PARSAN Geophysics

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Ground Penetrating Radar

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Ground Penetrating Radar, also known as GPR, Georadar, Subsurface Interface Radar, Geoprobing Radar, is a totally non-destructive technique to produce a cross section profile of subsurface without any drilling, trenching or ground disturbances. Ground penetrating radar (GPR) profiles are used for evaluating the location and depth of buried objects and to investigate the presence and continuity of natural subsurface conditions and features.

Basic Principle

The GPR operates by transmitting electromagnetic impulses into the ground through transmitter antenna. The transmitted energy is reflected from various buried objects or distinct contacts between different earth materials, across which there is a contrast in dielectric constant. The antenna then receives the reflected waves and displays them in real time on screen. Data is also saved in appropriate memory for later processing and interpretation.

Ground penetrating radar waves can reach depths upto 60 meters in low conductivity materials such as dry sand or granite. Clays, shale and other high conductivity materials may attenuate or absorb GPR signals, greatly decreasing the depth of penetration.

The depth of penetrating in also determined by the GPR antenna used. Antennas with low frequency obtain reflections from deeper depths but have low resolution. These low frequency antennas are used for investigating the geology of a site, such as for locating sinkholes or fractures, and to locate large, deep buried objects.

Antennas with higher frequencies (300 to 2000 MHz) obtain reflections from shallow depths (0 to 10 meters) and have a high resolution. These high frequency antennas are used to investigate surface soils and to locate small or large shallow buried objects, pipes, cables and rebar in concrete.

GPR can detect objects of any material, metallic or non-metallic.

Application Areas

  • Geological and hydro-geological investigations including mapping of bedrock topography, water levels, solution features, glacial structures, soils and aggregates.
  • Engineering investigations to evaluate dams, sea walls, tunnels, pavements, roadbeds, railway embankments, piles, bridge decks, river scour, buildings and monuments.
  • Location and evaluation of buried structures including utilities, foundations, reinforcing bars, cavities, tombs, archaeological artifacts, and animal burrows.
  • investigations: location of buried engineering structures and underground storage tanks.
  • Subsurface mapping for cables, pipes and other buried structures prior to trench-less operations.

Advantages

  • Rapid ground coverage - Antenna towed either by hand or from a vehicle.
  • High-resolution coverage of the survey area, detecting even small objects.
  • On-site interpretation possible due to instant graphic display.

Limitations

  • Data acquisition may be slow over difficult terrain.
  • Depth of penetration is limited in materials with high electrical conductivities, clays.
  • Energy may be reflected and recorded from aboveground features, walls, canopies, unless antennae are well shielded.
  • Artifacts in the near surface (reinforcing bars, boulders, components of made ground) may scatter the transmitted energy and complicate the received signal and/or reduce depth of penetration.
  • Working on principle of reflection, GPR detects the utilities and provides information on depth and location. Classification. of utility any further can be done only with availability of background data and is not a deliverable of GPR survey.