The sulfur capture capacities of 11 limestones and six dolomites were
determined by means of a pressurized thermogravimetric analyser. The d
eterminations were made under conditions relevant to pressurized fluid
ized bed combustion. The actual experiments were performed at two diff
erent temperatures (850 and 950 degrees C) and at a pressure of 1.5 MP
a. Additionally, some experiments were performed at atmospheric pressu
re for comparison. The particle size of the samples was screened to 20
0-400 mu m. By using a thin (1 mm) sample layer diluted with an inert
material (quartz sand), the external mass transfer and the interpartic
le diffusion problems were excluded. For each experiment the conversio
n versus time curve was determined. The results showed great variation
s between different sorbent qualities. Conversions between 7 and 83% w
ere measured. The sulfur absorption capacity order was approximately t
he same under both atmospheric and pressurized conditions. Higher temp
erature resulted in considerably higher conversion. The temperature ef
fect differed between the absorbents and was clearly more pronounced f
or the dolomites than for the limestones. This resulted in one absorbe
nt being more efficient at 850 degrees C, while the other absorbent wa
s more efficient at 950 degrees C.