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A modified multi-elevated-temperature post-IR IRSL protocol for dating Holocene sediments using K-feldspar

机译:使用钾长石对全新世沉积物进行测年的改进的多温度后IR IRSL协议

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摘要

A modified multi-elevated-temperature post-IR infra-red stimulated luminescence (MET-pIRIR) protocol is proposed for dating young samples of Holocene age using K-feldspar. The protocol utilizes a five-step MET-pIRIR measurement with a moderate preheating of 200°C for 60s, and a narrow IR stimulation temperature increment of 30°C (i.e., the five measurement temperatures are 50, 80, 110, 140 and 170°C). Using this method, the residual doses of the MET-pIRIR signals are generally less than 1Gy. Holocene aeolian samples from Northern China were tested using the 30°C-increment modified MET-pIRIR method. The results demonstrate that similar ages from 140°C to 170°C were obtained for our samples, which were consistent with the quartz optically stimulated luminescence (OSL) ages. Based on this observation, the measurement procedures are further simplified to a three-step pIRIR protocol. The first IR stimulation at elevated temperature (110°C) is used to remove the fading affected signals. This is followed by two steps of IR stimulation at high temperatures (140 and 170°C) for equivalent dose (De) measurement. Dating results consistent with the expected ages have been obtained at stimulation temperatures of 140 and 170°C. It is suggested that the first IR stimulation can effectively remove the fading component. The three-step pIRIR method has minimized the experimental procedures, while keeping the age plateau test.
机译:提出了一种改进的多重高温后红外红外激发发光(MET-pIRIR)协议,用于使用钾长石对全新世年龄的年轻样品进行测年。该协议采用五步MET-pIRIR测量,其中200°C适度预热60s,IR刺激温度增量窄至30°C(即,五个测量温度分别为50、80、110、140和170 °C)。使用这种方法,MET-pIRIR信号的残留剂量通常小于1Gy。使用增加的30°C改进的MET-pIRIR方法测试了来自中国北方的全新世风沙样品。结果表明,我们的样品获得了从140°C到170°C的相似年龄,这与石英光学激发发光(OSL)年龄一致。基于此观察结果,将测量程序进一步简化为三步pIRIR协议。高温(110°C)下的第一个红外刺激用于去除褪色的受影响信号。接下来是在高温(140和170°C)下进行红外刺激的两个步骤,以进行等效剂量(De)测量。在140和170°C的刺激温度下已获得与预期年龄相符的约会结果。建议第一次IR刺激可以有效地去除褪色成分。三步pIRIR方法使实验程序减至最少,同时保持了平台期测试。

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