HT2 geoid model (based on the CGG2000 geoid model; Véronneau, 2001) as well as to gravity components from the Earth Gravitational Model 2008 (EGM2008; Pavlis et al., 2008). Figure 5 shows the profile data and Table 1 lists the difference statistics. From these results, we can conclude that the AIRGrav system has a repeatability better than the agreement of its estimates with the model data. The consistency of the short wavelength data in the AIRGrav data shows greater detail than the model data. 175
Airborne Gravity 2010 Figure 4. Gravity East Component, Alexandria Repeat Line. Figure 5. AIRGrav mean East component vs Models. 176
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