原文服务方: 地球化学学报(英文)       
摘要:
Element doping has been proved to be a useful method to correct for the mass bias fractionation when analyzing iron isotope compositions. We present a systematic re-assessment on how the doped nickel may affect the iron isotope analysis in this study by carrying out several experiments. We find three important factors that can affect the analytical results, including the Ni:Fe ratio in the analyte solutions, the match of the Ni:Fe ratio between the unknown sample and standard solutions, and the match of the Fe concentration between the sample and standard solutions. Thus, caution is required when adding Ni to the analyte Fe solutions before analysis. Using our method, the δ56Fe and δ57Fe values of the USGS standards W-2a, BHVO-2. BCR-2. AGV-2 and GSP-2 are consistent with the recommended literature values, and the long-term (one year) external reproducibility is better than 0.03 and 0.05‰(2SD) for δ56Fe and δ57Fe, respectively. Therefore, the analytical method established in our laboratory is a method of choice for high quantity Fe isotope data in geological materials.
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篇名 A re-assessment of nickel-doping method in iron isotope analysis on rock samples using multi-collect
来源期刊 学科 地球科学
关键词 Fe isotope Ni-doping Stable isotope Precision and accuracy Mass bias correction Pseudo-high mass resolution
年,卷(期) 2022,(3) 所属期刊栏目
研究方向 页码范围 355-364
页数 9页 分类号
字数 语种 英文
DOI 10.1007/s11631-020-00402-w
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Fe isotope
Ni-doping
Stable isotope
Precision and accuracy
Mass bias correction
Pseudo-high mass resolution
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地球化学学报(英文)
双月刊
2096-0956
52-1161/p
16开
贵阳市林城西路99号
1982-01-01
英语
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230
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