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9 - Ground-penetrating radar

Published online by Cambridge University Press:  05 April 2013

Mark E. Everett
Affiliation:
Texas A & M University
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Summary

While seismic-reflection and -refraction techniques are commonly employed to map near-surface layers, they do not have the high vertical resolution (detection of subsurface structures with length scales of 1.0 m or less) that is required for many applications. Ground-penetrating radar (GPR) can be a suitable geophysical tool in these situations. The technique is used to detect changes in subsurface electromagnetic impedance via the propagation and reflection at impedance boundaries of an electromagnetic wave generated by a transmitter deployed at the surface or, less commonly, within a borehole. Typical GPR frequencies are in the 10 MHz to 1 GHz range, much higher than the frequencies used in the electromagnetic (EM) induction method (see Chapter 8). The popularity of GPR as a near-surface geophysical technique lies partially in the similar appearance of radar sections to the seismic sections that are familiar to many geophysicists (Figure 9.1). Both seismic reflection and GPR are imaging techniques based on wave-propagation principles but there are important differences; these will be discussed in this chapter. Good overviews of the theory and practice of GPR appear in Davis and Annan (1989), Knight (2001), Neal (2004), Annan (2009), and Conyers (2011).

Example. Perchlorate transport in karst.

The occurrence of the perchlorate ion ClO4− in groundwater presents a great risk to human health since perchlorate has long been known to inhibit proper functioning of the thyroid. Beneath the Naval Weapons Industrial Reserve Plant (NWIRP) in central Texas, significant concentrations of perchlorate ions derived from the manufacture of rocket propellant have been detected in groundwater and springs. Hughes (2009) has described a wide-area (~ 500 ha) GPR survey in karst terrain with the goal of mapping subsurface structural features that might be indicative of major pathways for subsurface transport of perchlorate ions. The survey was executed by towing a 50 MHz GPR system for ~ 100 line-km on a sled behind an all-terrain vehicle.

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Publisher: Cambridge University Press
Print publication year: 2013

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  • Ground-penetrating radar
  • Mark E. Everett, Texas A & M University
  • Book: Near-Surface Applied Geophysics
  • Online publication: 05 April 2013
  • Chapter DOI: https://doi.org/10.1017/CBO9781139088435.010
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  • Ground-penetrating radar
  • Mark E. Everett, Texas A & M University
  • Book: Near-Surface Applied Geophysics
  • Online publication: 05 April 2013
  • Chapter DOI: https://doi.org/10.1017/CBO9781139088435.010
Available formats
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To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

  • Ground-penetrating radar
  • Mark E. Everett, Texas A & M University
  • Book: Near-Surface Applied Geophysics
  • Online publication: 05 April 2013
  • Chapter DOI: https://doi.org/10.1017/CBO9781139088435.010
Available formats
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