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On the dose dependency of the bleachable and non-bleachable components of IRSL from K-feldspar: Improved procedures for luminescence dating of Quaternary sediments

机译:关于钾长石IRSL中可漂白和不可漂白成分的剂量依赖性:第四系沉积物发光测年的改进程序

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The infrared (IR) stimulated luminescence (IRSL) and post-IR IRSL (pIRIR) signals from K-feldspar can, for convenience, be divided into two components, bleachable and 'non-bleachable', where the latter corresponds to the 'residual' signal observed in sunlight-bleached samples. In this paper, we examine the non-bleachable component of IRSL of K-feldspar for several sedimentary samples from across Eurasia. We observed a large variability in the residual doses among these samples after prolonged exposure to sunlight. By employing multiple elevated temperature (MET) IR stimulations at 50-300°C, we show that the residual dose increases systematically with stimulation temperature, attaining values as high as ~50Gy at 300°C, even after several hours to tens of hours of exposure to unfiltered sunlight. We examined two samples in detail and found that the bleachable and non-bleachable components produced different dose response curves. Pulse annealing studies showed that the non-bleachable component is more stable than the bleachable component, suggesting that a preheat procedure cannot eliminate the non-bleachable component. Additional experiments revealed that the non-bleachable component is dose dependent. Owing to this dose dependency, we demonstrate mathematically and empirically that the simple subtraction of a residual dose from the measured equivalent dose (D_e) - which is the most common approach employed (if any residual dose is subtracted at all) - will result in underestimation of the actual D_e. We present a method to correct for the dose dependency of the residual dose, which can improve the accuracy of either MET-pIRIR or pIRIR age estimates for samples in which the non-bleachable component represents a significant fraction of the measured signals.
机译:为了方便起见,可以将来自钾长石的红外(IR)激发发光(IRSL)和后红外IRSL(pIRIR)信号分为可漂白和“不可漂白”两个部分,其中后者对应于“残余”在日光漂白的样品中观察到信号。在本文中,我们检查了整个欧亚大陆的若干沉积物样品中钾长石IRSL的不可漂白成分。我们观察到,长时间暴露在阳光下,这些样品中的残留剂量存在很大差异。通过在50-300°C下使用多次高温(MET)IR刺激,我们显示了残余剂量随刺激温度的增加而系统地增加,即使在经过数小时至数十小时的加热后,其残留值在300°C时仍高达〜50Gy。暴露在未经过滤的阳光下。我们详细检查了两个样品,发现可漂白和不可漂白组分产生不同的剂量反应曲线。脉冲退火研究表明,不可漂白组分比可漂白组分更稳定,表明预热程序无法消除不可漂白组分。其他实验表明,不可漂白成分是剂量依赖性的。由于这种剂量依赖性,我们在数学和经验上证明,从所测得的当量剂量(D_e)中简单减去残留剂量-这是最常用的方法(如果完全减去任何残留剂量)将导致低估实际D_e。我们提出了一种校正残留剂量的剂量依赖性的方法,该方法可以提高MET-pIRIR或pIRIR年龄估计值的准确性,其中不可漂白成分占所测信号的很大一部分。

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