Ground Penetrating Radar is a revolutionary NDT survey technique to investigate the sub-surface. It is non-intrusive, detects metallic and non-metallic objects and voids, resolves construction layers and provides depth and thickness information.
Ground Penetrating Radar (GPR) is a geophysical survey method that uses pulses of electromagnetic radiation to image the subsurface. It provides a non-intrusive and non-destructive method of surveying the sub-surface. Ground penetrating Radar is a useful survey technique to investigate many materials including the ground, concrete, masonry, and asphalt.
A GPR transmitter emits pulses of electromagnetic energy into the subsurface. Changes in the sub-surface are detected based on differences in permittivities. When a change in the sub-surface is encountered, some of the electromagnetic energy is reflected back to the surface. This is detected by a receiving antenna and variations in the return signal are recorded. The information is displayed on a radargram.
Although Ground Penetrating Radar can detect changes in the sub-surface, it can’t determine their exact nature. Some features exhibit specific characteristics in the reflected wave pattern; for example, reflections from metallic surfaces have a high amplitude, while reflections from a void are reverse polarity. These help with identification of the detected features. However, in some cases, it may be necessary to supplement a Ground Penetrating Radar survey with absolute data from boreholes, sample cores, trial pits, etc.
Ground Penetrating Radar is a highly cost effective non-disruptive survey technique, offering a rapid means of obtaining subsurface information. Its many advantages include:
Ground Penetrating Radar (GPR) can effectively be used to locate and distinguish a wide variety of metallic and non-metallic materials. GPR works best when there is a big difference in the electromagnetic properties of the materials being surveyed. For this reason, metallic objects make ideal targets (e.g. reinforcement within concrete). Ground Penetrating Radar will however detect most materials providing there is a sufficient difference in the electromagnetic property between the target and surrounding material. Some of the more common target materials include:
Excavated areas, back-filled areas and any other ground disturbances can also be identified and mapped.
Ground Penetrating Radar will not work in certain ground conditions such as heavy clay soils, particularly if they are waterlogged. De-ionised water does not pose a problem to GPR, however water with a high mineral content (e.g. sea water) attenuates the signal making it an unsuitable medium. Ground Penetrating Radar is also unable to penetrate through metallic objects, including dense reinforcement.
The electrical conductivity of the scanned medium, the transmitted centre frequency, and the radiated power all influence the penetration depth.
An increase in electrical conductivity attenuates the GPR electromagnetic wave, resulting in a decrease in the penetration depth.
Higher frequencies provide a higher resolution; however, penetration depth is limited. Conversely a lower frequency provides greater penetration depth, albeit at a lower resolution. The choice of antennae frequency is dependent on the investigation objectives, including the width of survey path; for example, an antenna frequency of 400 MHz has a 0.3 m survey path width. Generally, it is advisable to use the highest frequency possible, although often it is necessary to scan with more than one frequency to provide the best results.
The following table shows examples of typical penetration depths achieved by different frequencies and potential application:
||Typical max. Penetration Depth
||Examples of Potential Use|
|2.6 GHz||0.3 m||Rebar mapping, structural concrete investigation|
|1.5 GHz||0.45 m||Reinforced concrete slabs, conduit detection|
|900 MHz||0.9 m||Pipe, detection, shallow soils, construction thickness|
|400 MHz||2 m||Utility surveys, shallow geology, buried object detection.|
Investigations can also be undertaken using lower frequency antennae (200 – 16 MHz). Maximum penetrations depths vary according the subsurface media but can reach as deep as 30 or 40 m. Examples of potential use include detection of groundwater tables, depth to bedrock, mapping of landfills and commercial assessment of sands and gravels in glacial landforms.
Contact us to find out more about Ground Penetrating Radar, its uses, and how it could help you:
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