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Sample Digestion and Combined Preconcentration Methods for the Determination of Ultra-Low Gold Levels in Rocks

机译:样品消解和联合富集方法测定岩石中超低金含量

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摘要

The gold abundance in basic rocks, which normally varies between 0.5 and 5 ppb, has served as a very important indicator in many geoscience studies, including those focused on the planetary differentiation, redistribution of elements during the crustal process, and ore genesis. However, because gold is a monoisotopic element that exhibits a nugget effect, it is very difficult to quantify its ultra-low levels in rocks, which significantly limits our understanding of the origin of gold and its circulation between the Earth crust, mantle, and core. In this work, we summarize various sample digestion and combined preconcentration methods for the determination of gold amounts in rocks. They include fire assay, fire assay combined with Te coprecipitation and instrumental neutron activation analysis (INAA) or laser ablation inductively coupled plasma mass spectrometry, fusion combined with Te coprecipitation and anion exchange resins, dry chlorination, wet acid digestion combined with precipitation, ion exchange resins, solvent extraction, polyurethane foam, extraction chromatography, novel solid adsorbents, and direct determination by INAA. In addition, the faced challenges and future perspectives in this field are discussed.
机译:基本岩石中的金含量通常在0.5 ppb和5 ppb之间变化,已成为许多地球科学研究中非常重要的指标,包括那些侧重于行星分化,地壳过程中元素的重新分布以及矿石成因的研究。但是,由于金是一种具有同位素效应的单同位素元素,因此很难量化其在岩石中的超低含量,这极大地限制了我们对金的起源及其在地壳,地幔和岩心之间的循环的理解。 。在这项工作中,我们总结了用于确定岩石中金量的各种样品消解和组合的预浓缩方法。其中包括着火测定,结合Te共沉淀和仪器中子活化分析(INAA)的火测定,激光烧蚀电感耦合等离子体质谱,结合Te共沉淀和阴离子交换树脂的融合,干式氯化,湿酸消化结合沉淀,离子交换树脂,溶剂萃取,聚氨酯泡沫,萃取色谱,新型固体吸附剂,以及通过INAA直接测定。此外,讨论了该领域面临的挑战和未来前景。

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