1887
ASEG2012 - 22nd Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

Over the past decades, airborne electromagnetic (AEM) surveys have mostly been used in connection with mineral exploration and a variety of issues in hydrogeophysical mapping. However, increasingly, AEM is used for a wide range of geotechnical purposes: pollution mapping, geotechnical assessment on road and freeway alignments, bathymetry, and depth to bedrock.

We present an investigation using a helicopterborne transient electromagnetic system along the planned trace of a gas pipeline. Oil and gas pipelines are often buried at a depth of a few meters and the cost of construction depends critically on whether the subsurface is composed of soft sediments that can be easily excavated or hard rock formations that require much heavier equipment and possibly have to be blasted. The aim of the AEM survey was to distinguish between the soft, relatively conductive sediments and the hard, relatively resistive bedrock in the upper few meters of the subsurface.

Data were collected with a rather small transmitter moment, but a high repetition frequency that simultaneously allowed high acquisition speed, and reliable data quality. Measurements were inverted with 1D models with both vertical and lateral constraints to produce model sections along flight lines. A novel method of statistical analysis of the set of equivalent models for each inverted model, calibrated against boreholes, improved the estimates of the presence of hard rock along the flight lines.

Loading

Article metrics loading...

/content/journals/10.1071/ASEG2012ab225
2012-12-01
2026-01-13
Loading full text...

Full text loading...

References

  1. Auken E., Christiansen A.V., Westergaard J.H., Kirkegaard C., Foged N. and Viezzoli A. 2009. An integrated processing scheme for high-resolution airborne electromagnetic surveys, the SkyTEM system. Exploration Geophysics, 40, 184-192.
  2. Beard L. P. and Lutro O. 2000. Airborne geophysics and infrastructure planning - A case history. Journal of Environmental and Engineering Geophysics, 5, 1-10.
  3. Christensen N.B. 2002. A generic 1-D imaging method for transient electromagnetic data: Geophysics, 67, 438-447.
  4. Christensen N.B. and Tølbøll R.J. 2009. A lateral model parameter correlation procedure for 1D inverse modeling. Geophysical Prospecting, 57, 919-929.
  5. Christensen N.B., Reid J.E. and Halkjær M. 2009. Fast, laterally smooth inversion of airborne transient electromagnetic data. Near Surface Geophysics, 7, 599-612. doi: 10.3997/1873-0604.2009047.
  6. Hodges G., Rudd J. and Boitier D. 2000. Mapping conductivity with Helicopter Electromagnetic Surveys as an aid to planning and monitoring pipeline construction:Proceedings of the Symposium on the Applications of Geophysics to Engineering and Environmental Problems, Engineering and Environmental Geophysical Society, 47-56.
  7. Inman J.R. Jr., Ryu J. and Ward S.H. 1975. Resistivity inversion. Geophysics 38, 1088-1108.
  8. Menke W. 1989. Geophysical data analysis: Discrete inverse theory. Academic Press Inc.
  9. Pfaffhuber A.A., Grimstad E., Domaas U., Auken E., Foged N. and Halkjaer M. 2010. Airborne EM mapping of rockslides and tunnelling hazards: The Leading Edge, 29, 956-959.
  10. Serban D.Z. and Jacobsen B.H. 2001. The use of broadband prior covariance for inverse palaeoclimate estimation. Geophysical Journal International 147, 29-40.
  11. Sørensen K.I. and Auken E. 2004. SkyTEM - A new highresolution helicopter transient electromagnetic system. Exploration Geophysics, 35, 191-199.
  12. Tarantola A. 1987. Inverse problem theory, methods for data fitting and model parameter estimation. Elsevier, Amsterdam.
/content/journals/10.1071/ASEG2012ab225
Loading
  • Article Type: Research Article
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