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Comparison of the properties of various optically stimulated luminescence signals from potassium feldspar

机译:钾长石的各种光激发发光信号的性质比较

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Various optically stimulated luminescence signals from K-feldspar have been used to determine the equivalent doses of sediment samples. Understanding the properties of these optical signals is critical to evaluate their applicability and limitations to optical dating. In this paper, some properties of IRSL, post-IR OSL and post-IR IRSL signals (detected in the UV region using U-340 filters) from a museum sample of K-feldspar were investigated by analyzing the relationships between optical and TL signals, and the effect of optical bleaching and heating on optical signals. The trap parameters of the different optical signals were calculated using the pulse annealing method. The results show that this sample exhibits two regenerated TL peaks at ~140 and ~330 °C. Corresponding to the low temperature TL peak, the OSL and post-IR OSL signals appear to be more associated with lower temperature TL than the IRSL signal measured at 50°C. Corresponding to the high temperature TL peak, the post-IR IRSL signals mainly originate from the more thermally stable traps associated with the high temperature TL, compared with the IRSL and post-IR OSL signals. However, the post-IR IRSL _(225°C) signal is shown to be hard to be bleached by blue light and simulated sunlight, compared with the IRSL _(50°C) and low temperature post-IR IRSL signals. The implication for optical dating is that the elevated temperature post-IR IRSL signals can be preferentially applied over other signals from K-feldspar, but it is desirable that the effectiveness of the pre-depositional zeroing of these signals is assessed.
机译:来自钾长石的各种光学激发的发光信号已用于确定沉积物样品的当量。了解这些光信号的特性对于评估其适用性和对光测年的限制至关重要。本文通过分析光和TL信号之间的关系,研究了来自钾长石博物馆样品的IRSL,IR IR OSL和IRIR IRSL信号的某些特性(使用U-340滤光片在紫外区域检测到) ,以及光漂白和加热对光信号的影响。使用脉冲退火方法计算不同光信号的陷阱参数。结果表明,该样品在〜140和〜330°C处显示两个再生的TL峰。与低温TL峰值相对应,与在50°C下测得的IRSL信号相比,OSL和IR-IR OSL信号似乎与较低的温度TL相关性更高。对应于高温TL峰值,与IRSL和IR-OSL信号相比,IR-IR IRSL信号主要源自与高温TL相关的更热稳定的陷阱。但是,与IRSL _(50°C)和低温IRIR后的IRSL信号相比,IRIR IR __(225°C)后的信号显示很难被蓝光和模拟的阳光漂白。光学测年的含义是,IR后IRSL高温信号可以优先于来自钾长石的其他信号施加,但是希望评估这些信号的沉积前置零的有效性。

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