Airborne Geophysics
Airborne geophysical systems have been in use since 1943.
They used magnetometers for geophysical mapping and detecting
submarines. The airborne electromagnetic systems came out in the
1950’s. These early devices were mounted on airplanes.
In the 1960’s these systems were applied to use with
helicopters.

Airborne geophysics utilizes several types of surveys to
accomplish their goals like airborne magnetic surveys,
electro-magnetic surveys, and radiometric surveys.
The three main airborne geophysics procedures are
magnetic, electromagnetic, and radioactive. These
airborne methods have a big impact on the mining industry. Better
geophysical tools, global positioning systems, and airborne
platforms have been useful in engineering and environmental
problems, though only to certain problems in these two areas of
endeavor.
Airborne geophysical surveys are also used for oil and
mineral exploration and land management. Airborne geophysical
methods have been used in detecting and mapping exposed bedrock.
But better methods are needed to explore natural aggregate
resources.
Magnetometer surveys map magnetic occurrences in the
earth’s magnetic field caused by magnetic minerals earth’s upper
crust. Electro-magnetic surveys are aimed at conducting a quick and
cheap search for metallic conductors. It is also applicable to
general geologic mapping and many engineering problems.
The radiometric surveys look for radioactive material in
rock.
Airborne geophysical surveys are used for land management
as in Western Australia where huge
parts of the farming land has been affected by soil salinity.
Geophysics has shown that topography and other factors are the
cause of the high salinity of the soil, according to The Bulletin
of the Australian Society of Exploration Geophysicists.
Airborne electromagnetic surveys are useful in
investigations of different geological eras. For instance, they can
help in locating subglacial valleys, which helps to understand
water reservoirs.
There are still many unanswered questions about the
geologic structure of Antarctica and
these questions may be answered by airborne geophysics. Maud Land
has proved that airborne geophysics is capable of helping to map
Precambrian Antarctica.
Antarctica plays a key role in climatic and
geodynamic history of the earth and again airborne geophysics can
help learn about this history and the climatic role involved and
how this data affect the whole earth.
Climate research is enhanced with airborne research,
specifically studying ice sheet and lithosphere interactions. They
do this by using multiple sensors. Scientist are trying to
determine how these two physical factors interact with each other
causing long-term climate variability. In these studies they use
ice-penetrating radar on long-range research aircraft.
They have to have special antenna structures that can
operate at 300 knots. They first tackled this problem in the 1970’s
working in Antarctica.
Airborne geophysics has the capability of being used for a
myriad of uses including mining, solving environmental problems,
engineering, land and water management, archeology, detecting
submarines, and many other scientific applications.
With global warming and other atmospheric problems it
seems that airborne geophysics can play a vital role in solving
them and making the world safer for everyone to live in and it can
help solve our energy problems.
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