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In this study the homogeneity of the zinc isotopic composition in the NIST SRM 683 reference material was examined by measuring the Zn isotopic signature in microdrilled sample powders from two metal nuggets. Zinc was purified using AG MP ‐1M resin and then measured by MC ‐ ICP ‐ MS . Instrumental mass bias was corrected using the “sample‐standard bracketing” method and empirical external normalisation with Cu doping. After evaluating the potential effects of varying acid mass fractions and different matrices, high‐precision Zn isotope data were obtained with an intermediate measurement precision better than ± 0.05‰ (δ 66 Zn, 2 s ) over a period of 5 months. The δ 66 Zn JMC ‐Lyon mean values of eighty‐four and fourteen drilled powders from two nuggets were 0.11 ± 0.02‰ and 0.12 ± 0.02‰, respectively, indicating that NIST SRM 683 is a good isotopic reference material with homogeneous Zn isotopes. The Zn isotopic compositions of seventeen rock reference materials were also determined, and their δ 66 Zn values were in agreement with most previously published data within 2 s . The δ 66 Zn values of most of the rock reference materials analysed were in the range 0.22–0.36‰, except for GSP ‐2 (1.07 ± 0.06‰, n = 12), NOD ‐A‐1 (0.96 ± 0.03‰, n = 6) and NOD ‐P‐1 (0.78 ± 0.03‰, n = 6). These comprehensive data should serve as reference values for quality assurance and interlaboratory calibration exercises.
Chen et al. (Sat,) studied this question.