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Accurate and precise determination of Lu and Hf contents and Hf isotopic composition at the sub-nanogram level in geological samples using MC-ICP-MS

机译:使用MC-ICP-MS精确准确地测定地质样品中亚纳米级的Lu和Hf含量以及Hf同位素组成

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摘要

We describe protocols for highly reproducible analysis of Lu and Hf contents and Hf isotopic composition at sub-nanogram levels in geological samples by MC-ICP-MS. Powdered samples were spiked with a Lu-176-Hf-180 enriched tracer and completely digested using conventional HF, HNO3 and HClO4 acid dissolution protocols. Fluoride salts were dissolved during a final H3BO3 digestion and chemical purification was performed using a single Eichrom Technologies Ln resin. All measurements were carried out on a Neptune Plus MC-ICP-MS employing an Aridus II desolvator. In order to demonstrate the robustness of the proposed protocol, six rock reference materials (RMs) were analysed, spanning various rock types with very low Lu and Hf contents (from nanogram to sub ng g(-1) levels). The results are in good agreement within uncertainty with published values for the analysed RMs. Relative to other approaches and low-blank levels, this protocol has great potential for Lu-Hf analysis of low volume (100-500 mg) samples in geochemistry, cosmochemistry and environmental sciences (e.g., peridotite, garnet, meteorites, dust, etc.).
机译:我们描述了通过MC-ICP-MS在地质样品中的亚纳米级水平对Lu和Hf含量以及Hf同位素组成进行高度可重复分析的协议。用富含Lu-176-Hf-180的示踪剂掺入粉末状样品,并使用常规HF,HNO3和HClO4酸溶解方案完全消化。在最终的H3BO3消化过程中将氟化盐溶解,并使用单一的Eichrom Technologies Ln树脂进行化学纯化。所有测量均在采用Aridus II去溶剂剂的Neptune Plus MC-ICP-MS上进行。为了证明所提出协议的鲁棒性,分析了六种岩石参考材料(RM),涵盖了Lu和Hf含量非常低(从纳克到ng g(-1)含量)的各种岩石类型。在不确定的范围内,结果与已分析的RM的公布值一致。相对于其他方法和低空白水平,该方案对于在地球化学,宇宙化学和环境科学(例如橄榄岩,石榴石,陨石,粉尘等)中对少量(100-500 mg)样品进行Lu-Hf分析具有巨大的潜力。 )。

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  • 来源
    《Journal of Analytical Atomic Spectrometry》 |2019年第6期|1256-1262|共7页
  • 作者单位

    China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Sch Earth Sci & Resources, Beijing 100083, Peoples R China|Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China;

    Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Curtin Univ, Sch Earth & Planetary Sci, John de Laeter Ctr, Perth, WA, Australia;

    Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Sch Earth Sci & Resources, Beijing 100083, Peoples R China;

    Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

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