Hydrothermal precipitation of hematite from the model solution of zinc hydrometallurgical extraction

被引:0
|
作者
Li, Chunlin [1 ,2 ]
Deng, Zhigan [1 ,2 ]
Yang, Fuxian [1 ,2 ]
Wei, Chang [1 ,2 ]
Li, Xingbin [1 ,2 ]
Li, Minting [1 ,2 ]
机构
[1] Kunming Univ Sci & Technol, Fac Met & Energy Engn, Kunming 650093, Peoples R China
[2] State Key Lab Complex Nonferrous Met Resources Cle, Kunming 650093, Peoples R China
基金
中国国家自然科学基金;
关键词
hematite; precipitation; particle size distribution; zinc hydrometallurgy; silicon; PARTICLE-SIZE; SULFATE; ALPHA-FE2O3; CONDUCTIVITY; HYDROLYSIS; SILICATE; KINETICS; PRODUCT;
D O I
10.1515/ijcre-2023-0073
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
The effect of temperature and silicon concentration on iron precipitation and morphology of hematite particles was discussed. The results showed that increase of initial silicon centration will lead to the decrease of iron removal efficiency, and the Fe content decreases and S content increases in hematite. Increasing temperature is beneficial to increase iron removal rate and Fe content in hematite, but increasing temperature can not decrease silicon content in hematite. The content of Si in precipitate is proportional to the concentration of silicon in solution. Silicon is adsorbed on the surface of hematite in the form of silicic acid. Hematite particle was agglomerated microsphere. Increasing concentration of silicon will increase the disorder degree of hematite crystallization. With the increase of silicon concentration, the agglomeration of hematite particle was more obvious, and the average particle size of hematite particles increased. At 175 C-degrees, the morphology of iron precipitation particles are composed of flake particles and rhomboid massive particles, but when the temperature rises to 195 degrees C, the agglomeration phenomenon is obvious, small flake particles agglomerate into microspherical aggregates.
引用
收藏
页码:299 / 309
页数:11
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