摘要
对黄铁矿－软锰矿浸出过程的热力学平衡进行了重新计算，并结合电化学实验及微观检测讨论了浸出反应机理，表明浸出中单质硫的生成是导致锰浸出率低的主要因素．
The thermodynamic equilibrium of the pyrite-manganese ore leaching system was recalculated. The leaching mechanism was discussed in combination with the electrochemical experiment and micromeasurement. The results show that the generation of sulphur decreases the manganese leaching rate.
出处
《化工冶金》
CSCD
北大核心
1998年第2期161-165,共5页
关键词
软锰矿
黄铁矿
浸出
热力学
电化学
硫
Manganese ore, Pyrite, Leaching mechanism, Thermodynamics, Electrochemistry
