GROUND PENETRATING RADAR
THE METHOD Ground penetrating radar
(GPR) provides a high resolution, cross-sectional image of the shallow
subsurface. A short pulse of electromagnetic energy is radiated downward.
When this pulse strikes an interface between layers of material with
different electrical properties, part of the wave reflects back, and
the remaining energy continues to the next interface. Depth measurements
to interfaces are determined from travel time of the reflected pulse and
the velocity of the radar signal.
EQUIPMENT NAEVA Geophysics operates three
GPR systems:
FIELD PROCEDURES The GPR method provides a very rapid means of non-intrusive data collection. The system is most commonly moved along the surface at a consistent pace as data are collected continuously along profiles. The depth at which a feature can be imaged is largely dependent on subsurface material type (resistive versus conductive). With prior knowledge of expected subsurface materials and clearly defined objectives, an experienced operator can optimize data collection parameters to compensate for less than ideal geologic environments. The Conquest and Noggin generate real-time images on a LCD, which can later be uploaded to a computer. The Pulse Ekko 100 is a fully digital system, which allows for a great deal of post collection processing. The data are presented as cross-sectional profiles in wiggle trace, color fill, or gray scale format. To carry processing further, the data can be formatted for importation into a variety of commercial processing programs including 3-D visualization packages. |
The EKKO 100 is extremely versatile with the electronics mounted to a backpack and the antennae attached to a sled or a large-wheeled cart with an integrated odometer.
Sensors & Software Noggin 250 GPR used to aid in the detection of subsurface utilities and other targets.
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