Calcination pretreatment effects on acid leaching characteristics of rare earth elements from middlings and coarse refuse material associated with a bituminous coal source

•Calcination of coal sources decomposes structure of associated mineral matter.•Calcination as a pre-treatment step prior leaching increases REE recovery.•Recovery of light REEs preferentially increase by 50–65 percentage points.•Exceeding 600 °C causes a reduction in poor volume and REE recovery.•E...

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Veröffentlicht in:Fuel (Guildford) 2019-08, Vol.249 (C), p.130-145
Hauptverfasser: Zhang, Wencai, Honaker, Rick
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Sprache:eng
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Zusammenfassung:•Calcination of coal sources decomposes structure of associated mineral matter.•Calcination as a pre-treatment step prior leaching increases REE recovery.•Recovery of light REEs preferentially increase by 50–65 percentage points.•Exceeding 600 °C causes a reduction in poor volume and REE recovery.•Evidence suggests strong correlation between REEs and phosphorus. The pretreatment of middlings and coarse refuse material collected from a Pocahontas No.3 coal source using calcination was investigated for the potential of improving the leaching recovery of rare earth elements. Calcination at 600 °C significantly and preferentially improved light REE (LREE) recovery to values in the range of 80–90% using 1.2 M HCl. The positive effect was due to the increased pore diameter and volume as well as thermal decomposition of the minerals associated with the LREEs. Heavy REE recovery was not increased after calcination at 600 °C due to the need for higher temperatures to achieve thermal decomposition of HREE minerals. Furthermore, some HREEs were also associated with sulfide minerals (e.g., pyrite) which were transformed into low-solubility oxides (e.g., hematite) after roasting at 600 °C. Based on the leaching characteristics of the major elements (Fe, Al, Ca and Mg) and REEs along with SEM-EDX data, it was concluded that REEs in the two samples mainly occurred as phosphate minerals. In the middlings, some of the minerals were completely encapsulated by kaolinite, which was less apparent in the coarse refuse. In addition, it was found that a portion of the REEs (10–25%) in the samples were associated with the organic matter and micro-dispersed minerals in the organic matrix, was released after calcination and easily recovered using 0.1 M (NH4)2SO4 solution at pH 5. Scandium primarily occurred in mineral forms with minimum amounts associated with ion-adsorbed clays and organic association.
ISSN:0016-2361
1873-7153
DOI:10.1016/j.fuel.2019.03.063