The effect of the presence of limestone and dolomite in coal, and calc
ium in lignite, on atmospheric-pressure temperature-programmed reducti
on (AP-TPR) analysis was studied. AP-TPR experiments were carried out
on a bituminous coal with added limestone and dolomite and on a demine
ralized lignite. The results showed that both calcium minerals capture
d the gaseous H2S formed under AP-TPR conditions and produced CaS. Con
sequently the sulfur recovery monitored was too low and the AP-TPR kin
etograms were deformed. The study also showed that the influence of do
lomite is greater than of limestone. AP-TPR analysis of lignite demine
ralized and then loaded with calcium ions again showed a clear lowerin
g of sulfur comparable with that of dolomite, but starting at a higher
temperature. Copyright (C) 1997 Elsevier Science Ltd.