Oxidation of MgO-C refractories containing 20 wt-% graphite was conducted b
y measuring the weight loss at regular intervals at various temperatures fi
om 800 to 1600 degrees C in ail. The rate of decarburisation increased wit
h rise in temperature from 800 to 1400 degrees C and then remained more ol
less constant from 1400 to 1600 degrees C. The oxidation kinetics were anal
ysed in detail and reaction rate models derived for the temperature range 8
00-1400 degrees C. The reaction rate was found to be controlled by diffusio
n of oxygen through the decarburised layer. At higher temperatures (>1400 d
egrees C), oxidation of graphite also takes place indirectly by the reactio
n MgO(s)+C(s)-->Mg(g)+ CO(g). The magnesium vapour thus produced is reoxidi
sed at the outer surface and redeposited as MgO. This leads to a reduction
in porosity in the decarburised outer shell and, consequently, a reduction
in the rate of oxidation. (C) 2000 IoM Communications Ltd.