Geochemistry of Carboniferous–Permian Coal from the Wujiawan Mine, Datong Coalfield, Northern China: Modes of Occurrence, Origin of Valuable Trace Elements, and Potential Industrial Utilization

This paper provides new geochemical data focusing on valuable elements in the coal, parting, and floor samples in the No. 5 coal seam of the Taiyuan Formation from the Wujiawan mine, Datong coalfield, northern China. The minerals mainly consist of kaolinite, calcite, and pyrite, as well as trace amo...

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Main Authors: Jialiang Ma, Lin Xiao, Ke Zhang, Yukun Jiao, Zhenzhen Wang, Jinxiao Li, Wenmu Guo, Pengpeng Gao, Shenjun Qin, Cunliang Zhao
Format: Article
Language:English
Published: MDPI AG 2020-08-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/10/9/776
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spelling doaj-10f721da0eed40a1a060c063a828d49a2020-11-25T03:37:18ZengMDPI AGMinerals2075-163X2020-08-011077677610.3390/min10090776Geochemistry of Carboniferous–Permian Coal from the Wujiawan Mine, Datong Coalfield, Northern China: Modes of Occurrence, Origin of Valuable Trace Elements, and Potential Industrial UtilizationJialiang Ma0Lin Xiao1Ke Zhang2Yukun Jiao3Zhenzhen Wang4Jinxiao Li5Wenmu Guo6Pengpeng Gao7Shenjun Qin8Cunliang Zhao9School of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaSchool of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaSchool of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaHebei Provincal Coalfield Geology Bureau Geophysical Prospecting & Survey Administration, Xingtai 054000, ChinaSchool of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaSchool of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaSchool of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaSchool of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaSchool of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaSchool of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, ChinaThis paper provides new geochemical data focusing on valuable elements in the coal, parting, and floor samples in the No. 5 coal seam of the Taiyuan Formation from the Wujiawan mine, Datong coalfield, northern China. The minerals mainly consist of kaolinite, calcite, and pyrite, as well as trace amounts of quartz and illite. The No. 5 coal is enriched in Li, Ga, high field strength elements (HFSEs), and rare earth elements and yttrium (REY) when compared with world hard coals. Of particular interest is the high average concentration of Li (67.66 μg/g), which is around seven times higher than the value for world hard coals. Lithium, Ga, and HFSEs have strong inorganic affinities, whereas REY have organic affinities. The main carrier of Li, Ga, and HFSEs is aluminosilicate minerals, while REY appear to occur with organophosphorus. These HFSEs are enriched, both in the parting and in the adjacent coal samples. This suggests that these elements are likely to leach out during the diagenetic process. The distribution patterns of REY, along with the ratio of Al<sub>2</sub>O<sub>3</sub>/TiO<sub>2</sub> and the figure of Zr/TiO<sub>2</sub> vs. Nb/Y are suggestive of their derivation from felsic parent material. In the northern and eastern part of the Datong coalfield, there are several regions where the Li content is higher than the mineable grade, in particular in the northern Datong coalfield where there is a mine with an Li content of 294.6 μg/g. This is significantly higher than the mineable grade. Therefore, there is a potential for financially viable recovery of Li in these coals of the Datong coalfield.https://www.mdpi.com/2075-163X/10/9/776Datong coalfieldmineralstrace elementsfelsic detritallithium
collection DOAJ
language English
format Article
sources DOAJ
author Jialiang Ma
Lin Xiao
Ke Zhang
Yukun Jiao
Zhenzhen Wang
Jinxiao Li
Wenmu Guo
Pengpeng Gao
Shenjun Qin
Cunliang Zhao
spellingShingle Jialiang Ma
Lin Xiao
Ke Zhang
Yukun Jiao
Zhenzhen Wang
Jinxiao Li
Wenmu Guo
Pengpeng Gao
Shenjun Qin
Cunliang Zhao
Geochemistry of Carboniferous–Permian Coal from the Wujiawan Mine, Datong Coalfield, Northern China: Modes of Occurrence, Origin of Valuable Trace Elements, and Potential Industrial Utilization
Minerals
Datong coalfield
minerals
trace elements
felsic detrital
lithium
author_facet Jialiang Ma
Lin Xiao
Ke Zhang
Yukun Jiao
Zhenzhen Wang
Jinxiao Li
Wenmu Guo
Pengpeng Gao
Shenjun Qin
Cunliang Zhao
author_sort Jialiang Ma
title Geochemistry of Carboniferous–Permian Coal from the Wujiawan Mine, Datong Coalfield, Northern China: Modes of Occurrence, Origin of Valuable Trace Elements, and Potential Industrial Utilization
title_short Geochemistry of Carboniferous–Permian Coal from the Wujiawan Mine, Datong Coalfield, Northern China: Modes of Occurrence, Origin of Valuable Trace Elements, and Potential Industrial Utilization
title_full Geochemistry of Carboniferous–Permian Coal from the Wujiawan Mine, Datong Coalfield, Northern China: Modes of Occurrence, Origin of Valuable Trace Elements, and Potential Industrial Utilization
title_fullStr Geochemistry of Carboniferous–Permian Coal from the Wujiawan Mine, Datong Coalfield, Northern China: Modes of Occurrence, Origin of Valuable Trace Elements, and Potential Industrial Utilization
title_full_unstemmed Geochemistry of Carboniferous–Permian Coal from the Wujiawan Mine, Datong Coalfield, Northern China: Modes of Occurrence, Origin of Valuable Trace Elements, and Potential Industrial Utilization
title_sort geochemistry of carboniferous–permian coal from the wujiawan mine, datong coalfield, northern china: modes of occurrence, origin of valuable trace elements, and potential industrial utilization
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2020-08-01
description This paper provides new geochemical data focusing on valuable elements in the coal, parting, and floor samples in the No. 5 coal seam of the Taiyuan Formation from the Wujiawan mine, Datong coalfield, northern China. The minerals mainly consist of kaolinite, calcite, and pyrite, as well as trace amounts of quartz and illite. The No. 5 coal is enriched in Li, Ga, high field strength elements (HFSEs), and rare earth elements and yttrium (REY) when compared with world hard coals. Of particular interest is the high average concentration of Li (67.66 μg/g), which is around seven times higher than the value for world hard coals. Lithium, Ga, and HFSEs have strong inorganic affinities, whereas REY have organic affinities. The main carrier of Li, Ga, and HFSEs is aluminosilicate minerals, while REY appear to occur with organophosphorus. These HFSEs are enriched, both in the parting and in the adjacent coal samples. This suggests that these elements are likely to leach out during the diagenetic process. The distribution patterns of REY, along with the ratio of Al<sub>2</sub>O<sub>3</sub>/TiO<sub>2</sub> and the figure of Zr/TiO<sub>2</sub> vs. Nb/Y are suggestive of their derivation from felsic parent material. In the northern and eastern part of the Datong coalfield, there are several regions where the Li content is higher than the mineable grade, in particular in the northern Datong coalfield where there is a mine with an Li content of 294.6 μg/g. This is significantly higher than the mineable grade. Therefore, there is a potential for financially viable recovery of Li in these coals of the Datong coalfield.
topic Datong coalfield
minerals
trace elements
felsic detrital
lithium
url https://www.mdpi.com/2075-163X/10/9/776
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