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三重四极杆电感耦合等离子体质谱仪测定铼含量

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铼(Re)是自然界中最稀有的元素之一,因其含量低而测定较为困难.三重四极杆电感耦合等离子体质谱仪(ICP-MS/MS)为解决该难题提供了技术支持.本文利用ICP-MS/MS建立了快速分析Re含量的方法.结果表明,ICP-MS/MS的灵敏度较传统的单杆ICP-MS显著提高,能够准确分析Re含量低至0.5 pg/mL的样品;样品中基体(Ca、K、Mg、Na)浓度在较低时对Re的分析没有影响,浓度高于2000 μg/mL时基体干扰会降低分析结果的准确性.因此,分析时可先通过离子交换纯化或稀释以减小基体效应的影响再进行样品测试.采用该方法对河水标样SLRS-6、岩石标样BHVO-2和BCR-2的Re含量进行分析,其结果分别为(14.4±0.4)pg/mL、(0.59±0.05)ng/g和(12.46±1.21)ng/g,均与报道结果一致.最后,利用建立的方法分析常见的自然样品(如河水、岩石、土壤、沉积物等)的Re含量,获得了与前人报道一致的分析结果,这些结果丰富了自然界Re含量储库,也增加了对自然界Re变化的认识.
The measurement of Re concentration by using the triple quadrupole inductively coupled plasma mass spectrometer
Rhenium(Re)is one of the rarest elements in nature,and it is difficult to be analyzed due to its low content in nature samples.The triple quadrupole inductively coupled plasma mass spectrometer(ICP-MS/MS)provides technical support for solving this problem.In this study,we have established a method for rapidly analyzing Re content by using the triple quadrupole ICP-MS/MS.The results show that the sensitivity of the triple quadrupole ICP-MS/MS is obviously higher than that of the traditional single-rod ICP-MS.The lowest Re content of 0.5 pg/mL in sample can be accurately measured by using the triple quadrupole ICP-MS/MS.There is no influence for Re analysis when contents of matrix elements(Ca,K,Mg,Na)in sanples are relatively low.However,the accuracy of analytical results will be reduced by the matrix interference when contents of matrix elements in samples are higher than 2000 μg/mL.Therefore,the sample can be measured after ion exchange or dilution to reduce the influence of matrix effects.Analytical results of Re contents of the river water standard SLRS-6,the rock standard BHVO-2,and the rock standard BHVO-2 by using the method are(14.4±0.4)pg/mL,(0.59±0.05)ng/g and(12.46±1.21)ng/g,respectively.They are respectively consistent with previously resported results.Finally,we have analyzed Re contents of common natural samples,such as river waters,rocks,soils and sediments,by using the newly established method and obtained results which are consistent with previously reported data.These results enrich the reservoir of Re contents in nature and enhance our understanding of variations of Re contents in nature.

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张玉红、汪进、贺茂勇、邓丽、王安琪、曲远馨

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中国科学院地球环境研究所,黄土与第四纪地质国家重点实验室,西安 710061

中国科学院大学,北京 100049

西安地球环境创新研究院,西安 710061

三重四极杆电感耦合等离子体质谱 Re含量 实验分析 标准曲线

中国科学院战略性先导科技专项(B类)国家自然科学基金资助项目

XDB4000000042003056

2024

矿物岩石地球化学通报
中国矿物岩石地球化学学会 中国科学院地球化学研究所

矿物岩石地球化学通报

CSTPCD北大核心
影响因子:0.912
ISSN:1007-2802
年,卷(期):2024.43(3)