Chemical factors affecting the leaching rate of uranium in CO2 + O2 leaching within autoclave-an example from Nalinggou deposit in the Ordos Basin, North of China

被引:2
|
作者
Chen, Ting [1 ]
Liu, Jinhui [1 ]
Yang, Yihan [2 ]
Zhang, Jianjun [3 ]
Xu, Qi [2 ]
Li, Wenjuan [1 ]
Yu, Rong [1 ]
Yang, Shiqi [1 ]
机构
[1] East China Univ Technol, Sch Water Resources & Environm Engn, 418 Guanglan Rd, Nanchang 330013, Peoples R China
[2] Inner Mongolia Min Co Ltd, CNNC, Hohhot 010010, Peoples R China
[3] East China Univ Technol, Inst Geol Survey, 418 Guanglan Rd, Nanchang 330013, Peoples R China
基金
中国国家自然科学基金;
关键词
Nalinggou deposit; CO2 + O-2 leaching; Chemical characterization; Leaching condition; SANDSTONE; DEPOSIT; NORTH;
D O I
10.1007/s10967-024-09551-1
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
The concentration of uranium in the rock sample was 35.0 mu g/g, the concentration ratio of CO2 and O-2 injected was 1:1, the autoclaves pressure was 0.02 MPa. The uranium leaching rate varied from 28.70 to 37.97%, and when the concentration of HCO3- is lower, the output rate of U is significantly increased as it increases, when its concentration exceeds the threshold value, U's output concentration is no longer infinitely increased. Calcite and dolomite were saturated and precipitated during the leaching process due to the high initial pH; with the injection of CO2, calcite and dolomite remained near- or under-saturated and did not precipitate.
引用
收藏
页码:3767 / 3780
页数:14
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