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Comparison of blue and red TL from quartz

机译:石英中蓝色和红色TL的比较

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摘要

Following a suggestion by Scholefield and Prescott that blue and red emissions in quartz may involve the same electron traps, we have made a detailed study of blue and red TL glow peaks in some Australian sedimentary quartz samples (Scholefield, R.B., Prescott, J.R., 1999. The red thermoluminescence of quartz: 3-D spectral measurements. Radiat. Meas. 30, pp. 83-95). Allowing for thermal quenching of the blue TL, the Rapidly Bleaching Peak (at 325 degreesC for a ramp rate of 20 K s(-1)) and the low temperature peaks at 140-220 degreesC appear to be identical in the blue and red. We conclude that the electron traps are the same, but that the blue and red luminescence centers probably do not occur in the same grains. On present evidence we cannot determine whether or not the Slowly Bleaching Peak (at 375 degreesC for 20 K s(-1)) involves the same traps in the blue as in the red. As did Scholefield and Prescott, we find no evidence of a red peak at 100 degreesC. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 25]
机译:根据Scholefield和Prescott的建议,石英中的蓝色和红色发射可能涉及相同的电子陷阱,我们对一些澳大利亚沉积石英样品中的蓝色和红色TL辉光峰进行了详细研究(Scholefield,RB,Prescott,JR,1999年)。石英的红色热致发光:3-D光谱测量(辐射测量,第30页,第83-95页)。考虑到蓝色TL的热淬灭作用,蓝色和红色的快速漂白峰(在325℃时,斜率为20 K s(-1))和140-220℃的低温峰似乎相同。我们得出的结论是,电子陷阱相同,但是蓝色和红色发光中心可能不会出现在同一晶粒中。根据目前的证据,我们无法确定缓慢漂白峰(在375摄氏度下20 K s(-1))是否包含与红色相同的陷阱。与Scholefield和Prescott一样,我们没有发现100摄氏度出现红色峰的迹象。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:25]

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