Introducing MC-MICAP-MS: using a N2-based plasma ion source for Sr isotope abundance ratio measurements

IF 3.1 2区 化学 Q2 CHEMISTRY, ANALYTICAL
Anika Retzmann, Ashok Menon and Michael E. Wieser
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Abstract

High-precision metal(loid) isotope abundance ratios are a powerful research tool across various disciplines. These ratios are typically measured using multi-collector mass spectrometry with ion sources such as gas source, thermal ionization, or inductively coupled plasma (i.e., IRMS, TIMS, and MC-ICP-MS). This study presents the first integration of the recently developed microwave inductively coupled atmospheric-pressure plasma (MICAP) ion source, which sustains a plasma using N2, with a multi-collector mass spectrometer and offers the first characterization of the resulting MC-MICAP-MS instrument for high-precision metal isotope abundance ratio measurements. The performance of the MC-MICAP-MS instrument was evaluated by measuring Sr isotope abundance ratios and directly comparing the results with those obtained using established technology (i.e., MC-ICP-MS) with an Ar-ICP as the ion source. Initial results using the MICAP ion source show that the 87Sr/86Sr intensity ratio precision (approx. 0.007%) and the repeatability of the 87Sr/86Sr intensity ratio (approx. 0.010%), as well as the intermediate precision of the conventional 87Sr/86Sr isotope abundance ratio (approx. 0.0013%) are fully comparable to those of conventional MC-ICP-MS systems. The instrumental isotopic fractionation (IIF) observed for the new MC-MICAP-MS instrument was predominantly mass-dependent for Sr. This allowed the successful application of common IIF correction strategies, such as internal normalisation and standard-sample bracketing, for the determination of Sr isotope abundance ratios. The conventional 87Sr/86Sr isotope abundance ratios and δ88Sr/86SrSRM987 values measured for various geological and biological reference materials (i.e., seawater, basalt, slate, and bone) using MC-MICAP-MS were consistent with previously reported values obtained from established technologies such as TIMS and MC-ICP-MS. Overall, this study demonstrates that MICAP is an applicable and viable alternative ion source for multi-collector mass spectrometry, maintaining both double-focusing properties and high-precision performance without compromising the accuracy and reliability of the measurement results.

Abstract Image

MC-MICAP-MS:利用n2基等离子体离子源测量Sr同位素丰度比
高精度金属同位素丰度比是跨学科研究的有力工具。这些比率通常使用多收集器质谱法测量,离子源如气源、热电离或电感耦合等离子体(即IRMS、TIMS和MC-ICP-MS)。本研究首次将最近开发的微波电感耦合大气压等离子体(MICAP)离子源与多收集器质谱仪集成,该质谱仪使用氮气维持等离子体,并首次对用于高精度金属同位素丰度比测量的MC-MICAP-MS仪器进行了表征。MC-MICAP-MS仪器的性能通过测量Sr同位素丰度比来评估,并直接将结果与使用Ar-ICP作为离子源的现有技术(即MC-ICP-MS)获得的结果进行比较。使用MICAP离子源的初步结果表明,87Sr/86Sr的强度比精度约为。0.007%)和87Sr/86Sr强度比的重复性(约为0.007%)。0.010%),以及常规87Sr/86Sr同位素丰度比(约为0.010%)的中间精度。0.0013%)与传统的MC-ICP-MS系统完全相当。新的MC-MICAP-MS仪器观测到的仪器同位素分馏(IIF)主要依赖于Sr的质量。这允许成功应用常见的IIF校正策略,如内部归一化和标准样品包套,以确定Sr同位素丰度比。MC-MICAP-MS测量的各种地质和生物参考物质(即海水、玄武岩、板岩和骨骼)的常规87Sr/86Sr同位素丰度比和δ88Sr/86SrSRM987值与TIMS和MC-ICP-MS等现有技术获得的结果一致。总体而言,本研究表明MICAP是一种适用且可行的多收集器质谱替代离子源,在不影响测量结果的准确性和可靠性的情况下保持双聚焦特性和高精度性能。
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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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