The sulfidation of calcined limestone and dolomite was studied in an a
mbient pressure quartz thermogravimetric analyzer (TGA) reactor unit a
t 982-degrees-C. Comparative sulfidation experiments were performed wi
th and without the presence of HCI using both calcined limestone and d
olomite in two particle sizes. The reactant gas contained H2S, H-2, H2
O, and nitrogen. The H2S and HCl content of the reactant gas was chose
n to represent oxygen-blown and air-blown coal gasification environmen
ts. The results of this study indicate that the addition of both steam
and HCI enhances the overall rate of sulfidation reaction and that th
e rate is linearly dependent on the HCI content of the reactant gas up
to 100 ppm for limestone and 150 ppm for dolomite. The sulfidation re
action rate is insensitive to HCI concentrations above these levels fo
r these sorbents. The results obtained in this study suggest that the
enhancement of the sulfidation reaction rate in the presence of HCI is
caused by surface phenomena that are related to the presence of steam
.