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Determination of major and trace elements in geological samples by laser ablation solution sampling-inductively coupled plasma mass spectrometry

机译:激光烧蚀溶液采样电感耦合等离子体质谱法测定地质样品中的主要和微量元素

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摘要

To overcome the major shortcomings in conventional ICP-MS analysis with sample introduction by nebulization, a new solution sampling method was developed using laser ablation (LA). With this sampling method, water-related interferences were reduced by 1-2 orders of magnitude, the effects of which are similar to those obtained in membrane desolvation ICP-MS. Another important advantage of this method is that the matrix effects became insignificant in the ICP-MS analysis whether employing a matrix with the sample dilution factor varying between 80 and 2000 or an acid matrix ranging from 2% to 30% (v/v) HNO3. Compared with LA-ICP-MS analysis of solids, this sampling method exhibited 70-250 times improvement in signal sensitivity and the detection limits for most elements were two orders of magnitude lower. Unlike solid sample analysis, the commonly observed time-resolved element fractionation during laser ablation was negligible in solution sampling by LA. With the widely used reference material NIST 610 silicate glass as the external calibration standard and indium as the internal standard element, major and trace elements in a series of geological reference materials (ranging from mafic to felsic rocks) were successfully determined: the feasibility was verified with accuracies within 10% for 45 elements, and most of the precisions were reported as RSD better than 7%. Besides, due to the high tolerance of matrix effects, this method is comparatively green and environment friendly because of the minute consumption of acid and ultrapure water during the sample preparation process, which was reduced by 20-100 times compared to that in the conventional nebulization method. Being simple and effective, this method opens up a new prospect for the solution sampling of ICP-MS analysis.
机译:为了克服常规ICP-MS分析中的主要缺点,采用雾化引入介绍,采用激光烧蚀(LA)开发了一种新的解决方案采样方法。利用这种取样方法,水相关的干扰减少了1-2的数量级,其效果类似于膜DeSolvation ICP-MS中获得的效果。该方法的另一个重要优点是,在ICP-MS分析中,基质效应是不显着的,无论是否使用稀释剂的样品稀释因子在80%和2000之间的稀释因子或酸基质范围为2%至30%(v / v)hnO3之间。与固体的La-ICP-MS分析相比,这种采样方法的信号灵敏度提高了70-250倍,并且大多数元素的检测限量是两个数量级。与固体样品分析不同,激光消融期间的常见时间分辨的元素分级在La溶液采样中可以忽略不计。利用广泛使用的参考材料NIST 610硅酸盐玻璃作为外部校准标准和作为内标元件的铟,成功确定了一系列地质参考材料中的主要和微量元素(从MAFIC到肠岩)中成功确定:验证了可行性对于45个元素的10%以内的准确度,大部分精度被报告为RSD,优于7%。此外,由于基质效应的耐受性高,这种方法相对较为绿色和环保,因为在样品制备过程中的酸和超纯水的微小消耗,与传统雾化相比减少了20-100次方法。这种方法简单有效,为ICP-MS分析的解决方案采样开辟了新的前景。

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  • 来源
    《Journal of Analytical Atomic Spectrometry》 |2019年第6期|1126-1134|共9页
  • 作者单位

    China Univ Geosci State Key Lab Geol Proc & Mineral Resources Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci State Key Lab Geol Proc & Mineral Resources Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci State Key Lab Geol Proc & Mineral Resources Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci State Key Lab Geol Proc & Mineral Resources Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci State Key Lab Geol Proc & Mineral Resources Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci State Key Lab Geol Proc & Mineral Resources Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci State Key Lab Geol Proc & Mineral Resources Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci State Key Lab Geol Proc & Mineral Resources Wuhan 430074 Hubei Peoples R China;

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