1887
Volume 4, Issue 1
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

The effect on stripping factors of the air between aircraft and ground can be determined by counting at various altitudes over pure sources of uranium and thorium. One published set of spectra from a small crystal indicates that stripping factors vary with altitude, and ground determined values are probably too low at 100 metres altitude. The ability of various window systems to separate uranium and thorium series radiation differs, even for identical crystal volumes and ideal conditions. The systems can be compared if complete calibration is available. The narrow window systems are most precise and in addition they offer practical advantages because they are highly specific for the radiation from natural radionuclides.

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/content/journals/10.1071/EG973131
1973-03-01
2026-01-14
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References

  1. DOIG, R., 1968: The natural gamma ray flux, in-situ analysis Geophysics, v.33, pp.311-328.
  2. GRASTY, R. L. and A. G. DARNLEY, 1971: Calibration of gamma ray spectrometers for ground and airborne use. Geol. Surv. Canada Prof. Paper 71-17.
  3. GREGORY, A. F. and J. L. HORWOOD, 1965: A spectrometric study of the attenuation in air of gamma rays from mineral sources Canada, Dept. Mines & Tech. Surveys, Mines Branch Res. Rep. R110.
  4. KILLEEN, P. G. and C. M. CARMICHAEL, 1970: Gamma ray spectrometer calibration for field analysis of thorium, uranium and potassium. Can. J. Earth Sciences, v.7, pp.1093-1098.
  5. LANCZOS, D., 1961: Linear differential operators. Van Nostrand, London.
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  • Article Type: Research Article

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