Thermal decomposition behavior of Mountain Pass rare earth concentrate in air/CO2 atmosphere

被引:0
作者
Sun, Xu [1 ,2 ]
Li, Zheng [1 ]
Meng, Deliang [1 ]
Huang, Xiaowei [1 ,2 ,3 ]
Feng, Zongyu [1 ,2 ]
Wang, Meng [1 ,2 ,3 ]
Zhao, Yan [1 ]
机构
[1] Grirem Adv Mat Co Ltd, Natl Engn Res Ctr Rare Earth, Beijing 100088, Peoples R China
[2] Gen Res Inst Nonferrous Met, Beijing 100088, Peoples R China
[3] GRIMAT Engn Inst Co Ltd, Beijing 101407, Peoples R China
基金
中国国家自然科学基金;
关键词
Mountain Pass rare earth mine; Roasting; Thermal decomposition; Rare earths; BASTNAESITE; NACL-CACL2; OXIDATION; KINETICS; CAO;
D O I
10.1016/j.jre.2024.04.002
中图分类号
O69 [应用化学];
学科分类号
081704 ;
摘要
The Mountain Pass mine is recognized as one of the world's primary sources of rare earth minerals. These rare earth minerals mainly consist of bastnaesite and a small amount of monazite phosphate, which cannot be decomposed and recovered through conventional oxidative roasting and hydrochloric acid leaching process. An efficient, clean, and economical process called the "combined method" was proposed for the utilization of the Mountain Pass mine to extract rare earths from Mountain Pass rare earth concentrate (MPREC). The main steps of this process include weak oxidation atmosphere roasting, step leaching of hydrochloric acid, solid-liquid separation, the monazite slag with sulfuric acid roasting water leaching, etc. In this paper, the roasting process of MPREC under a weak oxidation atmosphere was investigated. The study examines the thermal decomposition kinetics, phase transition process, and leaching behavior of MPREC in air/CO2 atmosphere. Results show that, the activation energy (Ea) for MPREC thermal decomposition in air and CO2 atmosphere are 146 and 320 kJ/mol, respectively. At temperature above 500 degrees C in air or above 700 degrees C in CO2 atmosphere, REOF are generated from bastnaesite through an in-situ reaction with CaO, which is decomposed from CaCO3, to form CaF2 and rare earth oxide (REO). Thus, F is regulated into solid phase. In an oxidizing atmosphere, the thermal decomposition of bastnaesite is accompanied by the rapid oxidation of Ce(III). In contrast, the oxidation of Ce(III) in a CO2 atmosphere is significantly inhibited. At 700 degrees C, the oxidation rate of Ce in air is 74.09%, while in a CO2 atmosphere, it is only 33.83%. The hydrochloric acid leaching experiment shows that, the leaching rate of rare earth after roasting at 600 degrees C under an air atmosphere reaches to 82.9%, and it reaches 87% after roasting at 800 degrees C under a CO2 atmosphere. The reduction of Ce oxidation in a weak oxidizing atmosphere significantly improves the leaching rate of Ce. (c) 2025 Published by Elsevier B.V. on behalf of Chinese Society of Rare Earths.
引用
收藏
页码:843 / 850
页数:8
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