Vertical distribution and occurrence state of the residual leaching agent (ammonium sulfate) in the weathered crust elution-deposited rare earth ore

被引:24
|
作者
Huang, Shuxin [1 ]
Li, Zhanhui [1 ]
Yu, Junxia [1 ]
Feng, Jian [1 ]
Hou, Haobo [2 ,3 ]
Chi, Ruan [1 ]
机构
[1] Wuhan Inst Technol, Sch Chem & Environm Engn, Minist Educ,Key Lab Green Chem Proc,Minist Educ, Hubei Novel Reactor & Green Chem Technol Key Lab, Wuhan 430074, Peoples R China
[2] Wuhan Univ Zhaoqing, GD HK & MO Environ Technol Res INST, Zhaoqing, Guangdong, Peoples R China
[3] Wuhan Univ, Sch Resource & Environm Sci, Wuhan 430072, Hubei, Peoples R China
关键词
Residual ammonium; Weathered crust elution-deposited rare earth ore; Distribution; Elution; CLAY-MINERALS; FIXED AMMONIUM; SOIL; ELEMENTS; ALUMINUM; NITROGEN; MINERALIZATION; ADSORBENTS; COMPOUND; KINETICS;
D O I
10.1016/j.jenvman.2021.113642
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Weathered crust elution-deposited rare earth ore (WCE-DREO) are rich in middle and heavy rare earth, and ammonium sulfate ((NH4)(2)SO4) was often used as leaching agent to leach rare earths by in-situ leaching method. However, much of (NH4)(2)SO4 would remained in the ore body during the leaching process, and release of it would cause seriously environmental pollution after the mine closure. To efficiently remove it, the rare earth ore properties and vertical distribution and occurrence state of the residual leaching agent at mine roof (GP1), mine waist (GP2), and mine foot (GP3) with different depth were investigated and efficient elution method was proposed in this study. Results showed that the rare earth ore mainly consist of quartz, clay minerals (halloysite, illite, and kaolinite) and rock-forming minerals, and pH and moisture contents of them were ranged from 4.0 to 5.0 and 10-20%, respectively. Residual agent was mainly enriched in the middle and deep layer of the ore body with the main form of ammonium nitrogen (NH4+-N), and content of it at the three sites followed the order of GP1>GP3>GP2, which was related to the content of the clay minerals and the moisture. Occurrence state experimental results illustrated that about 95% of the NH4+-N existed as water-soluble ammonium (WS-AN) and adsorbable ammonium (AS-AN), and 5% of it existed as fixed ammonium (FX-AN), and concentration ratio of them was in order: WS-AN > AS-AN >> FX-AN. Based on the results above, MgCl2 solution was used as an eluent to remove the leaching agent from the ore, and results showed that higher than 90% of residual ammonium could be removed from the ore
引用
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页数:12
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