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Thallium Mass Fraction and Stable Isotope Ratios of Sixteen Geological Reference Materials

机译:十六个地质参考材料的铊质量分数和稳定同位素比

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> Thallium stable isotope ratio and mass fraction measurements were performed on sixteen geological reference materials spanning three orders of magnitude in thallium mass fraction, including both whole rock and partially separated mineral powders. For stable isotope ratio measurements, a minimum of three independent digestions of each reference material was obtained. High‐precision trace element measurements (including Tl) were also performed for the majority of these RM s. The range of Tl mass fractions represented is 10?ng?g ?1 to 16?μg?g ?1 , and Tl stable isotope ratios (reported for historical reasons as ε 205 Tl relative to NIST SRM 997) span the range ?4 to +2. With the exception – attributed to between‐bottle heterogeneity – of G‐2, the majority of data are in good agreement with published or certified values, where available. The precision of mean of independent measurement results between independent dissolutions suggests that, for the majority of materials analysed, a minimum digested mass of 100?mg is recommended to mitigate the impact of small‐scale powder heterogeneity. Of the sixteen materials analysed, we therefore recommend for use as Tl reference materials the USGS materials BCR ‐2, COQ ‐1, GSP ‐2 and STM ‐1; CRPG materials AL ‐I, AN ‐G, FK ‐N, ISH ‐G, MDO ‐G, Mica‐Fe, Mica‐Mg and UB ‐N; NIST SRM 607 and OREAS
机译: >铊稳定同位素比和质量分数测量十六个地质参考材料,跨越铊质量分数的三个数量级,包括整体岩石和部分分离的矿物粉末。对于稳定的同位素比率测量,获得了每种参考材料的至少三种独立消化。对于大多数这些 RM> S也对高精度痕量元件测量(包括T1)进行了高精度痕量元素测量。所示的T1质量级分的范围是10?Ng?g Δ1至16Ω·μg?g α1和tl稳定同位素比(因为唯一的历史原因 205相对于 NIST SRM 997)的TL跨越范围?4至+2。除了瓶子之间的异质性 - G-2之间的例外,大多数数据与可用的公布或认证价值观吻合良好。独立分解之间的独立测量结果的平均值表明,对于分析的大部分材料,建议使用最小的100μm镁质量以减轻小规模粉末异质性的影响。在分析的十六种材料中,我们建议用作TL参考材料 USGS 材料 BCR -2, COQ -1, GSP -2和 STM -1; CRPG -I, A AN -G, FK -N, ISH -G, MDO -G,MICA-Fe,MICA-MG和 UB -N; NIST SRM 607和 OREAS

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