辉钼矿
铋
钼
浸出(土壤学)
化学
盐酸
分解
无机化学
冶金
核化学
材料科学
地质学
有机化学
石英
流体包裹体
土壤科学
土壤水分
作者
Yeqiong Xu,Xuheng Liu,Xingyu Chen,Jiangtao Li,Lihua He,Fenglong Sun,Zhongwei Zhao
标识
DOI:10.1016/j.seppur.2023.124218
摘要
Through thermodynamic calculations, the E-pH diagrams of the Bi-S-H2O and Bi-S-Cl-H2O systems at 298 K were plotted, the dominant regions of the components in the system and their changes with pH were clarified, and the mechanism and thermodynamic conditions for the decomposition of Bi2S3 in acidic systems were clarified. The key to the decomposition of Bi2S3 in acidic systems was based on the coordination of Cl− and Bi3+. The formation of BiCl4− can promote the decomposition of Bi2S3 in acidic systems, based on this characteristic, HCl was used to achieve efficient leaching of bismuth in molybdenite-bismuthinite mixed ore. Under the optimized conditions of hydrochloric acid concentration of 6 mol/L, liquid-to-solid ratio of 5:1, temperature of 95 °C, stirring speed of 400 rpm, and time of 300 min, the leaching efficiency of bismuth reached 97.64 %, and the bismuth content in the leaching residue was 0.93 %, while molybdenum remained in the form of MoS2 in the residue, The efficient separation of molybdenum and bismuth has been achieved, providing a new process to solve the traditional separation of molybdenite-bismuthinite mixed ores.
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