Ground Penetrating Radar
Ground penetrating radar (GPR, sometimes
called ground probing radar, georadar or earth sounding radar) is a noninvasive
electromagnetic geophysical technique for subsurface exploration, characterization
and monitoring. It is widely used in locating lost utilities, environmental
site characterization and monitoring, agriculture, archaeological and forensic
investigation, unexploded ordnance and land mine detection, groundwater,
pavement and infrastructure characterization, mining, ice sounding, permafrost,
void and tunnel detection, sinkholes, subsidence, karst, and a host of
other applications. It may be deployed from the surface by hand or
vehicle, in boreholes, between boreholes, from aircraft and from satellites.
It has the highest resolution of any geophysical method for imaging the
subsurface, with centimeter scale resolution sometimes possible.
Resolution is controlled by wavelength
of the propagating electromagnetic wave in the ground. Resolution
increases with increasing frequency (shorter wavelength). Depth of
investigation varies from less than one meter in mineralogical clay soils
like montmorillonite to more than 5,400 meters in polar ice. Depth
of investigation increases with decreasing frequency but with decreasing
resolution. Typical depths of investigation in fresh-water saturated,
clay-free sands are about 30 meters. Depths of investigation (and
resolution) are controlled by electrical properties through conduction
losses, dielectric relaxation in water, electrochemical reactions at the
mineralogical clay-water interface, scattering losses, and (rarely) magnetic
relaxation losses in iron bearing minerals. Scattering losses are
the result of spatial scales of heterogeneity approaching the size of the
wavelength in the ground (like the difference between an ice cube and a
snowball in scattering visible light). Detectability of objects in
the ground depends upon their size, shape, and orientation relative to
the antenna, contrast with the host medium, as well as radiofrequency
noise and interferences. This is representative but greatly oversimplified,
see: http://www.g-p-r.com GPGN520
Copyright 1998-1999 by Gary R. Olhoeft. All Rights
Reserved.