Washability of Coal from Seams IV and VIII of the Tavantolgoi Deposit

被引:4
作者
Jargalmaa, S. [1 ]
Gerelmaa, T. [1 ]
Baterdene, E. [2 ]
Tsatsral, G. [1 ]
Avid, B. [1 ]
Purevsuren, B. [1 ]
Dugarjav, J. [1 ]
机构
[1] Mongolian Acad Sci, Inst Chem & Chem Technol, Ulaanbaatar 51, Mongolia
[2] Mongolian Univ Sci & Technol, Ulaanbaatar, Mongolia
关键词
Tavantolgoi coal; Float-and-sink tests; Washability curve;
D O I
10.1007/s11053-014-9245-9
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Samples from the Tavantolgoi coal deposit were analyzed by petrographic, elemental, FTIR, XRD, and float-and-sink tests. The deposit is Permian age and characterized by lithotypes that are bright, semi-bright, semi-dull, and dull. Microscopically identified macerals in the deposit are fusinite and vitrinite components and minerals. The inorganic elements in the deposit are Si and Al, indicating an abundance of aluminum silicates, followed by Fe, Cu, and Ca in decreasing order. Ash in the deposit is silica type, in which the point of fusibility is usually higher than the other types. Float-and-sink tests show that the ash in seam IV can be separated easily from coal, whereas the ash in seam VIII has medium degree of difficulty of separation.
引用
收藏
页码:189 / 195
页数:7
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