漂白后复合中心的残余孔洞浓度

IF 1.2 4区 地球科学 Q3 Earth and Planetary Sciences
N. K. Pawlak, A. Timar-Gabor, A. Chruścińska
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引用次数: 0

摘要

摘要利用石英电子自旋共振(ESR)的俘获电荷测年法已逐渐用于沉积物测年。只有当这些信号在层形成之前被阳光照射归零时,或者当人们知道它们的ESR残余水平(信号中未漂白的部分)时,ESR信号才能用于精确的年龄估计。众所周知,与用于沉积物测年的石英中的Al孔中心相关的ESR信号具有显著的残差信号。从发光模型的角度来看,作为空穴陷阱,Al空穴中心被认为是石英中的复合中心。最近,实验证明,Al空穴中心的ESR信号取决于过去石英样品吸收的总剂量。通过对包括两个复合中心的模型的电荷传输过程的模拟,证实了同样的效果。在此,通过对各种模型参数的计算机模拟,详细研究了复合中心中的残余空穴浓度(RHC)对过去样品吸收的总剂量的依赖性。研究了中心参数的各种关系对残差作为剂量函数的依赖性的影响,并讨论了其对测年实践的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Residual Hole Concentration in Recombination Centres after Bleaching
Abstract Trapped charge dating method using electron spin resonance (ESR) of quartz is progressively used for sediment dating. ESR signals can be used for accurate age estimation only when these signals are zeroed by sunlight exposure before the layer creation or when one knows their ESR residual level (the part of the signal that is not bleached). It is well known that the ESR signal related to the Al-hole centres in quartz used for sediment dating has a significant residual signal. From the point of view of luminescence models, as a hole trap, the Al-hole centre is considered as a recombination centre in quartz. Recently, it was demonstrated experimentally that the ESR signal of the Al-hole centre is dependent on the total dose absorbed by the quartz sample in the past. The same effect was confirmed by simulations of the charge transport processes for a model including two recombination centres. Here, the dependence of residual hole concentration (RHC) in the recombination centres on the total dose absorbed by a sample in the past is studied in detail by computer simulations for a wide range of model parameters. The impact that the various relations of centre parameters have on the dependence of the residual as a function of dose is investigated and the implications for the dating practice are discussed.
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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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