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首页> 外文期刊>Talanta: The International Journal of Pure and Applied Analytical Chemistry >Development and application of new ion-exchange techniques for the separation of the platinum group and other siderophile elements from geological samples
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Development and application of new ion-exchange techniques for the separation of the platinum group and other siderophile elements from geological samples

机译:用于从地质样品中分离铂族和其他亲铁元素的新型离子交换技术的开发和应用

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摘要

Two new anion-exchange techniques have been developed for the separation of the platinum group elements Ru, Pd, Ir, Pt and the siderophile metals Re, Ag, Zn and Cd from geological samples following a NiS fire assay digestion procedure. Both methods are simple and permit the isolation of these elements in sufficient purity for quantitative analysis by isotope dilution-inductively coupled plasma mass spectrometry (ID-1CPMS) at yields of 75-95%. The high affinity of the considered elements to anion exchange resins allows the use of small (1.25 ml) columns even for the processing of 5-10 g sized silicate rock samples. Following fire assay digestion and dissolution of the NiS buttons in aqua regia, the samples are loaded onto the resin bed as solutions in 1 M HC1. After elution of the bulk sample matrix with dilute HC1 and HNO_3, Zn and Cd are stripped from the column using 0.8 M HNO_3. Small amounts of bromine water are added to the dilute mineral acids for the stabilization of strongly retained Ir(IV). Following this, the ion-exchange techniques permit the sequential elution of Ag, Re and the PGE using 11 M HC1, 8 M HNO_3 and 13.5 M HNO_3. The ion-exchange methods have been applied to separation of Ru, Pd, Re. Ir and Pt from the geological referencematerial SU-la prior to concentration measurements by ID-ICPMS. Our analytical results are in good agreement with previously published data for this sample and display an external reproducibility (based upon repeat dissolutions) of approximately 2-10% for the elements considered in this study.
机译:已经开发了两种新的阴离子交换技术,用于按照NiS火分析消解程序从地质样品中分离铂族元素Ru,Pd,Ir,Pt和嗜铁金属Re,Ag,Zn和Cd。两种方法都很简单,并且可以分离出足够纯度的这些元素,以便通过同位素稀释-电感耦合等离子体质谱法(ID-1CPMS)进行定量分析,产率为75-95%。考虑到的元素对阴离子交换树脂的高亲和力,即使在处理5-10 g大小的硅酸盐岩石样品时,也可以使用小型(1.25 ml)色谱柱。用火分析消化并溶解王水中的NiS按钮后,将样品作为1 M HCl中的溶液上样到树脂床上。用稀HCl和HNO_3洗脱大部分样品基质后,使用0.8 M HNO_3从柱中汽提Zn和Cd。将少量溴水添加到稀无机酸中,以稳定强烈保留的Ir(IV)。此后,离子交换技术允许使用11 M HCl,8 M HNO_3和13.5 M HNO_3顺序洗脱Ag,Re和PGE。离子交换方法已经应用于Ru,Pd,Re的分离。在通过ID-ICPMS进行浓度测量之前,来自地质参考物质SU-la的Ir和Pt。我们的分析结果与该样品的先前公布数据非常一致,并且对于本研究中考虑的元素而言,其外部重现性(基于重复溶解)约为2-10%。

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