期刊
INTERNATIONAL JOURNAL OF COAL GEOLOGY
卷 201, 期 -, 页码 109-126出版社
ELSEVIER
DOI: 10.1016/j.coal.2018.11.019
关键词
Coal; Rare earth elements; Lanthanides; Scandium; Bottom ash; Lignite; Landfill; Ceplea Valley
资金
- UEFISCDI, Romania [28/2015]
- Fundacao para a Ciencia e a Tecnologia, IP (FCT, Portugal) [ERA-MIN/0006/2014]
- FCT [SFRH/BPD/76230/2011]
- National Natural Science Foundation of China [41420104001]
- Project 111 [B17042]
- Fundação para a Ciência e a Tecnologia [SFRH/BPD/76230/2011, ERA-MIN/0006/2014] Funding Source: FCT
This study aims to demonstrate, by a detailed fundamental analysis, an alternative for the production of rare earth elements, including yttrium and scandium (REY + Sc), from the historic bottom ash deposit at Ceplea Valley (Romania). Twenty-five samples representing 20% of this deposit were studied using a combination of chemical (proximate and elemental analysis), mineralogical and petrographic techniques. This analysis also included, for the first time, a scanning electron microscopy with X-ray microanalysis SEM/EDS point-count method for tracking REE-bearing minerals. The results showed that the bulk REY + Sc concentration is consistent throughout the landfill, and a bottom ash composite sample was made to assess the chemical composition of several size fractions. Based on Seredin-Dai's criteria (Seredin and Dai, 2012), the plot of the outlook coefficient of REY ores (C-outl) versus the percentage of critical REY of the deposit samples (278 ppm in average) and of the composite sample size fractions shows that this ash is a potentially promising source of REY. However, Gd seems to be the most promising element, especially in the 0.090-0.125 mm and < 0.063 mm size fractions. Finally, the SEM/EDS results show that the only REE-bearing minerals (except one case with Y, Gd, Er, Dy) are micrometre-sized phosphate grains with Ce, La and Nd, with an average diameter of 4.85 mu m, which do not entirely account for the total REE determined by ICP-MS and indicates that a fraction of these elements must be dispersed in the glassy aluminosilicate matrix.
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