碳质粉砂岩序次提取的ICP OES多元素分析

Medet Junussov, F. Mádai, Bánhidi Olivér
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引用次数: 2

摘要

炭质粉砂岩是Bakyrchik金矿床中一种浸染型富硫化物沉积岩。Bakyrchik矿床位于哈萨克斯坦东部,其中包括Qalba黄金省。本文的主要目的是对碳质粉砂岩中重金属的化学萃取及其元素浓度的测定进行了论证。在工作中使用了从矿床中提取的岩石样品,该样品为绢云母碳质粉砂岩。在顺序萃取法中,选择了水溶性部分(与去离子水反应)萃取水溶性金属,可还原金属部分(与氯化氢羟铵反应)萃取所有可还原金属,有机物和硫化物(与过氧化氢反应)溶解有机物和硫化铜,提取金属氧化物和残余部分(与王水反应)萃取所有剩余金属四个阶段。本文包括分析方法和研究展望。它们是x射线衍射(测定矿物成分)、x射线荧光(测定化学成分)和电感耦合等离子体-光学发射光谱法(测定重金属浓度)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sequential extraction of carbonaceous siltstone rock for multi-element analysis by ICP OES
Abstract The carbonaceous siltstone rock material is a disseminated sulfide-rich sedimentary rock from a sediment-hosted gold deposit of Bakyrchik. The Bakyrchik deposit is located in Eastern Kazakhstan, which includes in Qalba gold province. The main purpose of this paper is a demonstration on chemical extraction of heavy metals from the carbonaceous siltstone rock and detection of its elemental concentrations. In the work was used a rock sample from the deposit which is a sericizited carbonaceous-siltstone rock. In sequential extraction method was selected four stages such as water soluble fraction (reaction with deionized water) for extraction of water soluble metals, reducible metal fraction (reaction with hydroxyl ammonium chloride) for extracting all reducible metals, organics and sulfides (reaction with hydrogen peroxide) for dissolution of organics and copper sulfide, and extraction of metal oxides and residual fraction (reaction with aqua regia) for extracting of all remaining metals. The paper comprises analytical methods for research outlooks. They are X-Ray Diffraction (determination of mineralogical composition), X-Ray Fluorescence (determination of chemical composition) and Inductively Coupled Plasma – Optical Emission Spectrometry (determination of heavy metal concentrations).
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