
Airborne Gravity with AIRGrav
Sander Geophysics Limited (SGL)
offers airborne gravity surveys using our Airborne Inertially Referenced
Gravimeter - AIRGrav. SGL´s AIRGrav is the only purpose-built airborne gravimeter, and was designed specifically
for the unique characteristics of the airborne environment. This design
approach has resulted in a superior gravity instrument which can be flown in
an efficient survey aircraft during normal daytime conditions. In addition,
AIRGrav can easily be flown in combination with magnetic and/or radiometric
instruments to increase the survey benefits. AIRGrav was
designed primarily for petroleum exploration, where it is an economical
alternative to ground and shipborne surveys. AIRGrav also
has exciting application in regional geophysics, mineral exploration and
geodesy.
The AIRGrav system
includes an all new gravimeter on a three-axis inertially stabilized
platform, combined with high resolution Differential GPS (DGPS) to correct
for aircraft movements due to turbulence, aircraft vibrations and drape flying. The gyro
stabilized inertial platform makes the gravimeter much less affected by horizontal accelerations than other
systems, which use modified sea gravimeters. This allows AIRGrav to
achieve consistently higher resolution. The AIRGrav system
is currently available to fly fixed-wing or helicopter surveys.
Terrain corrections are performed using either an existing digital terrain model or terrain data
acquired in the course of the gravimetric survey. Digital terrain models can be supplemented
with remote sensing data if required, depending on the nature of the terrain and the resolution
of the survey. Terrain corrections for airborne gravity surveys are in some ways easier than
ground surveys because airborne gravity does not require near station corrections, and is not susceptible
to errors due to anomalous densities near a gravity station.
Production surveys have been
flown under a variety of conditions including offshore, at a constant
altitude over rolling terrain, and with a loose drape over high mountains
(>3,000 m). Because the system is relatively tolerant of turbulence, it
works well on drape surveys and in moderate to severe turbulence.
Sander Geophysics recently completed a combined gravity and magnetic survey in the
Turner Valley area, south of Calgary, Canada. The map above shows the first vertical
derivative of the terrain corrected Bouguer
gravity with the shadow of the first vertical derivative of the total
magnetic intensity. The data set consists of over 12,000 lkm of data flown
on 250 m spaced east-west lines, and 1,000 m north-south lines. The extent of
the data set is 60 km from north to south. Noise was calculated to be 0.3
mGal. Gravity anomalies of less than 2 mGal can be seen clearly on the data
set and correlate well with known oil and gas fields.
Results from numerous AIRGrav
surveys have been rigorously analyzed to determine system performance and
optimum processing parameters. The graph below shows rms gravity
noise plotted against filter length (20 s = 1 km). The graph shows that the
noise level drops off quickly as the filter length increases, which
indicates that noise is concentrated in the higher frequencies. The graph
also clearly illustrates the relationship between accuracy and resolution,
and how one can be traded off against the other depending on the client´s
objectives.

The following graph demonstrates the effect of averaging a number of lines (a process which
is similar to stacking seismic data), which can be achieved by flying
closely spaced lines and applying a filter with a wavelength longer than the
line spacing. The graph shows rms gravity noise plotted against the number
of lines averaged, for various filter lengths. Using this procedure, the
final grid data will have a noise level significantly lower than the
individual profile data.
Shown below are typical AIRGrav survey
parameters. As described above, the accuracy and resolution of the gravity
data depends on the aircraft speed and the line spacing.
| Accuracy RMS (mGal) |
Resolution ½ sine wave (m) |
Aircraft |
Velocity (kt) |
Line Spacing (m) |
Production Rate (km/day) |
| 0.2 |
4,000 |
fixed-wing |
120 |
1000 |
500 |
| 0.2 |
2,200 |
fixed-wing |
95 |
300 |
150 |
| 0.2 |
1,100 |
helicopter |
50 |
200 |
100 |
| 0.2 |
700 |
helicopter |
35 |
50 - 100 |
30 |
AIRGrav services include survey planning, data acquisition, preliminary
processing in the field, final data processing to terrain corrected Bouguer gravity and a
comprehensive technical report. SGL also offers integrated interpretation of
AIRGrav, aeromagnetic and other data sets.
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