In Ground Penetrating Radar (GPR) surveys, electromagnetic waves of frequencies between 50MHz and 2.6GHz are transmitted into the ground or structure. The transmitted energy is reflected back to the surface when it encounters significant contrasts in dielectric properties (e.g. changes in ground conditions).
With the wide range of antennas available, GPR can be applied to numerous geological, environmental and engineering applications with investigation depths from a couple of centimetres to up to ~10m bgl. The data can be collected as a series of 1D soundings, 2D traverses, or in more complex situations as a 3D volume. With this dynamic versatility, the GPR technique can be applied in a wide variety of circumstances.
For utility detection, GPR offers a reliable way to locate services that cannot be located by traditional methods (e.g. non-metallic pipes). The data acquired from GPR can be observed in real-time, displaying a 2D profile of the near-surface, which can help us understand features in the near-surface and can aid in making an engineering judgement based on the experience of the user.