Optimization of gamma‐ray logging techniques for uranium

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.

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

Author(s):  
Narasimman Sundararajan ◽  
Bernhard Pracejus ◽  
Salah Al- Khirbash ◽  
Talal Al-Hosni ◽  
Ala Ebrahimi Ebrahimi ◽  
...  

The Proterozoic basement of the Dhofar region of the Sultanate of Oman might be considered as a potential source of Uranium mineralization like other Proterozoic basins of the world, which collectively contribute 30%-40% to the global production.  Uranium exploration assumes great importance in this part of the world and therefore geochemical and geophysical exploration for Uranium was initiated.  Initial, random sampling of the study area with Gamma ray spectrometry as well as in situ XRF (Xray Florescence) analysis indicated the presence of   around 30-40 ppm of Uranium. Since Gamma ray spectrometry results in the calculation of the heat produced during radioactive decay of Potassium (K), Uranium (U) and Thorium (Th) within the rocks in the study area, measurements were acquired along eleven traverses of varying length from 100-250 m at a traverse interval of 20 m and sampling interval of 10 m. Individual plots of the concentrations  of radioelements such as U, K and Th have shown favorable anomalous radioactive sources. Besides this, Uranium to Thorium (eU/eTh) and Uranium to Potassium (eU/K) ratio plots have been presented and the alteration zones associated with Uranium mineralization through all traverses have been identified. Further, the generated composite ternary image based on the combination of K, Th and U from Gamma ray spectrometry determines different relative amounts of radioelements and paves the way for deciphering the level of radioactivity in the study area. However, there seems to be no presence of strong Uranium anomalies in the near surface of the limited study area. As the study area is heavily faulted, the depth to concealed  subsurface fault structures  is  estimated to be around  64 m based on Hartley spectral analysis of total magnetic anomaly (line-6). 


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.


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

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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