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Electrical
Resistivity
Seismic Refraction
ReMi Shear Wave
Magnetics
Electromagnetics
Gravity
Downhole Seismic
CSL
Marine Geophysics
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THE GROUND PENETRATING RADAR (GPR) METHOD
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The GPR method provides information which can be used
to help determine:
 | The location and depth of metallic and
non-metallic buried objects such as voids, utilities, pipes, drums, tanks,
cables and boulders |
 | The presence of rebar in concrete |
 | The extent of
contaminant plumes |
 | The location of archaeological sites |
 | The condition
of brick, masonry and concrete structures |
 | The condition
of sub-grades beneath roads, railroad tracks, and runways |
 | The boundaries of buried landfills and trenches |
 | Depth and thickness of soil strata on land and under fresh water |
 | Bedrock topography |
 | Depth to the water table |
In a GPR survey, high frequency (10 MHz to 3,000 MHz)
electromagnetic (EM) pulses are used to detect changes in EM properties
(dielectric permittivity, conductivity and magnetic permeability) as a function
of depth.
Energy is propagated into the ground from a transmitting antenna and is
reflected back to a receiving antenna from subsurface boundaries at which there
are EM property contrasts. As the antennas are moved along the survey line, a
series of scans are collected and positioned side by side to form a profile of
the subsurface.
The lateral resolution of a GPR survey depends upon the
spacing of the GPR profiles and the rate at which data is collected along the
profile. The vertical resolution of the technique is a complex function of the
amplitude and wavelength of the EM pulse, the propagation characteristics of the
host material and the target, the complexity of the geology, noise from manmade
and natural sources, and the depth shape and size of the target. Typically,
vertical resolution of a few centimeters can be obtained with high frequency
antennas (1 GHz) at depths of less than one meter, while lower frequency
antennas (10 MHz) may have a resolution of a meter or so at depths to over fifty
meters. Penetration depths of 5,000 meters have been achieved under certain
conditions such as polar ice or salt deposits.
The GPR method is limited to areas which do not contain
high conductivity soils, or sediments which are saturated with salt water or
other highly conductive fluids.

Example of GPR Data
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