王水
分析化学(期刊)
化学
同位素稀释
铂族
同质性(统计学)
基质(化学分析)
校准
同位素
铂金
矿物学
质谱法
色谱法
金属
数学
物理
统计
生物化学
有机化学
量子力学
催化作用
作者
Huai Cheng,Zaicong Wang,Kang Chen,Keqing Zong,Zongqi Zou,Tao He,Zhaochu Hu,M. Fischer-Gödde,Yanhong Liu
摘要
Determination of gold abundances in natural rock is critical for applications, but very challenging. Here, we report a method for determining gold with a very low mass fraction (> 0.01 ng g −1 ) in rocks. The method involves Carius tube digestion with reverse aqua regia , chromatographic separation to remove most of the sample matrix and measurement by high‐sensitivity ICP ‐ MS . The mono‐isotopic element gold was quantified by external calibration using an internal standardisation of gold to platinum that was precisely determined by isotope dilution. The method is robust and the obtained results are indistinguishable (< 5–10%, 2 s ) from those independently obtained by a standard addition technique on the same solution. The results from reference materials TDB ‐1 and GP t‐2 are consistent with the certified values and those determined by HF ‐ aqua regia digestion, confirming the validity of the method. TDB ‐1 ( n = 20), GP t‐2 ( n = 6), BHVO ‐2 ( n = 9) and other mafic RM s are homogenous for gold (10–20%, 2 s ) at the 2 g test portion level; however, sample heterogeneity affects some RM s. Gold and platinum‐group elements also display different extents of sample heterogeneity for different RM s. Given the homogeneity observed for TDB ‐1, GP t‐2 and BHOV ‐2, they are recommended as well‐suited RM s for inter‐laboratory comparison studies of gold.
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