Matches in SemOpenAlex for { <https://semopenalex.org/work/W3082391255> ?p ?o ?g. }
- W3082391255 endingPage "776" @default.
- W3082391255 startingPage "776" @default.
- W3082391255 abstract "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 Al2O3/TiO2 and the figure of Zr/TiO2 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." @default.
- W3082391255 created "2020-09-08" @default.
- W3082391255 creator A5030064573 @default.
- W3082391255 creator A5043065834 @default.
- W3082391255 creator A5045732898 @default.
- W3082391255 creator A5048377825 @default.
- W3082391255 creator A5053595484 @default.
- W3082391255 creator A5068285872 @default.
- W3082391255 creator A5075444205 @default.
- W3082391255 creator A5089110196 @default.
- W3082391255 creator A5090660514 @default.
- W3082391255 creator A5090678271 @default.
- W3082391255 date "2020-08-31" @default.
- W3082391255 modified "2023-10-16" @default.
- W3082391255 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" @default.
- W3082391255 cites W1773725738 @default.
- W3082391255 cites W1775883310 @default.
- W3082391255 cites W1963574048 @default.
- W3082391255 cites W1964592821 @default.
- W3082391255 cites W1968168577 @default.
- W3082391255 cites W1970182451 @default.
- W3082391255 cites W1977471363 @default.
- W3082391255 cites W1977552998 @default.
- W3082391255 cites W1979619129 @default.
- W3082391255 cites W1979836306 @default.
- W3082391255 cites W1983297630 @default.
- W3082391255 cites W1988627424 @default.
- W3082391255 cites W1991352764 @default.
- W3082391255 cites W1992065927 @default.
- W3082391255 cites W1992292460 @default.
- W3082391255 cites W1993057794 @default.
- W3082391255 cites W1994445773 @default.
- W3082391255 cites W1996807275 @default.
- W3082391255 cites W1999448338 @default.
- W3082391255 cites W2001171914 @default.
- W3082391255 cites W2007975985 @default.
- W3082391255 cites W2010348370 @default.
- W3082391255 cites W2011688818 @default.
- W3082391255 cites W2012422083 @default.
- W3082391255 cites W2019737722 @default.
- W3082391255 cites W2023146552 @default.
- W3082391255 cites W2023759362 @default.
- W3082391255 cites W2024249259 @default.
- W3082391255 cites W2035680956 @default.
- W3082391255 cites W2038066842 @default.
- W3082391255 cites W2038363821 @default.
- W3082391255 cites W2043621358 @default.
- W3082391255 cites W2044034399 @default.
- W3082391255 cites W2057063592 @default.
- W3082391255 cites W2059614644 @default.
- W3082391255 cites W2060133470 @default.
- W3082391255 cites W2063608352 @default.
- W3082391255 cites W2064493626 @default.
- W3082391255 cites W2068636664 @default.
- W3082391255 cites W2068766004 @default.
- W3082391255 cites W2070597174 @default.
- W3082391255 cites W2073369201 @default.
- W3082391255 cites W2084456237 @default.
- W3082391255 cites W2093350953 @default.
- W3082391255 cites W2093750105 @default.
- W3082391255 cites W2111119089 @default.
- W3082391255 cites W2118835828 @default.
- W3082391255 cites W2128448183 @default.
- W3082391255 cites W2165712457 @default.
- W3082391255 cites W2170538923 @default.
- W3082391255 cites W2181469240 @default.
- W3082391255 cites W2219663543 @default.
- W3082391255 cites W2268826899 @default.
- W3082391255 cites W2323971120 @default.
- W3082391255 cites W2332354175 @default.
- W3082391255 cites W2342348073 @default.
- W3082391255 cites W2388158256 @default.
- W3082391255 cites W2468230850 @default.
- W3082391255 cites W2468944540 @default.
- W3082391255 cites W2496781418 @default.
- W3082391255 cites W2527777557 @default.
- W3082391255 cites W2547053780 @default.
- W3082391255 cites W2566091732 @default.
- W3082391255 cites W2594917321 @default.
- W3082391255 cites W2605875252 @default.
- W3082391255 cites W2709073124 @default.
- W3082391255 cites W2789585216 @default.
- W3082391255 cites W2794319356 @default.
- W3082391255 cites W2875364626 @default.
- W3082391255 cites W2887518479 @default.
- W3082391255 cites W2895697769 @default.
- W3082391255 cites W2898624148 @default.
- W3082391255 cites W2922198985 @default.
- W3082391255 cites W2947883078 @default.
- W3082391255 cites W2959157846 @default.
- W3082391255 cites W2985465445 @default.
- W3082391255 cites W3005104221 @default.
- W3082391255 cites W3018775932 @default.
- W3082391255 cites W3041497954 @default.
- W3082391255 cites W3048922791 @default.
- W3082391255 cites W4242247618 @default.
- W3082391255 cites W4376849557 @default.
- W3082391255 doi "https://doi.org/10.3390/min10090776" @default.