Preliminary Characterisation of New Reference Materials (CaW-0, CaW-1 and CaW-3) for Microanalysis of Rare Earth Elements in Scheelite by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry

IF 2.7 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Yu Zhang, Shiyong You, Fuwen Tan, Jianfeng Shao, Jianzong Zhou, Tengfei Zheng, Wenxian Yi, Ping Xia, Lanlan Jin, Haitao Li, Ruixiang Wang, Herui Wen, Yuqiu Ke, Yijian Sun
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Abstract

In this work, we prepared three CaWO4 single crystals (CaW-0, CaW-1 and CaW-3) doped with rare earth elements (REEs) at nominal mass fractions of 50, 250 and 5000 μg g-1 using the Czochralski method. Electron probe microanalysis (EPMA) and laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) were employed to evaluate the within- and between-unit homogeneity of major elements and REEs, respectively. The within-unit variation (sr) of 0.40–0.84% and between-unit sr of 0.14–1.48% for major elements were obtained. Within- and between-unit sr of 0.53–5.56% were also found for REEs by LA-ICP-MS spot analyses. A comparison of the sr of repeat analyses was compared with the analytical uncertainty (u), i.e., the mean square weighted deviation (MSWD), which is close to or slightly higher than 1, indicating that no obvious chemical heterogeneity was found in these crystals. Reference values for these elements were obtained through various analytical methods across four different laboratories and applications of the reference materials to calibrating REE mass fractions in a natural scheelite were performed. No significant difference of the results was found as t values are less than 2.75 at the 99% confidence interval. The excellent linearity (R2 > 0.98) between the REE mass fractions and both LA-ICP-MS signal intensity and wafer absorbance was found, but the crater height and the absolute mass transported into ICP-MS decreased when REE mass fractions as well as the colour of crystals increased. These results suggest that the reference materials have the potential to calibrate REE mass fractions in natural scheelite.

Abstract Image

通过激光烧蚀-电感耦合等离子体-质谱法显微分析白钨矿中稀土元素的新标准物质(CaW-0、CaW-1 和 CaW-3)的初步表征
在这项工作中,我们用Czochralski法制备了三种稀土元素(CaW-0, CaW-1和CaW-3)掺杂的caw - 4单晶,标称质量分数分别为50,250和5000 μg -1。采用电子探针微量分析(EPMA)和激光烧蚀-电感耦合等离子体质谱(LA-ICP-MS)分别评价了样品中主要元素和稀土元素的单位内和单位间均匀性。主要元素的单位内变异(sr)为0.40 ~ 0.84%,单位间变异(sr)为0.14 ~ 1.48%。通过LA-ICP-MS斑点分析,发现稀土元素的单位内和单位间sr为0.53 ~ 5.56%。将重复分析的sr与分析不确定度(u),即均方加权偏差(MSWD)进行比较,u接近或略高于1,表明这些晶体中没有发现明显的化学非均质性。通过四个不同实验室的不同分析方法获得了这些元素的参考值,并应用参考物质校准了天然白钨矿中的稀土元素质量分数。在99%的置信区间t值小于2.75,结果没有发现显著差异。结果表明,稀土元素质量分数与LA-ICP-MS信号强度和晶圆吸光度呈良好的线性关系(R2 > 0.98),但随着稀土元素质量分数的增加和晶体颜色的增加,陨石坑高度和传递到ICP-MS中的绝对质量减小。这些结果表明,该标准物质具有校准天然白钨矿稀土质量分数的潜力。
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来源期刊
Geostandards and Geoanalytical Research
Geostandards and Geoanalytical Research 地学-地球科学综合
CiteScore
7.10
自引率
18.40%
发文量
54
审稿时长
>12 weeks
期刊介绍: Geostandards & Geoanalytical Research is an international journal dedicated to advancing the science of reference materials, analytical techniques and data quality relevant to the chemical analysis of geological and environmental samples. Papers are accepted for publication following peer review.
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