Behavior of ammonium adsorption by clay mineral halloysite

被引:59
作者
Jing, Qing-xiu [1 ,2 ]
Chai, Li-yuan [1 ]
Huang, Xiao-dong [2 ]
Tang, Chong-jian [1 ]
Guo, Huan [2 ]
Wang, Wei [2 ]
机构
[1] Cent S Univ, Sch Met & Environm, Changsha 410083, Hunan, Peoples R China
[2] Jiangxi Univ Sci & Technol, Sch Met & Chem Engn, Ganzhou 341000, Peoples R China
基金
中国国家自然科学基金;
关键词
ionic rare earth mining area; halloysite; ammonium pollution; adsorption; dynamics; RARE-EARTH ORE; AQUEOUS-SOLUTIONS; REMOVAL; NANOTUBES; WATER; IONS; EQUILIBRIUM; KINETICS; CHITOSAN; ELEMENTS;
D O I
10.1016/S1003-6326(17)60185-7
中图分类号
TF [冶金工业];
学科分类号
0806 ;
摘要
Ammonium pollution becomes severe during mining of ionic rare earth-ores in southern China. As one of the main clay minerals in soils of ionic rare earth mines, halloysite plays an important role in ammonium adsorption. In this study, the saturated adsorption capacity, factors affecting adsorption and adsorption kinetics of halloysite for ammonium were investigated. The results indicated that the ammonium adsorption of halloysite was saturated with 1.66 mg/g at 303 K, pH of 5.6 and initial ammonium concentration of 600 mg/L (about half of the actual initial in-situ leaching concentration). When the initial concentration of NH4| -N, pH values and temperatures (288 K to 313 K) increased, the ammonium adsorption capacity of halloysite increased. The ammonium isothermal adsorption of halloysite matched the Langmuir and Freundlich isotherms. The adsorption process of ionic rare earth mining soils for ammonium was favorable. And the adsorption process followed closely the pseudo-second kinetic equation.
引用
收藏
页码:1627 / 1635
页数:9
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