首页> 外文期刊>Journal of Analytical Atomic Spectrometry >Use of Ga for mass bias correction for the accurate determination of copper isotope ratio in the NIST SRM 3114 Cu standard and geological samples by MC-ICPMS
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Use of Ga for mass bias correction for the accurate determination of copper isotope ratio in the NIST SRM 3114 Cu standard and geological samples by MC-ICPMS

机译:使用Ga进行质量偏差校正,以通过MC-ICPMS准确测定NIST SRM 3114 Cu标准品和地质样品中的铜同位素比

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摘要

The absolute determination of the Cu isotope ratio in NIST SRM 3114 based on a regression mass bias correction model is performed for the first time with NIST SRM 944 Ga as the calibrant. A value of 0.4471 ± 0.0013 (2SD, n = 37) for the ~(65)Cu/~(63)Cu ratio was obtained with a value of +0.18 ± 0.04‰ (2SD, n = 5) for δ~(65)Cu relative to NIST 976. The availability of the NIST SRM 3114 material, now with the absolute value of the ~(65)Cu/~(63)Cu ratio and a δ~(65)Cu value relative to NIST 976 makes it suitable as a new candidate reference material for Cu isotope studies. In addition, a protocol is described for the accurate and precise determination of δ~(65)Cu values of geological reference materials. Purification of Cu from the sample matrix was performed using the AG MP-1M Bio-Rad resin. The column recovery for geological samples was found to be 100 ± 2% (2SD, n = 15). A modified method of standard-sample bracketing with internal normalization for mass bias correction was employed by adding natural Ga to both the sample and the solution of NIST SRM 3114, which was used as the bracketing standard. An absolute value of 0.4470 ± 0.0013 (2SD, n = 37) for ~(65)Cu/~(63)Cu quantified in this study was used to calibrate the ~(69)Ga/~(71)Ga ratio in the two adjacent bracketing standards of SRM 3114, their average value of ~(69)Ga/~(71)Ga was then used to correct the ~(65)Cu/~(63)Cu ratio in the sample. Measured 5~(65)Cu values of 0.18 ± 0.04‰ (2SD, n = 20), 0.13 ± 0.04‰ (2SD, n = 9), 0.08 ± 0.03‰ (2SD, n = 6), 0.01 ± 0.06 (2SD, n = 4) and 0.26 ± 0.04‰ (2SD, n = 7) were obtained for five geological reference materials of BCR-2. BHVO-2, AGV-2, BIR-1a, and GSP-2, respectively, in agreement with values obtained in previous studies.
机译:基于NIST SRM 944 Ga作为校准物,首次基于回归质量偏差校正模型对NIST SRM 3114中的Cu同位素比进行绝对确定。 〜(65)Cu /〜(63)Cu比的值为0.4471±0.0013(2SD,n = 37),δ〜(65)的值为+0.18±0.04‰(2SD,n = 5)铜相对于NIST976。NIST SRM 3114材料的可用性,现在具有〜(65)Cu /〜(63)Cu比的绝对值和相对于NIST 976的δ〜(65)Cu值适合作为Cu同位素研究的新候选参考材料。此外,描述了一种协议,用于准确和精确地确定地质参考材料的δ〜(65)Cu值。使用AG MP-1M Bio-Rad树脂从样品基质中纯化Cu。发现地质样品的色谱柱回收率为100±2%(2SD,n = 15)。通过对样品和NIST SRM 3114溶液添加天然Ga并使用自然归一化方法对标准样品进行包围校正,并采用内部归一化进行质量偏差校正,该方法用作包围标准。本研究中定量的〜(65)Cu /〜(63)Cu的绝对值为0.4470±0.0013(2SD,n = 37),用于校准两个样品中的〜(69)Ga /〜(71)Ga比与SRM 3114的括号标准相邻,它们的〜(69)Ga /〜(71)Ga平均值用于校正样品中的〜(65)Cu /〜(63)Cu比。测得的5〜(65)Cu值分别为0.18±0.04‰(2SD,n = 20),0.13±0.04‰(2SD,n = 9),0.08±0.03‰(2SD,n = 6),0.01±0.06(2SD) ,五个BCR-2地质参考物质的n = 4)和0.26±0.04‰(2SD,n = 7)。 BHVO-2,AGV-2,BIR-1a和GSP-2分别与先前研究中获得的值一致。

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  • 来源
    《Journal of Analytical Atomic Spectrometry》 |2016年第1期|280-287|共8页
  • 作者单位

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China;

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China;

    Chemical Metrology, Measurement Science and Standards, National Research Council Canada, Ottawa, Ontario, Canada K1A 0R6;

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