Process mineralogy of Weishan rare earth ore by MLA

Mineral liberation analyser (MLA) was applied to quantitatively analyze the rare earth ore from Weishan in Shandong. Mineralogy parameters, such as mineral composition, occurrence states of rare earth elements (REEs) and valuable elements, mineral embedded grain size distribution, mineral associatio...

Full description

Saved in:
Bibliographic Details
Published inJournal of rare earths Vol. 37; no. 3; pp. 334 - 338
Main Authors Xu, Caili, Zhong, Chengbin, Lyu, Renliang, Ruan, Yaoyang, Zhang, Zhenyue, Chi, Ru′an
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.03.2019
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Mineral liberation analyser (MLA) was applied to quantitatively analyze the rare earth ore from Weishan in Shandong. Mineralogy parameters, such as mineral composition, occurrence states of rare earth elements (REEs) and valuable elements, mineral embedded grain size distribution, mineral association and liberation, are obtained. Results show that the contents of REEs and other valuable elements mainly contained in the ore were La 1.02 wt%, Ce 4.29 wt%, Pr 0.34 wt%, Nd 0.84 wt%, Sr 3.4 wt% and Ba 26.53 wt%, respectively. The REEs mainly occur in bastnaesite and carbocernaite in the form of independent mineral and the contents of bastnaesite and carbocernaite in the ore were 5.96 wt% and 12.30 wt%, respectively. 67.34% of strontium occurs in carbocernaite and the rest occurs in celestobarite and strontianite mineral. 92.71% of barium occurs in barite. Liberation of main rare-earth minerals such as bastnaesite and carbocernaite is more than 80% when the grinding fineness is 78.42% passing 74 μm. The research results could be employed to provide detailed basic theoretical data for further improvement of the beneficiation process flow and the processing index of rare earth ore, the recycling of other valuable minerals and the comprehensive utilization of tailings. Liberation of bastnaesite and carbocernaite by free surface. [Display omitted]
ISSN:1002-0721
2509-4963
DOI:10.1016/j.jre.2018.06.008