Devolatilized (950-degrees-C) anthracite was activated in 0.1 MPa CO2
at 950-degrees-C and 0.1 MPa air at 425-degrees-C and 450-degrees-C. A
t comparable gasification rates and carbon burn-offs in CO2 and air, l
arger surface areas and pore volumes were developed by activation in C
O2. This is attributed foremost to less uniform activation through the
anthracite particles when gasification takes place in air. Also, the
formation of a stable oxygen complex, concurrent with carbon gasificat
ion in air, may reduce the efficiency of anthracite activation.