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

Author:

Zhang Yu123,You Shiyong12,Tan Fuwen12,Shao Jianfeng12,Zhou Jianzong4,Zheng Tengfei12,Yi Wenxian12,Xia Ping12,Jin Lanlan4,Li Haitao4,Wang Ruixiang3,Wen Herui25,Ke Yuqiu123ORCID,Sun Yijian25

Affiliation:

1. Key Laboratory of Testing and Tracing of Rare Earth Products for State Market Regulation, Faculty of Materials Metallurgy and Chemistry Jiangxi University of Science and Technology Ganzhou 341000 P.R. China

2. Jiangxi Provincial Key Laboratory of Functional Molecular Materials Chemistry, Faculty of Materials Metallurgy and Chemistry Jiangxi University of Science and Technology Ganzhou 341000 P.R. China

3. Key Laboratory of Ionic Rare Earth Resources and Environment, Ministry of Natural Resources, Faculty of Materials Metallurgy and Chemistry Jiangxi University of Science and Technology Ganzhou 341000 P.R. China

4. State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences China University of Geosciences Wuhan 430074 P.R. China

5. National Rare Earth Functional Material Innovation Center Ganzhou 341000 P.R. China

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.

Funder

National Key Research and Development Program of China

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology,Geochemistry and Petrology,Geology

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