1887
ASEG2001 - 15th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Spectral component analysis is commonly applied to airborne gamma ray spectral data to reduce statistical noise in the measurements of potassium, uranium and thorium. This technique has been applied to continuous 5-second ground measurements with a portable gamma ray spectrometer using a 7.6 cm x 7.6 cm (3 inch x 3 inch) sodium iodide detector. The results have shown that the reduction in statistical noise is much greater than for large airborne detectors. Even with a short sampling time of 5-seconds, continuous ground measurements have practical significance for both geological mapping and mineral exploration.

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/content/journals/10.1071/ASEG2001ab048
2001-12-01
2026-01-25
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References

  1. Grasty, R.L., Holman, P.B. and Blanchard, Y.B., 1991, Transportable calibration pads for ground and airborne gamma ray spectrometers: Geological Survey of Canada Report 90-23.
  2. Grasty, R.L., Hovgaard, J. and LaMarre, J. 2001, Calibration of a 7.6 cm x 7.6 cm (3 inch x 3 inch) sodium iodide spectrometer for measuring air kerma rate: Radiation Protection Dosimetry (in press).
  3. Hovgaard, J. and Grasty R.L., 1997, Reducing statistical noise in airborne gamma ray data through spectral component analysis: Proceedings of Exploration 97: Fourth Decennial International Conference on Mineral Exploration. Toronto, 753-764.
  4. IAEA, 1989, Construction and use of calibration facilities for radiometric field equipment: Technical Report No. 309, International Atomic Energy Agency, Vienna, Austria.
  5. Minty, B., and McFadden, P., 1998. Improved NASVD smoothing of airborne gamma-ray spectra. Exploration Geophysics, 29, 516-523.
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