QUALITY AND UTILIZATION OF THE COAL FROM TAIYUAN FORMATION AND SHANXI FORMATION IN SUHAITU-KUCAOWA AREA, INNER MONGOLIA
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摘要: 苏亥图-苦草洼地区位于鄂尔多斯盆地的西部,古生界煤层的煤质为中灰、中高挥发分、中硫、低磷、低氯煤,煤类以气煤为主,局部以1/3焦煤或弱黏煤为主,可以作为炼焦配煤、动力燃料及民用煤,也可作煤的深加工原料煤等.Abstract: The Suhaitu-Kucaowa area is located in the west of Ordos Basin, where the coal from the Paleozoic formations is characterized by medium ash content, medium-high volatile component, medium sulfur, low phosphorus and low chlorine. The coal is dominated by gas coal, with locally 1/3 coking coal or weakly caking coal, which can be used as coking blend, power fuel and domestic coal, moreover, as raw material for deep processing.
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Key words:
- Ordos Basin /
- Suhaitu-Kucaowa area /
- coking blend /
- Inner Mongolia
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