Abstract
AbstractThe oxidation of high‐purity aluminium sheet in dry oxygen, moist oxygen, carbon dioxide and carbon monoxide (at total pressure 1.333 × 103 Nm−2) was studied in the range 673–923°K, using a vacuum microbalance to follow weight gains. 14CO2 and 14CO were used to elucidate the mechanism of the oxidation in these gases and to estimate the extent of carbon deposition in the oxide layer.The rate of oxidation in moist oxygen was similar to that in dry oxygen, the principle reaction being 2Al + 3H2O ← Al2O3 + 3H2.It is suggested that there are three steps in the reaction in CO2, viz. 2Al+3CO2 ← Al2O3 + 3CO, followed by 2Al + 3CO ← Al2O3 + 3C, and about 10% of the deposited carbon reacting further by 4Al + 3C ← Al4C3. Only the last two reactions are operative in carbon monoxide.The Arrhenius plots show a distinct break in the region 773–823°K for both carbon monoxide and carbon dioxide, but not for dry or moist oxygen. This is tentatively explained by a change in the rate‐determining process from diffusion via grain boundaries or cracks in the oxide, to lattice diffusion. It is suggested that carbon may become mobile in the oxide film between 773 and 823°K and may tend to congregate in the grain boundaries and cracks.The oxide film remained protective throughout the duration of the experiments in all the gases.
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