Determination of major and trace elements in silicate rock fused with lithium metaborate using laser ablation-inductively coupled plasma-mass spectrometry†

IF 3.1 2区 化学 Q2 CHEMISTRY, ANALYTICAL Journal of Analytical Atomic Spectrometry Pub Date : 2023-12-29 DOI:10.1039/D3JA00339F
Xiaoyun Qiu, Zhaochu Hu, Tao He, Tao Luo, Wen Zhang, Ming Li, Keqing Zong, Zaicong Wang and Yongsheng Liu
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Abstract

In this study, a novel lithium metaborate fusion technique using a homemade fusion furnace and graphite crucibles was developed to produce homogeneous glasses from silicate rock powder. The glasses were then analyzed for both major and trace element concentrations by LA-ICP-MS. The parameters of the ratio of flux-to-sample, melting temperature and time, and closed fusion were optimized. It was found that homogeneous glasses could be obtained, and the loss of Pb was effectively suppressed at a low melting temperature and short time (900 or 950 °C for 5 min) in closed fusion. Compared to Pt or Pt–Au crucibles in the traditional flux fusion method, homemade graphite crucibles are more economical and omit the need of any releasing agent because the bottom curve design allows the melt to shrink into a bead for easy removal. Accurate results by LA-ICP-MS can be directly obtained by applying a quantitative calibration strategy using 100% oxide normalization, which offers a solution for unknown sample analysis without the prior determination of the concentration of an internal standard element. The analytical results of 42 major and trace elements in 5 USGS silicate rock reference materials (covering mafic to felsic rock types) using the developed LiBO2 fusion technique are consistent with the reference values within 10% for most elements, and analytical precision (RSD) is within 10% for most elements. The developed method is simple for preparing homogeneous glasses from rock powders, which displays great potential for the rapid and accurate determination of mass fractions of major and trace elements in silicate rocks using LA-ICP-MS.

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利用激光烧蚀-电感耦合等离子体质谱法测定偏硼酸锂熔融硅酸盐岩中的主要元素和痕量元素
本研究利用自制的熔炉和石墨坩埚开发了一种快速、简单的偏硼酸锂熔融技术,用于利用 LA-ICP-MS 测定硅酸盐岩中的主要元素和痕量元素。对熔剂与样品的比例、熔化温度和时间以及封闭熔化等参数进行了优化。结果发现,在闭合熔融过程中使用较低的熔融温度和较短的熔融时间(900 或 950 ℃,5 分钟)时,可以获得均匀的玻璃,并有效地抑制了铅的损失。与传统助熔剂熔炼法中的铂或铂-金坩埚相比,自制石墨坩埚更为经济,而且由于底部设计成弧形,熔体可收缩成珠状,便于取出,因此无需添加任何脱模剂。通过采用 100% 氧化物归一化的定量校准策略,可直接获得 LA-ICP-MS 的准确结果,这为未知样品分析提供了一种无需事先确定内标元素浓度的解决方案。利用所开发的 LiBO2 融合技术对 5 种 USGS 硅酸盐岩参考材料(涵盖岩浆岩至长石岩类型)中的 42 种主要元素和痕量元素进行分析的结果表明,大多数元素与参考值的一致性在 10% 以内。大多数元素的分析精度(RSD)在 10%以内。所开发的方法易于从岩石粉末中制备均质玻璃,在利用 LA-ICP-MS 快速准确地测定硅酸盐岩中主要元素和痕量元素的质量分数方面显示出巨大的潜力。
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来源期刊
CiteScore
6.20
自引率
26.50%
发文量
228
审稿时长
1.7 months
期刊介绍: Innovative research on the fundamental theory and application of spectrometric techniques.
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