scholarly journals X-Ray Fluorescence Capabilities for Uranium Ore Analysis

1978 ◽  
pp. 51-58 ◽  
Author(s):  
K. K. Nielson ◽  
N. A. Wogman ◽  
R. L. Brodzinski
Keyword(s):  
X Ray ◽  
Author(s):  
A. Alsecz ◽  
J. Osa´n ◽  
J. Pa´lfalvi ◽  
I. Sajo´ ◽  
Z. Ma´the´ ◽  
...  

Uranium ore mining and milling have been terminated in the Mecsek Mountains (southwest Hungary) in 1997. Mine tailings ponds are located between two important water bases, which are resources of the drinking water of the city of Pe´cs and the neighbouring villages. The average U concentration of the tailings material is 71.73 μg/g, but it is inhomogeneous. Some microscopic particles contain orders of magnitude more U than the rest of the tailings material. Other potentially toxic elements are As and Pb of which chemical state is important to estimate mobility, because in mobile form they can risk the water basis and the public health. Individual U-rich particles were selected with solid state nuclear track detector (SSNTD) and after localisation the particles were investigated by synchrotron radiation based microanalytical techniques. The distribution of elements over the particles was studied by micro beam X-ray fluorescence (μ-XRF) and the oxidation state of uranium and arsenic was determined by micro X-ray absorption near edge structure (μ-XANES) spectroscopy. Some of the measured U-rich particles were chosen for studying the heterogeneity with μ-XRF tomography. Arsenic was present mainly in As(V) and uranium in U(VI) form in the original uranium ore particles, but in the mine tailings samples uranium was present mainly in the less mobile U(IV) form. Correlation was found between the oxidation state of As and U in the same analyzed particles. These results suggest that dissolution of uranium is not expected in short term period.


1979 ◽  
Vol 23 ◽  
pp. 81-86
Author(s):  
Ronald A. Vane ◽  
William D. Stewart ◽  
Mike Barker

AbstractEnergy dispersive X-ray fluorescence (EDXRF) spectrometry has been applied to the high speed analysis of uranium ore for the purpose of grading and sorting truckloads of ore at the mine. The system is able to analyze uranium ore in less than 60 seconds with uranium levels ranging from < 0.005% to > 5% U3O8. Precision at the 2σ level for 200 ppm ore is better than 10% relative. Good agreement is obtained with wet chemical results in a large variety of rock matrices.


1990 ◽  
Vol 212 ◽  
Author(s):  
Takashi Murakami ◽  
Hiroshi Isobe ◽  
Robert Edis

ABSTRACTThe relevance of alteration of chlorite, one of the major constituent minerals of the host rock to uranium ore at Koongarra, to the redistribution of uranium in the vicinity of the ore deposit has been examined. The chlorite alteration is produced by weathering; chlorite is transformed to vermiculite, through regularly interstratified chlorite/vermiculite. The Fe released from chlorite reprecipitates to form iron minerals, possibly ferrihydrite. Vermiculite is then replaced by kaolinite (and possibly smectite), further releasing Fe. On the millimeter scale, an alpha autoradiography study has shown that uranium concentrations are qualitatively proportional to the extent of the alteration; altered chlorite grains having higher uranium concentration. On the meter scale, the X-ray diffraction study has revealed that the abundances of chlorite, vermiculite, and kaolinite correspond well to the low, intermediate, and high uranium concentration zones, respectively. These suggest that the interaction of the uraniferous solution with chlorite causes the alteration of chlorite and the precipitation and sorption of uranium in the alteration products from the solution, and thus, the uranium migration is retarded at Koongarra.


2018 ◽  
pp. 63-68
Author(s):  
A. V. Beidin ◽  
◽  
V. A. Ovseichuk ◽  
A. A. Morozov ◽  
◽  
...  
Keyword(s):  
X Ray ◽  

2010 ◽  
Vol 23 (9) ◽  
pp. 739-745 ◽  
Author(s):  
Hailey S. Reynolds ◽  
Rahul Ram ◽  
Fiona A. Charalambous ◽  
Frank Antolasic ◽  
James Tardio ◽  
...  
Keyword(s):  
X Ray ◽  

1961 ◽  
Vol 33 (12) ◽  
pp. 1709-1713 ◽  
Author(s):  
W. C. Stoecker ◽  
C. H. McBride

RSC Advances ◽  
2015 ◽  
Vol 5 (107) ◽  
pp. 87908-87918 ◽  
Author(s):  
Daniel E. Crean ◽  
Claire L. Corkhill ◽  
Timothy Nicholls ◽  
Ryan Tappero ◽  
Jane M. Collins ◽  
...  

