SOIL SURVEYS
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August 2, 1990
Courtesy of NASA BBS at 205 895-0028
SOIL SURVEYS
Accurate soil surveys are necessary for soil conservation
measures, determining building sites, selecting park locations,
siting sewage plants and a variety of other reasons.
The traditional method of surveying requires auger boring into the
ground to obtain subsurface soil samples for classification, a slow
and fatiguing process since a typical survey might require hundreds
of depth measurements.
The U.S. Department of Agriculture's Soil Conservation Service
(SCS) is now employing an easier and faster method, developed in
cooperation with NASA, that involves use of ground penetrating radar
to produce subsurface graphs for interpretation by soil scientists.
The radar antenna is pulled by a four-wheel-drive vehicle along a
transect line, a straight line across the surface where normally
many borings would be made.
As it moves along the transect line at about five miles per hour,
the antenna transmits radio waves downward that are reflected back
to the antenna when they strike layers--soil, rock, water, man-made
objects--of different electromagnetic properties.
The antenna relays the reflected pulses to a graphic recorder
mounted in the vehicle. The system analyzes the data and produces
images on the recorder of subsurface "interfaces", areas where two
different types of features meet.
Soil scientists examine the recorder's printout. The information
does not entirely eliminate the need to dig holes, but only a few
are required to double-check the radar's findings.
The radar can penetrate to depths of seven to eight feet
routinely; in some types of soil it can reach 30 feet or more.
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