MC-ICPMS测定地质样品中Cu、Zn和Mo同位素比值的简便方法及质量偏差校正

Suzana de Souza Guedes, V. R. Bellotto, R. Santos, E. Dantas
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引用次数: 0

摘要

开发了一种简单快速的同时纯化地质样品中Cu、Zn和Mo的方法,并用多收集器电感耦合等离子体质谱法(MC-ICP-MS)准确、精确地测量了它们的同位素组成。该方法包括使用填充有阴离子交换树脂AG-MP-1的单个色谱柱来去除复杂基质并进一步纯化这三种元素。外部标准样品标准括号(SSB)程序与内部标准添加相结合,用于精确的质量偏差校正和精确的Cu、Zn和Mo同位素比率测量。该方法适用于不同的地质材料,如花岗闪长岩(GSP2-UGS)、石灰岩(JLS-1,日本)、水牛河沉积物(NIST SRM-8704)和亚马逊河流域的沉积物。这些样品的平均精度为:δ65/63Cu为0.08‰;δ66/67Zn为0.05‰,δ98/95Mo为0.04‰。主要优点是所提出的方法简单快速,可以定量回收不同原子质量和极低浓度范围的元素,主要是对Mo。此外,优化使仪器质量偏差的校准和校正更容易,从而导致与当前公布的其他方法一致的结果。将花岗闪长岩获得的Cu和Mo同位素组成与文献中报道的数据进行比较,表明本研究中开发的更简单的多元素方法可以在所需的精度范围内正确使用,作为同位素地球化学中的多代理工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A simple method for Cu, Zn and Mo purification and mass bias correction for precise and accurate isotopic ratio determination in geological samples by MC-ICPMS
A simple and quick method for simultaneous purification of Cu, Zn and Mo and accurate and precise measurement of their isotopic composition in geological samples using multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) has been developed. The method involves the use of a single chromatographic column filled with the anion exchange resin AG-MP-1 for complex matrix removal and further purification of these three elements. The external standard-sample-standard bracketing (SSB) procedure combined to internal standard addition was used for accurate mass bias correction and precise Cu, Zn and Mo isotopic ratio measurements. The method was applied to different geological materials, as granodiorite (GSP 2-USGS), limestone (JLS-1, Japan), Buffalo River Sediments (NIST SRM - 8704) and sediments from Amazon River Basin. The mean precision for these samples was: 0.08 ‰ for δ 65/63 Cu; 0.05 ‰ for δ 66/67 Zn and 0.04 ‰ for δ 98/95 Mo. The main advantage is that the proposed method is simple and rapid, and carries out the quantitative recovery of elements of different atomic masses and at very low concentration ranges, mainly for Mo. In addition, optimizations made the calibration and correction of instrumental mass bias easier, leading to consistent results with other methods that are currently published. The comparison of isotopic compositions of Cu and Mo obtained for granodiorite with respect to data reported in the literature demonstrate that the simpler and multi-element method developed in this study can be properly used within the required limits of accuracy as a multi-proxy tool in isotope geochemistry.
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