利用 MC-ICP-MS† 从地质材料中分离铁和镁以进行同位素分析的单柱高效程序

IF 3.1 2区 化学 Q2 CHEMISTRY, ANALYTICAL
Guanhong Zhu, Zhenmin Ge, Le Zhang, Gangjian Wei and Jinlong Ma
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引用次数: 0

摘要

铁和镁同位素越来越多地成为地质过程的综合代用指标。在传统化学方法中,铁和镁同位素的测定需要对样品进行不同的分割和多柱色谱纯化,以获得纯净的镁和铁馏分,这不仅耗时,而且不适合稀有珍贵的样品。本研究提出了一种新颖高效的色谱程序,利用装有 AGMP-50 树脂的单柱从地质基质中提纯铁和镁,然后利用多收集器电感耦合等离子体质谱法(MC-ICP-MS)精确测量铁和镁的同位素。在我们的实验中,首先用 7 mL 0.2 M HCl 和 0.5 M HF 的混合物收集铁组分,然后用 9 mL 1.3 M HCl 收集镁组分。这种方法适用于处理不同类型的岩石样本,可使铁的回收率达到 98%,镁的回收率达到 100%,并能有效去除基质元素,如 Al、Ti、Na、K、Ca 和其他微量元素。利用这种方法,报告了各种地质参考材料的铁和镁同位素组成。所有的铁和镁同位素分析结果都在分析不确定性范围内与所报告的数据一致,这验证了本文所建立的方法是可靠和可重复的。因此,该方法将成为未来获取地质样本中铁和镁同位素组成以及追踪地球化学或天体化学过程的一个重要选择。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

A single-column and efficient procedure for separating Fe and Mg from geological materials for isotopic analyses using MC-ICP-MS†

A single-column and efficient procedure for separating Fe and Mg from geological materials for isotopic analyses using MC-ICP-MS†

Fe and Mg isotopes have increasingly served as combined proxies for geological processes. Fe and Mg isotope determination requires consuming different splits of samples and multi-column chromatographic purification to obtain pure Mg and Fe fractions in conventional chemical procedures, which is time-consuming and not suitable for rare and valuable samples. This study presents a novel and efficient chromatographic procedure to purify both Fe and Mg from geological matrices, using a single column loaded with AGMP-50 resin, followed by precise measurements of Fe and Mg isotopes by multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). In our experiment, the Fe fraction was first collected using 7 mL of a mixture of 0.2 M HCl and 0.5 M HF, and then the Mg fraction was collected using 9 mL of 1.3 M HCl. This procedure is suitable for processing different types of rock samples and enabling an Fe recovery of >98% and full recovery of Mg, with effective removal of matrix elements such as Al, Ti, Na, K, Ca, and other trace elements. Using this method, the Fe and Mg isotopic compositions of various geological reference materials were reported. All of the Fe and Mg isotopic analytical results were in agreement with the reported data within analytical uncertainties, verifying that the method established here is robust and reproducible. Thus, this procedure will serve as a great option for obtaining both Fe and Mg isotopic compositions of geological samples and tracing geochemical or astrochemical processes in the future.

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来源期刊
CiteScore
6.20
自引率
26.50%
发文量
228
审稿时长
1.7 months
期刊介绍: Innovative research on the fundamental theory and application of spectrometric techniques.
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