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DISSOLUTION OF GOLD DURING PYRITE OXIDATION REACTION

机译:黄铁矿氧化反应期间金的溶解

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Numerous papers discuss the mechanism of alkaline oxidation of pyrite, but there is limited information available describing the kinetics of the pyrite sulphide to thiosulphate reaction. A previous investigation in this series determined the rate of sulphide oxidation and thiosulphate yield during the reaction of pyrite with sodium hydroxide under various testing conditions. The goal of the current study is to validate these rates using two different gold-containing pyrite concentrates. A further objective of the current work is to investigate the simultaneous dissolution of gold with the thiosulphate that is formed in-situ during pyrite oxidation.It was found that at 20 psi oxygen overpressure and a temperature of 80°C , the initial rates of sulphide oxidation and thiosulphate yield were close to 0.08 mol/h and 0.0155 mol/h, respectively. These rates are in agreement with previously published data. However, a shift from linearity occurred when the pH decreased below 12. A rapid decay of thiosulphate was evidenced at pH 8.3-9.2 while E_h was in the range of 22-141mV. Based on relevant thermodynamic analysis of metastable thiosalts system, such rapid decomposition is not expected at these pH and E_h values. It is believed that the presence of unreacted pyrite acting as a catalyst caused this behaviour. It appears that under mildly alkaline conditions, the rate of oxidation of sulphide to thiosulphate is slower than the rate of thiosulphate degradation, and as a result there is no significant build up of thiosulphate in solution under these conditions. The maximum extraction of gold and silver (96 and 75% respectively) was achieved under conditions of pH 10 - 12.
机译:众多论文讨论了黄铁矿碱性氧化的机制,但是有限的信息可用于描述硫化硫化物硫化物的动力学与硫代硫酸盐反应。本系列的先前研究确定了在各种试验条件下用氢氧化钠的硫铁矿反应过程中硫化物氧化和硫代硫酸盐产率。目前研究的目的是使用两种不同的含金黄铁矿浓缩物来验证这些速率。目前工作的另一个目的是研究金黄石氧化期间原位形成的硫代硫酸盐的同时溶解。发现,在20psi氧过压和80℃的温度下,硫化物的初始速率氧化和硫代硫酸盐产率分别接近0.08mol / h和0.0155mol / h。这些利率与先前发布的数据一致。然而,当pH值低于12时,在pH值下降时发生线性度的偏移。在pH 8.3-9.2中证明了硫代硫酸盐的快速衰减,而E_h在22-141mV的范围内。基于亚稳地硫磺系统的相关热力学分析,在这些pH和E_H值下预期这种快速分解。据信,存在作为催化剂的未反应的黄铁矿引起这种行为。似乎在轻度碱性条件下,硫化硫化物氧化率慢于硫代硫酸盐降解的速率,因此在这些条件下溶液中没有显着的硫代硫酸盐。在pH10-12的条件下实现金和银(96和75%)的最大提取。

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