Synchrotron microanalysis was used to provide novel advanced characterisation of uranium ore concentrate particles in application to nuclear forensic science.


1964 ◽  
Vol 8 ◽  
pp. 448-455
Author(s):  
D. R. Knoke ◽  
H. F. Waldron

AbstractSince the advent of vacuum and helium path X-ray spectrometers, and flow proportional counters, the determination of low-atomic-number elements by X-ray fluorescence has become relatively common for light-element matrices. However, there are no reports in the literature on the determination of the low atomic-number elements in a rnatrix approaching that of uranium. This paper describes the successful application of the vacuum path X-ray spectrometer for the determination of calcium in the range of 0.03 to 1.75% (on a U3O3 basis) in uranium ore concentrates. The procedure provides a 50% saving in analyst time, with no sacrifice of accuracy or precision, compared to the chemical method previously used. With a chromium target tube, the intensity of the calcium radiation is quite sufficient for accurate analyses even though the samples contain approximately 80% uranium. The heavy uranium matrix actually serves to minimize any absorption or enhancement effects that would normally be expected from the large number of impurities that are present in widely varied concentrations.Samples are prepared by dissolving 1.8 g of concentrate in 10.0 g of Na2B4O7 at 1050°C and casting into a disk on a polished aluminum plate. The advantages of this preparation compared to the use of pelletised powders will be discussed. The Ca Kα-to-U Mγ ratio is used to minimize the1 effect of instrumental and sample variations and to provide a linear relation with respect to the calcium concentration on a U3O8 basis. Calibration standards are prepared by the addition of CaHPO4 to either pure U3O8 or a uranium ore concentrate of low residual calcium. Data obtained during routine application of this procedure will be presented.


2020 ◽  
Vol 225 ◽  
pp. 05003
Author(s):  
T. Marchais ◽  
B. Pérot ◽  
C. Carasco ◽  
J-L. Ma ◽  
P-G. Allinei ◽  
...  

Gamma logging for uranium exploration are currently based on total counting with Geiger Müller gas detectors or NaI (TI) scintillators. However, the total count rate interpretation in terms of uranium concentration may be impaired in case of roll fronts, when the radioactive equilibrium of the natural 238U radioactive chain is modified by differential leaching of uranium and its daughter radioisotopes of thorium, radium, radon, etc. Indeed, in case of secular equilibrium, more than 95 % of gamma rays emitted by uranium ores come from 214Pb and 214Bi isotopes, which are in the back-end of 238U chain. Consequently, these last might produce an intense gamma signal even when uranium is not present, or with a much smaller activity, in the ore. Therefore, gamma spectroscopy measurements of core samples are performed in surface with high-resolution hyper-pure germanium HPGe detectors to directly characterize uranium activity from the 1001 keV gamma ray of 234mPa, which is in the beginning of 238U chain. However, due to the low intensity of this gamma ray, i.e. 0.84 %, acquisitions of several hours are needed. In view to characterize uranium concentration within a few minutes, we propose here a method using both the 92 keV gamma ray of 234Th and the 98.4 keV uranium X-ray. This last is due to uranium self-induced fluorescence caused by gamma radiations of 214Pb and 214Bi, which create a significant Compton scattering continuum acting as a fluorescence source and resulting in the emission of uranium fluorescence X-rays. The comparison of the uranium activity obtained with the 92 keV and 98.4 keV lines allows detecting a uranium heterogeneity in the ore. Indeed, in case of uranium nugget, the 92 keV line leads to underestimated uranium concentration due to gamma self-absorption, but on the contrary the 98.4 keV line leads to an overestimation because of increased fluorescence. In order to test this new approach, several tens of uranium ore samples have been measured with a handheld HPGe FALCON 5000 detector.


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