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Determination of lithium-7/lithium-6 isotope ratios in geological materials by inductively coupled plasma mass spectrometery.

机译:电感耦合等离子体质谱法测定地质材料中锂7 /锂6同位素的比率。

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摘要

A method for the determination of Li isotope ratios in a variety of Li-minerals using Inductively Coupled Plasma Mass Spectrometry is described. Lithium isotope ratios are determined with a precision of better than 0.1% and with an absolute accuracy of greater than 0.6% in samples containing as little as 60 ppb Li. Sample material is digested with HF and HCl in sealed Teflon vials and then Li is separated from the matrix on Bio-Rad AG50W-X8, 100-200 mesh cation exchange resin, since concomitant elements in solution are shown to cause isotope patio shifts at concentrations above 100 ppm for several elements (Na, K, Ca, Cs, Sr, Mg). The measured isotope ratios (
机译:描述了一种使用电感耦合等离子体质谱法测定各种锂矿中锂同位素比的方法。在低至60 ppb Li的样品中,锂同位素比的测定精度优于0.1%,绝对精度大于0.6%。样品材料在密封的特氟隆小瓶中用HF和HCl消解,然后在Bio-Rad AG50W-X8(100-200目阳离子交换树脂)上从基质中分离出Li,原因是溶液中伴随的元素在浓度下会引起同位素比值漂移某些元素(Na,K,Ca,Cs,Sr,Mg)的含量均高于100 ppm。测得的同位素比(

著录项

  • 作者

    Acheson, Barbara Marilyn.;

  • 作者单位

    Carleton University (Canada).;

  • 授予单位 Carleton University (Canada).;
  • 学科 Geochemistry.
  • 学位 M.Sc.
  • 年度 1995
  • 页码 223 p.
  • 总页数 223
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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