Lin An-Jun, Yang Tao, Jiang Shao-Yong
State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210093, P.R.China.
Rapid Commun Mass Spectrom. 2014 Apr 15;28(7):750-6. doi: 10.1002/rcm.6838.
Previous studies have indicated that prior chemical purification of samples, although complex and time-consuming, is essential in obtaining precise and accurate results for sulfur isotope ratios using multiple-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). In this study, we introduce a new, rapid and precise MC-ICP-MS method for sulfur isotope determination from water samples without chemical purification.
The analytical work was performed on an MC-ICP-MS instrument with medium mass resolution (m/Δm ~ 3000). Standard-sample bracketing (SSB) was used to correct samples throughout the analytical sessions. Reference materials included an Alfa-S (ammonium sulfate) standard solution, ammonium sulfate provided by the lab of the authors and fresh seawater from the South China Sea. A range of matrix-matched Alfa-S standard solutions and ammonium sulfate solutions was used to investigate the matrix (salinity) effect (matrix was added in the form of NaCl). A seawater sample was used to confirm the reliability of the method.
Using matrix-matched (salinity-matched) Alfa-S as the working standard, the measured δ(34)S value of AS (-6.73 ± 0.09‰) was consistent with the reference value (-6.78 ± 0.07‰) within the uncertainty, suggesting that this method could be recommended for the measurement of water samples without prior chemical purification. The δ(34)S value determination for the unpurified seawater also yielded excellent results (21.03 ± 0.18‰) that are consistent with the reference value (20.99‰), thus confirming the feasibility of the technique.
The data and the results indicate that it is feasible to use MC-ICP-MS and matrix-matched working standards to measure the sulfur isotopic compositions of water samples directly without chemical purification. In comparison with the existing MC-ICP-MS techniques, the new method is better for directly measuring δ(34)S values in water samples with complex matrices; therefore, it can significantly accelerate analytical turnover.
先前的研究表明,尽管样品的化学预纯化复杂且耗时,但对于使用多接收电感耦合等离子体质谱仪(MC-ICP-MS)获得精确准确的硫同位素比值结果而言,这是必不可少的。在本研究中,我们引入了一种无需化学纯化即可测定水样中硫同位素的新型快速精确的MC-ICP-MS方法。
分析工作在具有中等质量分辨率(m/Δm ~ 3000)的MC-ICP-MS仪器上进行。在整个分析过程中使用标准样品夹法(SSB)校正样品。参考物质包括Alfa-S(硫酸铵)标准溶液、作者实验室提供的硫酸铵以及来自中国南海的新鲜海水。使用一系列基质匹配的Alfa-S标准溶液和硫酸铵溶液来研究基质(盐度)效应(基质以NaCl形式添加)。使用一个海水样品来确认该方法的可靠性。
以基质匹配(盐度匹配)的Alfa-S作为工作标准,所测AS的δ(34)S值为(-6.73 ± 0.09‰),在不确定度范围内与参考值(-6.78 ± 0.07‰)一致,这表明该方法可推荐用于无需预先化学纯化的水样测量。未纯化海水的δ(34)S值测定也产生了优异结果(21.03 ± 0.18‰),与参考值(20.99‰)一致,从而证实了该技术的可行性。
数据和结果表明,使用MC-ICP-MS和基质匹配的工作标准直接测量水样的硫同位素组成而无需化学纯化是可行的。与现有的MC-ICP-MS技术相比,新方法更适合直接测量具有复杂基质的水样中的δ(34)S值;因此,它可以显著加快分析周转速度。