Significant contribution of organically-bound Mg, Ca, and Fe to inorganic PM10 emission during the combustion of pulverized Victorian brown coal

被引:64
作者
Gao, Xiangpeng [1 ]
Rahim, Muhammad Usman [1 ]
Chen, Xixia [1 ]
Wu, Hongwei [1 ]
机构
[1] Curtin Univ, Sch Chem & Petr Engn, Perth, WA 6845, Australia
基金
澳大利亚研究理事会;
关键词
Victorian brown coal; Combustion; PM10; Organically-bound inorganic species; LOW-RANK COALS; DROP-TUBE FURNACE; ASH FORMATION; MINERAL MATTER; SIZE DISTRIBUTIONS; PARTICLE FORMATION; INHERENT MINERALS; ELEMENTS; BEHAVIOR; GASIFICATION;
D O I
10.1016/j.fuel.2013.09.056
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
This study deployed water-washing and dilute acid washing of a Victorian brown coal to prepare a set of coal samples with simplified occurrence forms of inorganic species. The resulted water-washed coal contains dominantly organically-bound species (primarily Mg, Ca, and Fe) and discrete mineral particles whereas the acid-washed coal only consists of discrete mineral particles. The coal samples (i.e., the raw, the water-washed and the acid-washed coals) were combusted in a lab-scale drop-tube furnace in air at 1400 degrees C to produce inorganic particulate matter (PM) with aerodynamic diameter less than 10 mu m (PM10). Benchmarking on yields, particle size distribution, and chemical properties of PM10 produced from the combustion of the three coals clearly demonstrates that majority of PM10, including PM with aerodynamic diameter less than 1 mu m (PM1) and between 1 and 10 mu m (PM1-10), is contributed by organically-bound elements (mainly Mg, Ca, and Fe) whereas there is only limited contribution from discrete mineral particles due to their low contents in the brown coal. The results also clearly show that the water-soluble salts (e. g., NaCl) mainly contribute to the emission of PM with aerodynamic diameter less than 0.1 mu m (PM0.1). (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:825 / 832
页数:8
相关论文
共 65 条
[1]  
[Anonymous], 2011, ANN BOOK ASTM STAND, V82, P1, DOI [DOI 10.1520/E0870-82R06.2, DOI 10.1520/E0870-82R06]
[2]   A new method for determining the conversion of low-ash coals using synthetic ash as a tracer [J].
Ballantyne, TR ;
Ashman, PJ ;
Mullinger, PJ .
FUEL, 2005, 84 (14-15) :1980-1985
[3]   Release of inorganic material during coal devolatilization [J].
Baxter, LL ;
Mitchell, RE ;
Fletcher, TH .
COMBUSTION AND FLAME, 1997, 108 (04) :494-502
[4]   THE RELEASE OF IRON DURING THE COMBUSTION OF ILLINOIS NO-6 COAL [J].
BAXTER, LL ;
MITCHELL, RE .
COMBUSTION AND FLAME, 1992, 88 (01) :1-14
[5]   COMPARISON OF INORGANIC CONSTITUENTS IN 3 LOW-RANK COALS [J].
BENSON, SA ;
HOLM, PL .
INDUSTRIAL & ENGINEERING CHEMISTRY PRODUCT RESEARCH AND DEVELOPMENT, 1985, 24 (01) :145-149
[6]  
BREE 2012, 2012, AUSTR EN STAT
[7]  
Brockway D, 1991, SCI VICTORIAN BROWN
[8]   COAL ASH COMPOSITION OF AUSTRALIAN LOW RANK COALS [J].
BROWN, LJ ;
CASHION, JD ;
LEDGER, RC .
HYPERFINE INTERACTIONS, 1992, 71 (1-4) :1411-1414
[9]   Fireside slagging, fouling, and high-temperature corrosion of heat-transfer surface due to impurities in steam-raising fuels [J].
Bryers, RW .
PROGRESS IN ENERGY AND COMBUSTION SCIENCE, 1996, 22 (01) :29-120
[10]   Submicron ash formation from coal combustion [J].
Buhre, BJP ;
Hinkley, JT ;
Gupta, RP ;
Wall, TF ;
Nelson, PF .
FUEL, 2005, 84 (10) :1206-1214