Influence of coal particle size on particulate matter emission and its chemical species produced during coal combustion

被引:100
作者
Ninomiya, Y
Zhang, LA
Sato, A
Dong, ZB
机构
[1] Chubu Univ, Coll Engn, Dept Appl Chem, Kasugai, Aichi 1200, Japan
[2] Chinese Acad Sci, Inst Coal Chem, Taiyuan, Shanxi, Peoples R China
关键词
coal combustion; particulate matter; coal particle size; mineral transferring; chemical species;
D O I
10.1016/j.fuproc.2003.10.012
中图分类号
O69 [应用化学];
学科分类号
081704 ;
摘要
Pulverized coals were burnt in a laboratory-scale drop tube furnace to study emission of particulate matter (PM) in this process. Reaction temperature of 1200 degreesC, residence time of 2.4 s and an atmosphere, 20% 02 and N-2 being balance, were used as the combustion condition. Three coals were divided into three sizes, 125-250, 63-125 and <63 mu m, and subjected to combustion under above-mentioned conditions. PM was size-segregated by low-pressure-impactor (LPI) into different sizes ranging from 10.0 to 0.03 mu m. Besides its properties including concentration, particle size distribution and elemental composition, PM having three sizes was also subjected to CCSEM analysis to quantify the chemical species within them. The results indicate that, coal particle size affects PM emission significantly in the combustion. Decreasing coal particle size leads to formation of much PM. For coals of 125-250 gm, a single mode distribution of PM was formed, which has the central mode at approximately 4.0 mu m with an edge of 10.0 mu m. For coals of 63-125 mu m, the resultant PM had the similar distribution to that for coals of 125-250 mu m. In contrast, with coal particle size down to < 63 mum, a bimodal mode distribution of PM was formed. The large mode at 4.0 mum, mainly of aluminosilicate, was formed by the direct transferring of inherent excluded minerals into PM. Decreasing coal leads to prevalence of excluded fine mineral particles within it, and accordingly, more the fine mineral directly transferred into PM. Another mode was formed at about 0.5 mum, which was caused by both fragmentation of inherent minerals and vaporization of heavy metals within coal. Aluminosilicate salts are relatively abundant in this size, and their surface was coated with condensed heavy metallic vapors. In addition, the amount of PM having the size around 0.13 mum was also found relatively great in the case of combustion of coal < 63 mu m, it was mainly composed of vaporized alkali, heavy metals and their sulfate, chloride and phosphates. (c) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:1065 / 1088
页数:24
相关论文
共 30 条
[1]  
Baron P.A., 2001, AEROSOL MEASUREMENT, V2nd
[2]   Measurements of lead vapor and particulate in flames and post-flame gases [J].
Buckley, SG ;
Sawyer, RF ;
Koshland, CP ;
Lucas, D .
COMBUSTION AND FLAME, 2002, 128 (04) :435-446
[3]   Review of PM2.5 and PM10 apportionment for fossil fuel combustion and other sources by the chemical mass balance receptor model [J].
Chow, JC ;
Watson, JG .
ENERGY & FUELS, 2002, 16 (02) :222-260
[4]  
Clarke L.B., 1992, TRACE ELEMENTS EMISS, P111
[5]  
HEIN KRG, 2002, P TRAC EL WORKSH YOK, P141
[6]  
Hinds W. C., 1999, Aerosol Technology: Properties, Behavior, and Measurement of Airborne Particles, DOI [10.1016/0021-8502(83)90049-6, DOI 10.1016/0021-8502(83)90049-6]
[7]  
HINDS WC, 1999, AEROSOL TECHNOLOGY P, P260
[8]  
HIRABAYASHI M, 2001, ANAL SCI, V17, P1581
[9]  
*JIS, 1998, JIS HDB ENV MEAS, P581
[10]  
LEVIN EM, 1964, PHASE DIAGRAMS CERAM, P122