The rates of the alkali catalysed water-gas shift reaction (WGS) and s
team gasification of carbon have been studied at 1.5 x 10(5) Pa total
pressure as a function of temperature (800-1000 K), feed composition (
pure H2O or mixtures of H2O with either CO2, H-2 or CO), alkali metal
(Na, K, Rb, Cs) and K2CO3 loading (0-25 wt%). A four step kinetic mode
l is selected which describes the observed temperature dependency of t
he reaction rates and inhibition by CO, H-2 and CO2. Only beyond 950-1
000 K is the catalysed WGS oxygen exchange at thermodynamic equilibriu
m. In H2O atmospheres, with low CO2 or CO contents, the various alkali
elements exhibit similar activities due to high dispersion. At higher
CO2 concentrations the H2O gasification rate is strongly lowered, whi
le CO can completely inhibit H2O gasification, and only the WGS reacti
on takes place. The effect of potassium loading on the H2O gasificatio
n activity is similar to that observed for gasification in CO2.