. Pure CaSO4 is known to be very stable under oxidizing conditions at FBC bed temperatures (800-900.DEG.C.). However, the temperature of burning fuel
particles or the temperature near fuel feed points where volatile matter combustion occurs are considered to be higher than the average bed
temperature. In addition, there exist coal ash particles around the sulfated limestone particles (or fine sulfated limestone powders around coal
particles), and the temperature of CaSO4 decomposition may be affected by the coexistence. The objective of this work is to evaluate the decomposition
rate of CaSO4 mixed with coal ash. The mixture was heated up to 1350.DEG.C. in oxidizing atmosphere, measuring SO2 release and weight change of the
mixture. Pure CaSO4 was found to be very stable and decomposition occurred only at higher temperatures than 1250.DEG.C.. When coal ash was mixed with
CaSO4, the decomposition and SO2 release occurred at relatively lower temperatures, for example, 1000.DEG.C. |