ENVIRONMENTAL-IMPACT OF MINERAL TRANSFORMATIONS UNDERGONE DURING COAL COMBUSTION

被引:36
作者
CHINCHON, JS
QUEROL, X
FERNANDEZTURIEL, JL
LOPEZSOLER, A
机构
[1] Instituto de Geología 'Jaime Almera' (CSIC), U.E.I. Geología Ambiental, Barcelona, 08028, C/ Martí i Franqués s/n
来源
ENVIRONMENTAL GEOLOGY AND WATER SCIENCES | 1991年 / 18卷 / 01期
关键词
Emission Reduction - High Temperature Combustion - Mineral Transformations - Sulfur Coal Ash;
D O I
10.1007/BF01704573
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The mineral transformations undergone by high sulfur coal ash were studied. An X-ray diffraction (XRD) experiment was carried out to reproduce experimentally the mineral transformations produced during coal combustion in coal-fired power stations. We have verified that the anhydrite is the main crystalline phase that contains sulfur in the solid combustion waste from 500-degrees-C until its decomposition at 1060 +/- 10-degrees-C. Thus, this calcium sulfate is the main crystalline phase involved in the sulfur retention in the combustion wastes at high temperatures. Therefore, a considerable proportion of the sulfur would not be emitted into the atmosphere at temperatures lower than 1060-degrees-C. Taking as a reference the annual coal consumption of the Teruel Mining District (6 million tons), the mean sulfur content and the anhydrite content at 900-degrees-C, it was shown that the SO2 emissions could be reduced by approximately 13 percent (83,000 ton/yr) provided that the combustion temperature was 900-degrees-C.
引用
收藏
页码:11 / 15
页数:5
相关论文
共 3 条
[1]   QUANTIFICATION OF FLY-ASH IN CEMENTS AND MORTARS BY MEANS OF GAMMA-SPECTROMETRY [J].
CHINCHON, JS ;
LOPEZSOLER, A ;
REYES, AS ;
GINJAUME, M ;
VAZQUEZ, E ;
YAGUE, A .
CEMENT AND CONCRETE RESEARCH, 1989, 19 (02) :173-176
[2]  
CHINCHON JS, 1987, B LIAISON LABORATOIR, V147, P37
[3]   IRON SULFIDE PRECIPITATION SEQUENCE IN ALBIAN COALS FROM THE MAESTRAZGO BASIN, SOUTHEASTERN IBERIAN RANGE, NORTHEASTERN SPAIN [J].
QUEROL, X ;
CHINCHON, S ;
LOPEZSOLER, A .
INTERNATIONAL JOURNAL OF COAL GEOLOGY, 1989, 11 (02) :171-189