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Comparative Study on Two Pretreatment Processes for Chemical Phase Analysis of Gold in Geological Samples by Atomic Absorption Spectrometry

机译:原子吸收光谱法对地质样品中金的化学分析两种预处理方法的比较研究

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摘要

Sample pretreatment is important for chemical phase analysis of elements. In this study, the geological samples of the Laozuoshan gold mine are chosen to pretreat by ultrasonic centrifugation and cyclotron oscillation, and the content of gold in eight chemical phases (water-soluble, ion exchange and clay adsorption, organic matter bound, iron-manganese oxide bound, naked or seminaked, carbonate bound, sulfide bound, and insoluble silicate states) is determined by atomic absorption spectrometry. The results show that the gold content of water-soluble, ion exchange and clay adsorption, iron-manganese oxide, and naked or seminaked states in the rock and ore samples is low, and some samples have high gold content of insoluble silicate states in the two methods. However, the gold content of organic matter bound, carbonate bound, and sulfide bound states obtained by ultrasonic centrifugation and cyclotron oscillation methods is significantly different. According to the X-ray fluorescence spectrometry data and the actual geological condition, the result given by the cyclotron oscillation method is more reasonable. The gold content of sulfide bound state in sediment samples is the highest and consistent with the mineral information, which could be applied to preliminarily predict the rock and ore conditions in the corresponding mining areas. In contrast with ultrasonic centrifugation, the cyclotron oscillation method has the advantages of simplicity, high efficiency, practicality, and environmental protection, and it can be better used for the determination of gold chemical phase state in geological samples by atomic absorption spectrometry.
机译:样品预处理对于元素的化学相分析很重要。本研究选取老作山金矿的地质样品进行超声波离心和回旋振荡进行预处理,并在水溶性,离子交换和黏土吸附,有机物结合,铁锰等八个化学相中进行金含量测定。通过原子吸收光谱法确定氧化物键,裸键或半裸键,碳酸盐键,硫化物键和不溶性硅酸盐状态。结果表明,岩石和矿石样品中水溶性,离子交换和粘土吸附,铁锰氧化物以及裸或半裸态的金含量较低,有些样品中的不溶硅酸盐态的金含量高。两种方法。然而,通过超声离心和回旋振荡方法获得的有机物结合态,碳酸盐结合态和硫化物结合态的金含量存在显着差异。根据X射线荧光光谱数据和实际地质情况,回旋振荡方法给出的结果较为合理。沉积物样品中硫化物结合态的金含量最高,与矿物信息一致,可用于初步预测相应矿区的岩石和矿石状况。与超声离心相比,回旋振荡方法具有简便,高效,实用,环保等优点,可以更好地用于原子吸收光谱法测定地质样品中金的化学相态。

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