商业氧化镁热致发光与光致发光相关性的组分解析分析

IF 1.2 4区 地球科学 Q3 Earth and Planetary Sciences
N. Meriç, E. Şahiner, G. Kitis, G. Polymeris
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引用次数: 1

摘要

摘要本研究旨在使用市售氧化镁量化TL与CW-OSL或LM-OSL之间的关系。样品在两个不同的温度下漂白,并对积分信号进行成分分辨分析。根据本研究的数据,观察到的五个LM-OSL组分中的每一个都从至少两个不同的TL峰接收电子。在LM-OSL曲线中解析了两种不同的快速OSL组分,这两种组分都积累了来自Tmax>150°C的所有TL发光峰的电子。组分C3与102、135和194°C时的TL峰值有很好的相关性,而组分C4和C5与292°C、353°C和464°C的TL辉光峰值有关。我们注意到,对于CW-OSL,当两个或多个分量的强度相差一个数量级时,分辨率是好的。蓝色刺激基本上耗尽前两个TL峰,但不耗尽第三个峰。仅通过使用LM-OSL配置来实现高温TL峰的实质性耗尽。本研究的结果表明,尽管使用了不同的重组途径,但有助于TL和OSL的陷阱是相同的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Component-Resolved Analysis Towards Correlation between Thermoluminescence and Optically Stimulated Luminescence in Commercial Magnesium Oxide
Abstract The present study aimed at quantifying the relationship between TL and either CW-OSL or LM-OSL using commercially available magnesium oxide. The samples were bleached at two different temperatures, and a component-resolved analysis on the integrated signals was performed. According to the data of the present study, each one among the five observed LM-OSL component receives electrons from at least two different TL peaks. Two different fast OSL components were resolved in the LM-OSL curves, both accumulating electrons from all TL glow peaks with Tmax>150°C. Component C3 is very well correlated with the TL peaks at 102, 135 and 194°C, while components C4 and C5 are related to the TL glow peaks of 292°C, 353°C and 464°C. We note that for CW-OSL the resolution is good when two or more components differ in intensity by an order of magnitude. Blue stimulation depletes substantially the first two TL peaks but not the third peak. Substantial depletion of the high-temperature TL peaks is achieved only by using the LM-OSL configuration. The results of the present study suggest that the traps that contribute to TL and OSL are the same, despite using different recombination pathways.
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来源期刊
Geochronometria
Geochronometria 地学-地球科学综合
CiteScore
2.20
自引率
0.00%
发文量
1
审稿时长
>12 weeks
期刊介绍: Geochronometria is aimed at integrating scientists developing different methods of absolute chronology and using them in different fields of earth and other natural sciences and archaeology. The methods in use are e.g. radiocarbon, stable isotopes, isotopes of natural decay series, optically stimulated luminescence, thermoluminescence, EPR/ESR, dendrochronology, varve chronology. The journal publishes papers that are devoted to developing the dating methods as well as studies concentrating on their applications in geology, palaeoclimatology, palaeobiology, palaeohydrology, geocgraphy and archaeology etc.
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