Magnetic Separation Method for Isolating Rare-Earth Elements and Zirconium from Molten Salts

2020 ◽  
Vol 56 (6) ◽  
pp. 583-590
Author(s):  
L. S. Alekseeva ◽  
D. O. Savinykh ◽  
A. I. Orlova ◽  
M. Yu. Kalenova ◽  
A. M. Koshcheev ◽  
...  
2017 ◽  
Vol 58 (3) ◽  
pp. 400-405 ◽  
Author(s):  
Aida Abbasalizadeh ◽  
Annelies Malfliet ◽  
Seshadri Seetharaman ◽  
Jilt Sietsma ◽  
Yongxiang Yang

2019 ◽  
Vol 136 ◽  
pp. 50-61 ◽  
Author(s):  
George Blankson Abaka-Wood ◽  
Massimiliano Zanin ◽  
Jonas Addai-Mensah ◽  
William Skinner

Author(s):  
L. M. Arrigo ◽  
J. Jiang ◽  
Z. S. Finch ◽  
J. M. Bowen ◽  
C. L. Beck ◽  
...  

2019 ◽  
Vol 3 (35) ◽  
pp. 493-502 ◽  
Author(s):  
Vladimir A. Volkovich ◽  
Boris D. D. Vasin ◽  
Trevor R. R. Griffiths ◽  
Ilya B. Polovov ◽  
Evgenii O. O. Medvedev ◽  
...  

2012 ◽  
Vol 454 ◽  
pp. 268-272 ◽  
Author(s):  
Peng Gao ◽  
Yue Xin Han ◽  
Yong Sheng Sun ◽  
Chao Chen

Occurrence state of rare earth elements in the different deoxidization stages and the behavior of rare earth elements in the process of depth reduction were studied by analyzing XRD and SEM images of Bayan Obo oxide ore in different deoxidization time. The results showed that deoxidization time had a great effect on the occurrence state of rare earth elements. With the increase of deoxidization time, rare earth minerals gradually translated from bastnaesite and urdite into (CaO•2Ce2O3•3SiO2).This phase was white with a small size. It was columnar or massive in most cases and could be easily separated from the iron phase. 97.18% of the rare earth elements, which could be recovered by flotation, gravity separation and magnetic separation, entered the iron tailings.


2018 ◽  
Vol 316 (2) ◽  
pp. 443-450 ◽  
Author(s):  
E. H. Borai ◽  
I. M. Ahmed ◽  
A. M. Shahr El-Din ◽  
M. S. Abd El-Ghany

Minerals ◽  
2021 ◽  
Vol 11 (9) ◽  
pp. 950
Author(s):  
Mero-Lee Ursula Cornelius ◽  
Alechine Emmanuel Ameh ◽  
Chuks Paul Eze ◽  
Olanrewaju Fatoba ◽  
Asel Sartbaeva ◽  
...  

Rare earth elements (REEs) are essential raw materials in a variety of industries including clean energy technologies such as electric vehicles and wind turbines. This places an ever-increasing demand on global rare earth element production. Coal fly ash (CFA) possesses appreciable levels of REEs. CFA, a waste by-product of coal combustion, is therefore a readily available source of REEs that does not require mining. CFA valorisation to zeolites has been achieved via various synthesis pathways. This study aimed to evaluate one such pathway by monitoring how REEs partition during CFA processing by the wet, magnetic separation process and zeolitisation. South African CFA was subjected to wet, magnetic separation and subsequent zeolitisation of the nonmagnetic fraction (NMF); solid products were characterised by XRD, SEM, XRF and LA-ICP-MS. The wet, magnetic separation process resulted in the partitioning of a specific set of transition metals (such as Fe, Mn, Cr, V, Ni, Zn, Cu, Co and Mo) into the magnetic fraction (MF) of CFA, while REEs partitioned into the NMF with a total REE content of 530.2 ppm; thus, the matrix elements of CFA were extracted with ease. Zeolitisation resulted in a solid zeolite product (hydroxysodalite) with a total REE content of 537.6 ppm. The process of zeolitisation also resulted in the selective enrichment of Ce (259.1 ppm) into the solid zeolite product (hydroxysodalite), while other REEs were largely partitioned into the liquid phase. CFA valorisation by wet, magnetic separation and zeolitisation therefore allowed for the partitioning of REEs into various extraction products while recovering the matrix elements of CFA such as Fe, Si and Al. The findings of this study highlight the geopolitical importance of REEs in terms of the development of alternative processes for REE recovery from waste and alternative sources, which may potentially give countries that employ and develop the technology a key advantage in the production of REEs for the global market.


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