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首页> 外文期刊>Geostandards and geoanalytical research >Determination of Platinum-Group Elements in Geological Samples by Isotope Dilution-Inductively Coupled Plasma-Mass Spectrometry Combined with Sulfide Fire Assay Preconcentration
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Determination of Platinum-Group Elements in Geological Samples by Isotope Dilution-Inductively Coupled Plasma-Mass Spectrometry Combined with Sulfide Fire Assay Preconcentration

机译:同位素稀释-电感耦合等离子体质谱-硫化物火法预浓集法测定地质样品中的铂族元素

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摘要

A method was developed for the determination of platinum-group elements (PGE) in geological samples by isotope dilution-inductively coupled plasma-mass spectrometry combined with sulfide fire assay preconcentration. Samples were fused and PGE analytes were concentrated in sulfide buttons. The buttons were dissolved using HCl leaving PGE analytes in insoluble residues, which were digested in HNO3 and simultaneously processed for the distillation of Os. The remaining solutions were further prepared for the purification of Ru, Rh, Pd, Ir and Pt using a tandem assembly of cation and Ln resin columns. The eluents were directly analysed by membrane desolvation-ICP-MS. Ruthenium, Pd, Os, Ir and Pt were determined by isotope dilution, whereas Rh was determined by conventional reference material calibration combined with Ir-193 as the internal standard element. The method was validated using a series of PGE reference materials, and the measurement data were consistent with the recommended and the literature values. The measurement precision was better than 10% RSD. The procedural blanks were 0.121ng for Ru, 0.204 for Rh, 0.960ng for Pd, 0.111ng for Os, 0.045ng for Ir and 0.661ng for Pt, and the limits of detection (3s) were 0.011ng g(-1) for Ru, 0.008ng g(-1) for Rh, 0.045ng g(-1) for Pd, 0.009ng g(-1) for Os, 0.006ng g(-1) for Ir and 0.016ng g(-1) for Pt when a test portion mass of 10g was used. This indicates that the proposed method can be used for the determination of trace amounts of PGE in geological samples.
机译:建立了一种通过同位素稀释-电感耦合等离子体质谱联用硫化物着火法预富集测定地质样品中铂族元素(PGE)的方法。融合样品并将PGE分析物浓缩在硫化纽扣中。用HCl溶解纽扣,使PGE分析物留在不溶残留物中,将其在HNO3中消化,同时进行Os蒸馏处理。使用阳离子和Ln树脂柱的串联组件进一步制备剩余的溶液,以纯化Ru,Rh,Pd,Ir和Pt。通过膜去溶剂化-ICP-MS直接分析洗脱液。钌,Pd,Os,Ir和Pt是通过同位素稀释来确定的,而Rh是通过常规参考材料校准结合Ir-193作为内标元素来确定的。该方法已使用一系列PGE参考材料进行了验证,测量数据与推荐值和文献值一致。测量精度优于10%RSD。程序空白为Ru的0.121ng,Rh的0.204ng,Pd的0.960ng,Os的0.111ng,Ir的0.045ng和Pt的0.661ng,检测限为0.011ng g(-1)。 Ru,Rh 0.008ng g(-1),Pd 0.045ng g(-1),Os 0.009ng g(-1),Ir 0.006ng g(-1)和0.016ng g(-1)使用10 g的测试份质量时的Pt。这表明该方法可用于测定地质样品中痕量的PGE。

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