【引用本文】 秦燕, 徐衍明, 侯可军, 等. 铁同位素分析测试技术研究进展[J]. 岩矿测试, 2020, 39(2): 151-161. doi: 10.15898/j.cnki.11-2131/td.201908120120
QIN Yan, XU Yan-ming, HOU Ke-jun, et al. Progress of Analytical Techniques for Stable Iron Isotopes[J]. Rock and Mineral Analysis, 2020, 39(2): 151-161. doi: 10.15898/j.cnki.11-2131/td.201908120120



自然资源部成矿作用与资源评价重点实验室, 中国地质科学院矿产资源研究所, 北京 100037


青岛地质工程勘察院(青岛地质勘查开发局), 山东 青岛 266071

收稿日期: 2019-08-12  修回日期: 2019-09-17  接受日期: 2019-10-21

基金项目: 中央级公益性科研院所基本科研业务费专项(JYYWF20180104)

作者简介: 秦燕, 博士, 副研究员, 主要研究方向为同位素地球化学。E-mail:happyqinyan@sina.com

通信作者: 侯可军, 博士, 副研究员, 主要研究方向为同位素地球化学。E-mail:kejunhou@126.com

Progress of Analytical Techniques for Stable Iron Isotopes


Key Laboratory of Metallogeny and Mineral Assessment, Ministry of National Resources; Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China


Qingdao Geological Engineering Survey Institute(Qingdao Geological Exploration and Development Bureau), Qingdao 266071, China

Corresponding author: HOU Ke-jun, kejunhou@126.com

Received Date: 2019-08-12
Revised Date: 2019-09-17
Accepted Date: 2019-10-21


关键词: 铁同位素, 化学提纯, 溶液法, 质谱, 激光剥蚀, 基体效应


(1) 总结了铁同位素测试技术的研究进展。

(2) 归纳了测试过程产生同位素分馏的机制和校正方法。

(3) 对比了溶液法和微区原位铁同位素测试方法的优缺点。

Progress of Analytical Techniques for Stable Iron Isotopes



Iron is the most abundant element on earth with variable valences. It is widely distributed in various minerals, rocks, fluids and organisms, and is involved in diagenesis, mineralization, hydrothermal activities and life activities. The study of iron isotope composition provides important information for geochemistry, astrochemistry and biochemistry. The accurate measurement of Fe isotopes is an important basis for the development of related research.


To summarize the research progress of Fe isotope measurement technology.


The current chemical separation and purification methods and main instrumental analysis techniques commonly used for iron isotopes, were compared and analyzed in this review, and the mechanism of different types of fractionations during mass spectrometry were discussed. These advances included:(1) Improvement of anion resin during determination of iron isotope by solution method; (2) Mass spectrometry development from traditional thermal ionization mass spectrometry to multi-collector inductively coupled plasma mass spectrometry; (3) Development of laser in situ analytical technology. On this basis, the steps and calibration methods that would cause iron isotope fractionation during the analysis were summarized, and the advantages and disadvantages of different analytical methods were reviewed.


The analysis process of solution method was long and complicated, but the precision was high (0.03‰, 2SD) and the method was stable. In situ iron isotope analysis method developed from nanosecond laser denudation to femtosecond laser denudation, with shorter pulse duration, higher pulse peak intensity (up to 1012W), and focusing intensity exceeding 1020W/cm2. In situ iron isotope analysis method was fast and had high spatial resolution, which can be used to discuss the geochemical process from the microscopic perspective. However, the presence of matrix effects limited the widespread use of iron isotopes.


Shortening solution analysis process and developing a series of matrix-matched standard samples are the research direction of iron isotope analysis.

KEY WORDS: iron isotope, chemical separation, solution method, mass spectrometry, laser ablation, matrix effect


(1) Recent advances in Fe isotope analyses were reviewed.

(2) The mechanism and correction method of isotopic fractionation during mass spectrometry analysis were summarized.

(3) The advantages and disadvantages of solution and in situ methods for Fe isotope analyses were compared.



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