Emission of inorganic PM10 from included mineral matter during the combustion of pulverized coals of various ranks

被引:57
|
作者
Wen, Chang [1 ,2 ]
Gao, Xiangpeng [1 ]
Yu, Yun [1 ]
Wu, Jianqun [2 ]
Xu, Minghou [2 ]
Wu, Hongwei [1 ]
机构
[1] Curtin Univ, Sch Chem & Petr Engn, Perth, WA 6845, Australia
[2] Huazhong Univ Sci & Technol, State Key Lab Coal Combust, Wuhan 430074, Hunan, Peoples R China
关键词
Coal; Combustion; PM1; PM10; Coal rank; PARTICULATE MATTER; ASH FORMATION; PARTICLE-SIZE; BEHAVIOR; FRAGMENTATION; TEMPERATURE; CCSEM; TRANSFORMATIONS; COALESCENCE; CAPTURE;
D O I
10.1016/j.fuel.2014.09.114
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Three density-separated (1.4-1.6 g/cm(3)) and size-fractioned (63-90 mu m) Chinese coals (HLH lignite, PDS bituminous coal and CZ anthracite), containing dominantly included mineral matter, were prepared and then combusted in a drop-tube furnace in air at 1400 degrees C. Under the experimental conditions, the yields of particulate matter (PM) with aerodynamic diameters of <1 mu m (PM1), 1-10 mu m (PM1-10) and <10 mu m (PM10) as well as some key PM10-forming elements (e. g., Si, Fe and Mg) follow a rank sequence of the HLH lignite > the PDS bituminous coal > the CZ anthracite. Such a rank dependence is attributed to the discrepancies in the properties of included mineral matter in these coals and the coal combustion characteristics. The partition of Fe in the PM1 from the HLH lignite appears to result from the fragmentation and disintegration of included siderite during coal combustion. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:526 / 530
页数:5
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