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Determination of Trace Elements in Ice Core Samples by Laser Ablation Inductively Coupled Plasma Mass Spectrometry

机译:激光烧蚀电感耦合等离子体质谱法测定冰芯样品中的微量元素

摘要

The snow and iceshields of the polar regions serve as a climate archiveand deliver a useful insight back to about 250.000 years of earth climatehistory1,2. The aim of our investigation reported here was to establisha new method for the determination of trace elements in ice cores frompolar regions with Laserablation Inductively Coupled Plasma MassSpectrometry (LA-ICP-MS)3. Primarily, the construction of a cryogeniclaserablation chamber and the optimization of the analysis system forthe sample matrix were the main goals. This paper reports preliminaryresults from measurements of frozen ice samples, the achievable signalintensities, standard deviations and calibration graphs as well as the firstsignal progression of 208Pb in an 8000 years old ice core sample fromGreenland.
机译:极地地区的雪和冰盾可以作为气候档案,并为追溯约250.000年的地球气候历史提供有用的见解1,2。我们在此报告的调查目的是建立一种新的方法,通过激光烧蚀电感耦合等离子体质谱法(LA-ICP-MS)3测定极地冰芯中的痕量元素。首先,低温激光消融室的构建和样品基质分析系统的优化是主要目标。本文报告了来自格陵兰岛8000年历史的冰芯样品中冷冻冰样品的测量结果,可达到的信号强度,标准偏差和校正图以及208Pb的第一个信号变化的初步结果。

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