Nicole X. Nie, Rosa Grigoryan and Francois L. H. Tissot
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引用次数: 0
摘要
钾同位素在追踪地质过程方面大有可为,但其分析却充满了复杂性。目前已开发出使用不同代 MC-ICPMS 仪器的各种方法,每种方法都有明显的优缺点。在本研究中,我们报告了使用 Thermo Scientific Neoma 碰撞池 MC-ICPMS/MS 进行的 K 同位素测量,以探索该仪器的潜力。测试在湿等离子条件下进行,单次分析 5-25 次测量的精度为 0.03 至 0.1‰(95%c.i.),与其他成熟技术相当。在测试的 50-500 ppb K 浓度范围内,测量结果是准确的。样品和标准品之间的 K 浓度不匹配不超过 5%是可以接受的,而酸摩尔浓度不匹配对测量的 K 同位素组成有明显的影响。当基质元素的浓度低于钾的 2% 时,对钾同位素测量的影响不大。总之,我们的测试表明,使用 Neoma 碰撞池 MC-ICPMS/MS 测量钾同位素是可行的,但仪器对调谐设置的高灵敏度要求在进行此类测量时付出相当大的努力。
High precision analysis of potassium stable isotopes using the collision/reaction cell Neoma MC-ICPMS/MS†
Potassium isotopes hold great promise for tracing geological processes, but their analyses are fraught with complexities. Various methods using different generations of MC-ICPMS instruments have been developed, each with distinct advantages and disadvantages. In this study, we report on K isotopic measurements performed using the Thermo Fisher Scientific Neoma collision cell MC-ICPMS/MS to explore the potential of the instrument. Tests were conducted under wet plasma conditions and the precision achieved was ∼0.03 to 0.1‰ (95% c.i.) for 5–25 measurements in a single analytical session, comparable to other established techniques. The measurements were accurate within the tested concentration range of 50–500 ppb K. A K concentration mismatch between samples and standards of up to 5% was acceptable, while acid molarity mismatch had a pronounced effect on the measured K isotopic compositions. Matrix elements did not significantly impact K isotopic measurements when their concentration was below 2% of K. Several geostandards were measured and the obtained values agree with those from other measurement techniques. Overall, our tests suggest that measuring K isotopes with Neoma collision cell MC-ICPMS/MS is possible, but the high sensitivity of the instrument to tuning settings requires considerable efforts for conducting such measurements.