GPR / 910-709-5210

East Coast Underground offers GPR locating services to locate your underground utilities.  Ground-penetrating radar (GPR) is a geophysical method that uses radar pulses to image the subsurface.  This nondestructive method uses electromagnetic waves in the microwave band (UHF/VHF frequencies) of the radio spectrum, and detects the reflected signals from subsurface structures.  GPR can have applications in a variety of media, including rock, soil, ice, fresh water, pavements and structures.  In the right conditions, practitioners can use GPR to detect subsurface objects, changes in material properties, and voids and cracks 

GPR uses high-frequency (usually polarized) radio waves, usually in the range 10 MHz to 2.6 GHz. A GPR transmitter emits electromagnetic energy into the ground. When the energy encounters a buried object or a boundary between materials having different permittivities, it may be reflected or refracted or scattered back to the surface. A receiving antenna can then record the variations in the return signal. 

The electrical conductivity of the ground, the transmitted center frequency, and the radiated power all may limit the effective depth range of GPR investigation. Increases in electrical conductivity attenuate the introduced electromagnetic wave, and thus the penetration depth decreases.  Because of frequency-dependent attenuation mechanisms, higher frequencies do not penetrate as far as lower frequencies.  However, higher frequencies may provide improved resolution.  Thus operating frequency is always a trade-off between resolution and penetration.   Dry sandy soils or massive dry materials such as granite, limestone, and concrete tend to be resistive rather than conductive, and the depth of penetration could be up to 15-metre (49 ft).  In moist and/or clay-laden soils and materials with high electrical conductivity, penetration may be as little as a few centimetres.