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© 2022 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.

Abstract

The characterization and leaching mechanism of REEs from phosphogypsum (PG) in HCl was studied in-depth. REEs contained in the PG were 208 ppm, of which Y, La, Ce, and Nd were the four most abundant elements. The modes of occurrence of rare earth elements (REEs) in the PG were quantified using the sequential chemical extraction (SCE) method. Among the five REE occurrence species, the metal oxide form accounted for the largest proportion, followed by the residual, organic matter, and ion-exchangeable fractions, and REEs bound to carbonates were the least. From the comparison of the distributions of REEs and calcium in different occurrence states, it can be determined that REEs contained in the PG were mainly present in the residue state (existed in the gypsum lattice) and the metal oxide state (easily leached). The leaching results show that the suitable leaching conditions were acid concentration of 1.65 mol/L, S/L ratio of 1/10, and reaction temperature of 60 °C. At the condition, the maximum leaching efficiency for ∑REE was 65.6%, of which the yttrium leaching rate was the highest and reached 73.8%. Importantly, A new kinetic equation based on the cylindrical shrinking core model (SCM) was deduced and could well describe REE leaching process from PG. The apparent activation energy for ∑REE leaching was determined to be 20.65 kJ·mol−1.

Details

Title
Characterization and Leaching Kinetics of Rare Earth Elements from Phosphogypsum in Hydrochloric Acid
Author
Guan, Qingjun 1 ; Sui, Ying 2 ; Liu, Chufeng 2 ; Wang, Yongjie 2 ; Zeng, Chuxiong 2 ; Yu, Weijian 1 ; Gao, Zhiyong 3   VIAFID ORCID Logo  ; Zang, Zhenyue 4 ; Ru-an, Chi 5 

 Hunan Province Key Laboratory of Coal Resources Clean-Utilization and Mine Environment Protection, Hunan University of Science and Technology, Xiangtan 411199, China; [email protected]; School of Resource Environment and Safety Engineering, Hunan University of Science and Technology, Xiangtan 411199, China; [email protected] (Y.S.); [email protected] (C.L.); [email protected] (Y.W.); [email protected] (C.Z.) 
 School of Resource Environment and Safety Engineering, Hunan University of Science and Technology, Xiangtan 411199, China; [email protected] (Y.S.); [email protected] (C.L.); [email protected] (Y.W.); [email protected] (C.Z.) 
 School of Minerals Processing and Bioengineering, Central South University, Changsha 410017, China; [email protected] 
 School of XingFa Mining Engineering, Wuhan Institute of Technology, Wuhan 430079, China; [email protected] 
 School of XingFa Mining Engineering, Wuhan Institute of Technology, Wuhan 430079, China; [email protected]; Hubei Three Gorges Laboratory, Yichang 443007, China 
First page
703
Publication year
2022
Publication date
2022
Publisher
MDPI AG
e-ISSN
2075163X
Source type
Scholarly Journal
Language of publication
English
ProQuest document ID
2679823520
Copyright
© 2022 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.