Ground Penetrating Radar, also called GPR, is a non-destructive geophysical method capable of detecting most underground utilities, including concrete, fiberglass, transite, and plastic pipes that may not be detectable with conventional utility locating methods. In fact, GPR can be thought of as a subsurface imaging tool, offering solutions for many underground problems like subsurface voids, underground storage tanks, and more.

How Does GPR Work?

The Ground Penetrating Radar (GPR) equipment is mounted on a cart that is pushed along the surface of the ground that is being investigated. It transmits pulses of ultra high frequency radio waves down into the ground through a transducer or antenna. The transmitted energy is reflected back from various buried objects or distinct contacts between different dielectric properties of subsurface materials. An onboard antenna then receives the reflected radio waves, which are stored and interpreted in the digital control unit. This data makes up the final image, which is then reviewed and interpreted by the experts on the Master Locators team.

The end result is a constant profile or record of both metallic and non-metallic subsurface features without probing, digging, or drilling. This allows you to evaluate the location and approximate depth of buried objects, as well as investigate the presence and continuity of natural subsurface conditions and features.

Readable Depth

The readable depth is a function of the earth’s conductivity in the area tested, which is largely based on the materials that make up the area being investigated. The lower the conductivity, the deeper the depth of penetration. GPR waves can reach depths of up to 100 feet in low conductivity materials such as dry sand and granite. Clay, shale, and other high conductivity material may attenuate or absorb the radar signals, greatly decreasing the depth of penetration to 3 feet or less.

The type of GPR antenna will also determine the depth of penetration. Antennas with low frequencies from 25 to 200 MHZ obtain subsurface reflections from deeper depths, but have lower resolutions than higher frequency antennas. In addition to underground utilities, these low frequency antennas are used for investigating the geology of a site, such as for sinkholes or fractures, and also to locate large deep buried objects, such as underground storage tanks and septic tanks.