首页> 外文期刊>Geochemical Journal >NOTE Determination of 9Be in geological standard samples, JA-2 and JB-2, and of 9Be and 10Be in a basaltic rock sample for evaluation of uncertainty involved in 10Be/9Be ratio measurements
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NOTE Determination of 9Be in geological standard samples, JA-2 and JB-2, and of 9Be and 10Be in a basaltic rock sample for evaluation of uncertainty involved in 10Be/9Be ratio measurements

机译:注:测定地质标准样品JA-2和JB-2中的9Be,以及玄武岩样品中的9Be和10Be,以评估涉及10Be / 9Be比值测量的不确定度

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摘要

We determined the concentrations of 9Be in JB-2 and JA-2 geological standard samples using an inductively coupled plasma mass spectrometer (ICP-MS),, We determined 9Be abundance in standard samples of JA-2 and JB-2 as 2.26 ± 0.10 and 0.241 + 0.010 ppm, respectively, after comparing and selecting 9Be concentration data obtained by the internal standard method, the standard addition method and the column separation method. In the course of comparison, we identified a problem in the internal standard method, which is usually used for abundance analyses using an ICP-MS. Repeated analyses of a basalt lava gave a standard deviation of 10Be abundance of 9% (lcr, n = 5). From the results, we estimated the uncertainty of 10Be/9Be ratio as 10% (lo), considering a law of propagation of errors.
机译:我们使用电感耦合等离子体质谱仪(ICP-MS)确定了JB-2和JA-2地质标准样品中9Be的浓度,确定JA-2和JB-2标准样品中9Be的丰度为2.26±0.10比较和选择通过内标方法,标准添加方法和柱分离方法获得的9Be浓度数据后,分别获得0.21 + 0.010 ppm和0.241 + 0.010 ppm。在比较过程中,我们发现了内标方法中的一个问题,该方法通常用于使用ICP-MS进行丰度分析。对玄武岩熔岩的重复分析得出的10Be标准偏差为9%(lcr,n = 5)。根据结果​​,考虑误差传播定律,我们将10Be / 9Be比的不确定性估计为10%(lo)。

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