Technique for correcting for overburden effects in ground level radiometric surveys of uranium ore bodies

Geophysics ◽  
1979 ◽  
Vol 44 (1) ◽  
pp. 89-98 ◽  
Author(s):  
B. L. Dickson ◽  
G. J. Clark ◽  
B. J. McGregor

An experimental study of the effect of barren overburden on the gamma‐ray spectrum of uranium ore has been made. This has shown that counts in either of the two energy windows 0.56 to 0.64 MeV or 0.66 to 1.01 MeV may be used to correct for the decrease in total count rate as a result of overburden. The correction is limited to an overburden thickness‐density product of approximately [Formula: see text], which is equivalent to a correction factor of 16. Theoretical spectra have been modeled for a geometry similar to that used in the experiment and agree in the changes in spectral shape with overburden thickness. The calculations have also been used to evaluate the effects of ore thickness and to determine the useful limits of the correction factors. The method is mainly applicable to a mining environment where sufficiently high count rates exist.

2019 ◽  
Vol 151 ◽  
pp. 196-206
Author(s):  
M.E. Hammad ◽  
H. Kasban ◽  
R.M. Fikry ◽  
Moawad I. Dessoky ◽  
O. Zahran ◽  
...  

2018 ◽  
Vol 89 (10) ◽  
pp. 10I116 ◽  
Author(s):  
D. Rigamonti ◽  
A. Broslawski ◽  
A. Fernandes ◽  
J. Figueiredo ◽  
L. Giacomelli ◽  
...  

2013 ◽  
Author(s):  
T. Petrovič ◽  
M. Vencelj ◽  
M. Lipoglavšek ◽  
R. Novak ◽  
D. Savran

Geophysics ◽  
1980 ◽  
Vol 45 (2) ◽  
pp. 292-311 ◽  
Author(s):  
John G. Conaway ◽  
Quentin Bristow ◽  
Patrick G. Killeen

In gamma‐ray logging for uranium exploration and evaluation, many factors affect the accuracy of the final processed log. This paper presents the results of a study of various logging and data processing parameters over which the logger can exercise control. These include probe velocity, sampling interval, detector length, and, in the case of analog recording, ratemeter time constant and chart paper depth scale. Numerous replications of gamma‐ray logs past the same sequence of radioactive zones varying one logging parameter at a time, combined with theoretical considerations, lead to some useful conclusions regarding the effects of those parameters on the accuracy and resolution of the logs, and the efficacy of deconvolution techniques under various conditions. In general, digital recording is preferable to analog recording because, with the latter, the accuracy of the computed grade‐thickness product can suffer as a result of the extra steps of converting count rate to an analog chart record and back again to digital form for processing. In the case of digital gamma‐ray logging for uranium, it appears that it is less important to log slowly for good statistical accuracy than it is to use a small sampling or digitization interval. Under the high count‐rate conditions encountered in uranium logging, the factors limiting the accuracy of the log are likely to be detector length (which limits spatial resolution) and geologic noise (e.g., inhomogeneities in the rock); logging more slowly does not remedy these problems. In cases where the recorded gamma‐ray flux is low, such as in lithologic correlation, it may still be necessary to log very slowly to achieve acceptable statistical reliability.


Author(s):  
Stefan Korolczuk ◽  
Slawomir Mianowski ◽  
Jacek Rzadkiewicz ◽  
Pawel Sibczynski ◽  
Lukasz Swiderski ◽  
...  

2011 ◽  
Vol 17 (S2) ◽  
pp. 1192-1193 ◽  
Author(s):  
F Eggert ◽  
T Elam ◽  
R Anderhalt ◽  
J Nicolosi

Extended abstract of a paper presented at Microscopy and Microanalysis 2011 in Nashville, Tennessee, USA, August 7–August 11, 2011.


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