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The nature of unusual luminescence in natural calcite CaCO3
被引:24
|作者:
Gaft, Michael
[1
]
Nagli, Lev
[2
]
Panczer, Gerard
[3
]
Waychunas, Glenn
[4
]
Porat, Naomi
[5
]
机构:
[1] Open Univ, Dept Nat Sci, Raanana, Israel
[2] Tel Aviv Univ, Sch Phys & Astron, IL-69978 Tel Aviv, Israel
[3] Univ Lyon 1, CNRS, UMR 5620, Phys Chem Luminescence Mat Lab, F-69622 Villeurbanne, France
[4] Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Dept Geochem, Berkeley, CA 94720 USA
[5] Geol Survey Israel, IL-95501 Jerusalem, Israel
关键词:
calcite;
time-resolved luminescence;
radiation-induced luminescence centers;
D O I:
10.2138/am.2008.2576
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
The unusual luminescence of particular varieties of natural pink calcite (CaCO3) samples was Studied by laser-induced time-resolved luminescence spectroscopy at different temperatures. The luminescence is characterized by intense blue emission under shortwave UV lamp excitation with an extremely long decay time, accompanied by pink-orange luminescence under longwave UV excitation. Our investigation included optical absorption, natural thermostimulated luminescence (NTL) and Laser-Induced Breakdown Spectroscopy (LIBS) studies. Two luminescence centers were detected: (1) a narrow violet band, with lambda(max) = 412 mr, Delta = 45 nm, two decay components of tau(1) = 5 ns and tau(2) = 7.2 ms, accompanied by very long afterglow, and an orange emission band with lambda(max) = 595 nm, Delta = 90 nm, and tau = 5 ns. Both luminescence centers are thermally unstable with the blue emission disappearing after heating at 500 degrees C, and the orange emission disappearing after heating at different temperatures starting from 230 degrees C, although sometimes it is stable up to 500 degrees C in different samples. Both centers have spectral-kinetic properties very unusual for mineral luminescence, which in combination with extremely low impurity concentrations prevent their identification with specific impurity related emission. The most likely explanation of these observations may be the presence of radiation-induced luminescence centers. The long violet afterglow is evidently connected with trapped charge carrier liberation, with their Subsequent migration through the valence band and ultimate recombination with a radiation-induced center responsible for the unusual violet luminescence.
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页码:158 / 167
页数:10
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