ns-LA-MC-ICP-MS法测定锆石标准物质硅同位素组成

IF 3.3 2区 化学 Q2 CHEMISTRY, ANALYTICAL
Ze-Pei Yuan, Jin-Cheng Xie, Di-Cheng Zhu, Qing Wang, Liang-Liang Zhang, Li-Juan Xu, Xin-Yu Liang and Xia Qi
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引用次数: 0

摘要

硅同位素是研究地壳循环过程和板块构造动力学的有力地球化学示踪剂。虽然在原位Si同位素分析方面取得了重大进展,但激光参数对原位Si同位素测量精度和精度的影响以及分析过程中的基体效应仍有待系统研究和解决。本研究利用纳秒激光烧蚀(ns-LA)和多收集器电感耦合等离子体质谱(MC-ICP-MS)对原位硅同位素方法进行了优化。综合实验结果表明,激光重复频率为4-14 Hz,能量密度超过1.5 J cm−2,光斑尺寸为33-90µm是获得锆石参考物质MTUR1足够信号强度的理想条件。MTUR1锆石长期单点烧蚀和线扫描烧蚀所得δ30Si的外部重现性分别为0.26‰和0.11‰(2SD)。在非基质匹配的Si同位素分析中,持续观察到显著的基质效应。虽然在烧蚀池前引入水和z轴位置调整部分抑制了基体效应,但仍然存在相当大的分析偏差。我们将优化后的方法应用于天然和合成锆石标准物质(91 500、Plešovice、SA01、GJ-1、Tanz、蓬莱、班-1、青湖、GHR1和吉林)的检测。除mun -锆石的δ30Si值为- 2.10±0.64‰(2SD)外,其余锆石的δ30Si值相对均匀,范围为- 0.71±0.21‰~ - 0.29±0.13‰(2SD)。我们的数据揭示了青湖、LKZ-1、吉林、Temora-2、GHR1和MUN-zircon锆石参考物质中硅同位素组成在粒内和粒间的显著变化,表明这些材料的硅同位素数据有望追踪岩浆分异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Determination of silicon isotopic composition of zircon reference materials by ns-LA-MC-ICP-MS

Determination of silicon isotopic composition of zircon reference materials by ns-LA-MC-ICP-MS

Silicon isotopes serve as powerful geochemical tracers for elucidating crustal recycling processes and plate tectonic dynamics. Although significant progress has been made in in situ Si isotope analysis, the influence of laser parameters on the accuracy and precision of in situ Si isotope measurements, as well as the matrix effects during the analytical process, remains to be systematically investigated and resolved. This study optimized the in situ Si isotope method using nanosecond laser ablation (ns-LA) coupled with multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). Our results of comprehensive tests indicated that a laser repetition rate of 4–14 Hz, an energy density exceeding 1.5 J cm−2, and a spot size of 33–90 µm are ideal conditions to obtain adequate signal intensity for the zircon reference material MTUR1. The external reproducibility of δ30Si obtained by long-term single spot and line scan ablation of MTUR1 zircon was 0.26‰ and 0.11‰ (2SD), respectively. Significant matrix effects were consistently observed during non-matrix-matched Si isotope analysis. Although the introduction of water before the ablation cell and Z-axis position adjustment partially suppressed matrix effects, considerable analytical bias remained. We applied this optimized method to examine natural and synthetic zircon reference materials (e.g., 91 500, Plešovice, SA01, GJ-1, Tanz, Penglai, Ban-1, Qinghu, GHR1, and Jilin). In addition to MUN-zircon, which yielded a δ30Si value of −2.10 ± 0.64‰ (2SD), the other zircon reference materials gave relatively homogeneous Si isotopic compositions, with δ30Si values ranging from −0.71 ± 0.21‰ to −0.29 ± 0.13‰ (2SD). Our data reveal significant intra- and inter-grain variations in Si isotopic composition within the Qinghu, LKZ-1, Jilin, Temora-2, GHR1, and MUN-zircon zircon reference materials, indicating that Si isotopic data from these materials hold promise for tracing magmatic differentiation.

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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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