Abstract

Eudialyte ores from Norra Kärr (Sweden) and Kringlerne (Greenland) are considered a potential source of rare-earth elements (REE) for the development of a sustainable REE industry outside China. Magnetic separation is successfully applicated to recover eudialyte as a magnetic fraction. In the case of the Norra Kärr deposit, up to 20% of the REE and up to 40% of the Zr are lost during mineral processing in the non-magnetic fraction. Zr and REE are associated with non-magnetic minerals such as catapleiite, low- or non-magnetic eudialyte species, and both their intergrowths. Besides zirconosilicates such as catapleiite and eudialyte, the non-magnetic fraction has valuable and already-liberated minerals such as alkali feldspars and nepheline, which should not be considered as tailings. In this investigation, a possible way to recover REE bearing zirconosilicates from the non-magnetic fraction using flotation is presented. First, a low-grade eudialyte concentrate (1.8% Zr, 0.94% REE) from ground ore was obtained using magnetic separation. The non-magnetic fraction was then treated using froth flotation, and a Zr-REE bearing product (9% Zr, 1.5% REE) was obtained as froth product. For this purpose, phosphoric acid esters were used as selective collectors for zirconosilicates at a pH between 3.5 and 4.5. The reagent regime could be proposed not only to recover Zr- and REE-bearing minerals, but also simultaneously to remove Fe, Ti, and other colored impurities from the nepheline-feldspar product and to minimize the tailings volume.

Highlights

  • The development of a modern green and low-carbon industry in developed countries requires a sustainable and fair supply chain of critical raw materials such as cobalt, lithium, vanadium, and rare earth elements (REE) [1,2,3]

  • For this study, the main aim of the magnetic separation was the preparation of feed materials, which contain lost non-recoverable Zr- and REE-bearing minerals

  • It was aimed to recover complex rare zirconium minerals such as non-magnetic eudialyte species and catapleiite using froth flotation. These minerals normally get lost during wet, high-magnetic separation stages into the non-magnetic fraction

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Summary

Introduction

The development of a modern green and low-carbon industry in developed countries requires a sustainable and fair supply chain of critical raw materials such as cobalt, lithium, vanadium, and rare earth elements (REE) [1,2,3]. Norra Kärr is a peralkaline nepheline-syenite intrusive complex located in southcentral Sweden and is defined as comprising agpaitic rocks [6] It is a unique deposit of REE and HFSE elements with a high ratio of HREE relative to total REE (TREE) represented by eudialyte group minerals (EGM). The main aim of this research work is to determine a reagent regime to recover Zr- and REE-bearing minerals from the Norra Kärr ore by flotation, which in this case are currently lost into the non-magnetic fraction. With the use of froth flotation, it would be possible to simultaneously remove undesirable colored impurities and their intergrowths such as iron- and titanium-bearing minerals (titanite, micas (muscovite), pyroxenes, aegirine) from the non-magnetic fraction In this case, the tailings product of the froth flotation must be considered as an additional marketable by-product such as nepheline syenite. The identified gangue minerals are feldspars (albite Na(AlSi3O8), Minerals 2022, 12, 19 microcline K(AlSi3O8), plagioclase (Na,Ca)[(Si,Al)AlSi2]O8, pyroxenes (aegirine-augite series (Na,Ca,Fe2+,Mg)(Fe3+,Al,Fe2+,Mg,)Si2O6) and nepheline Na3K(Al4Si4O16) with its alteration and replacement products (analcime Na(AlSi2O6)·H2O, natrolite Na2Al2Si3O10·2H2O, cancrinite Na6Ca2[(CO3)2|Al6Si6O24]·2H2O)

Sample Characterization
Magnetic Separation Stage
Flotation Experiments
Reagents
Results and Discussion
Selection of Collectors for the Flotation of Zirconosilicate Minerals
Development of an Alternative Beneficiation Flowsheet for Norra Kärr Deposit
Conclusions
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