1887
Volume 49, Issue 3
  • E-ISSN: 1365-2478

Abstract

GPR reflection energy varies with antenna orientation relative to the strike and dip of the reflector. This directional dependence of GPR responses was investigated through numerical experiments and was used to estimate the azimuth of fractures and joints. Three antenna configurations were considered in this study: perpendicular‐broadside (YY mode), parallel‐broadside (XX mode) and cross‐polarization (YX mode). The reflection energy in the cross‐polarization mode shows a shape characteristic similar to the strike, regardless of the dip angle. Those in the other two modes show quite different amplitudes from the strike, depending on the dip angle. We have developed a strike‐direction‐finding scheme using data obtained from the three different modes for the same survey line. The azimuth angle of each reflector was displayed in colour on the GPR profile. This scheme was applied to a field survey at a granite quarry in southern Korea. The GPR profiles showed different images of the reflectors depending on the antenna configuration. The estimated azimuths of reflectors obtained using our scheme matched fairly well with those of known fractures and joints.

Loading

Article metrics loading...

/content/journals/10.1046/j.1365-2478.2001.00262.x
2001-12-21
2024-04-24
Loading full text...

Full text loading...

References

  1. AnnanA.P., WallerW.M., StrangwayD.W., RossiterJ.R., RedmanJ.P., WattsR.D.1975. The electromagnetic response of a low‐loss, 2‐layer dielectric earth for horizontal electric dipole excitation. Geophysics40, 286–298.
    [Google Scholar]
  2. BalanisC.A.1982.Antenna Theory Analysis and Design. Harper & Row, Philadelphia.
    [Google Scholar]
  3. DavidC.N.1999. The directional dependence of the ground‐penetrating radar response on the accumulation zones of temperate Alpine glaciers. First Break17, 249–259.
    [Google Scholar]
  4. EnghetaN. & PapasC.H.1982. Radiation patterns of interfacial dipole antenna. Radio Science17, 1557–1566.
    [Google Scholar]
  5. GestelJ.V. & StoffaP.L.1999. Multi‐configuration ground‐penetrating radar data. 69th SEG meeting, Houston, USA, Expanded Abstracts, 540–543.
  6. HollowayA.L.1992. Fracture mapping in granite rock using ground probing radar. In: Ground Penetrating Radar (ed. J.Pilon ), pp. 85–100. Geological Survey of Canada.
    [Google Scholar]
  7. LehmannF., BoernerD.E., HolligerK., GreenA.G.2000. Multicomponent georadar data: some important implications for data acquisition and processing. Geophysics65, 1542–1552.
  8. MiwaT., SatoM., NiitsumaH.1999. Subsurface fracture measurement with polarimetric borehole radar. IEEE Transactions on Geoscience and Remote Sensing37, 828–837.DOI: 10.1109/36.752199
    [Google Scholar]
  9. RobertsR.L. & DanielsJ.J.1996. Analysis of GPR polarization phenomena. Journal of Environmental and Engineering Geophysics1, 139–157.
    [Google Scholar]
  10. SatoM. & MiwaT.2000. Polarimetric borehole radar system for fracture measurement. Subsurface Sensing Technology and Applications1, 161–174.
    [Google Scholar]
  11. SongY. & LeeK.H.1998. A wide‐band integral equation solution for EM scattering by thin sheets. 68th SEG meeting, New Orleans, USA, Expanded Abstracts, 436–439.
  12. TurnerG.1994. Modeling antenna–ground interactions. Proceedings of the 5th International Conference on Ground‐Penetrating Radar, Ontario, Canada, pp. 205–221.
  13. Van OvermeerenR.A.1994. High speed georadar data acquisition for groundwater exploration in the Netherlands. Proceedings of the 5th International Conference on Ground‐Penetrating Radar, Ontario, Canada, pp. 1057–1073.
  14. WeideltP.1981. Report on Dipole Induction by a Thin Plate in a Conductive Halfspace with an Overburden . Federal Institute of Earth Sciences and Materials.
http://instance.metastore.ingenta.com/content/journals/10.1046/j.1365-2478.2001.00262.x
Loading
/content/journals/10.1046/j.1365-2478.2001.00262.x
Loading

Data & Media loading...

  • Article Type: Research Article

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error