Density functional theory study of H2O adsorption on different sphalerite surfaces

被引:1
作者
Deng, Zheng-bin [1 ,2 ,3 ,4 ]
Tong, Xiong [4 ,5 ]
Huang, Ling-yun [4 ,5 ]
Xie, Xian [4 ,5 ]
机构
[1] Guizhou Univ, Min Coll, Guiyang 550025, Guizhou, Peoples R China
[2] Guizhou Univ, Natl & Local Joint Lab Engn Effect Utilizat Reg M, Guiyang 550025, Guizhou, Peoples R China
[3] Guizhou Univ, Guizhou Key Lab Comprehens Utilizat Nonmetall Min, Guiyang 550025, Guizhou, Peoples R China
[4] Kunming Univ Sci & Technol, State Key Lab Complex Nonferrous Met Resources Cl, Kunming 650093, Yunnan, Peoples R China
[5] Kunming Univ Sci & Technol, Fac Land & Resource Engn, Kunming 650093, Yunnan, Peoples R China
来源
PHYSICOCHEMICAL PROBLEMS OF MINERAL PROCESSING | 2019年 / 55卷 / 01期
基金
芬兰科学院;
关键词
density functional theory; sphalerite; water adsorption; hydrophobicity;
D O I
10.5277/ppmp18111
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Effects of In, Ge, Fe substitution in the lattice of sphalerite on wettability were usually ignored, therefore the optimal flotation condition could be difficult to find due to lacking of sufficient theoretical study on water adsorption, resulting lower recoveries of different sphalerites. Adsorption of H2O on different sphalerite surfaces was studied using density functional theory (DFT) method. All computational models were built in a vacuum environment to eliminate the effects of oxygen and other factors. H2O molecule prefers to stay with ideal sphalerite, indium-beard sphalerite, germanium-beard sphalerite and marmatite surfaces rather than water. Compared with ideal sphalerite surface, Fe atom improves the hydrophilicity of surface, while In and Ge atoms reduce the hydrophilicity.
引用
收藏
页码:82 / 88
页数:7
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