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Low-magnesium uranium–calcite with high degree of crystallinity and gigantic luminescence emission
Cabrera (Madrid) low-Mg calcites exhibit: (i) an unusual twofold elevation in X-ray diffraction pattern intensity; (ii) a 60-fold elevation of luminescence emission, compared to six common natural calcites selected for comparison purposes; (iii) a natural relatively high radiation level of circa 200...
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Published in: | Applied radiation and isotopes 2007, Vol.65 (1), p.147-154 |
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Main Authors: | , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Cabrera (Madrid) low-Mg calcites exhibit: (i) an unusual twofold elevation in X-ray diffraction pattern intensity; (ii) a 60-fold elevation of luminescence emission, compared to six common natural calcites selected for comparison purposes; (iii) a natural relatively high radiation level of circa 200
nSv
h
−1 not detected in 1300 other calcites from the Natural History Museum of Madrid. Calcites were analysed by the X-ray diffraction powder method (XRD), cathodo-luminescence spectroscopy in scanning electron microscopy (CL-SEM), thermoluminescence (TL), differential thermal analysis (DTA), X-ray fluorescence spectrometry (XRF) and particle size distribution (PSD). The Cabrera calcite study shows: (i) helicoidally distributed steps along the (0
0
0
1) orientation; (ii) protuberance defects onto the (0
0
0
1) surface, observed by SEM; (iii) XRF chemical contents of 0.03% MgO, 0.013% of Y
2O
3, and 0.022% of U
3O
8, with accessory amounts of rare earth elements (REE); (iv) DTA dissociation temperature of 879
°C; (v) TL maxima peaks at 233 and 297
°C whose areas are 60 times compared to other calcites; (vi) spectra CL-SEM bands at 2.0 and 3.4
eV in the classic structure of Mn
2+ activators; (vii) a twofold XRD pattern explained given that sample is a low-Mg calcite. The huge TL and CL emissions of the Cabrera calcite sample must be linked with the uranyl group presence. This intense XRD pattern in low-Mg calcites could bring into being analytical errors. |
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ISSN: | 0969-8043 1872-9800 |
DOI: | 10.1016/j.apradiso.2006.07.010 |