High purity iron and a low carbon, low silicon steel were oxidised at temperatures of 800 to 1200oC, in atmospheres of N2-H2-H2O and N2-O2-H2O. Scales of wüstite grew at low oxygen potentials, and of FeO/Fe3O4/Fe2O3 at high potentials. In both cases, kinetics were parabolic after an initial transient period. The iron and steel behaved similarly in O2/H2O gases, but not in H2/H2O. Weight uptake kinetics for both metals were initially linear, changing to parabolic with time as diffusion slowed and became rate-controlling [1]. Iron generally reacted faster than steel, but eventually developed parabolic kinetics. The effect of p(O2) at fixed p(H2O) on kw for iron and steel is seen in Fig. 1 to be functionally similar. However, whereas the oxidation rate of steel is strongly dependent on p(H2O), that of iron is not [2,3]. The Arrhenius plot in Figure 2 shows that activation energies for the two materials are rather similar at 157 kJ mol-1 for temperatures of 800 to 1100oC, but iron oxidises almost three orders of magnitude faster than steel. However, at 1200oC, oxidation rates are closely similar.The predictions of the Wagner model of rate control by lattice diffusion of iron vacancies is shown to be quantitatively successful for reaction of pure iron in H2/H2O. The slower rates observed for steel are attributed to defect interactions with impurity species, perhaps including a hydrogen-bearing species. Gas composition effects on the parabolic rate constant, kw , for steel can be described by the expression: kw = A p(O2)1/4 + B p(H2O)1/2 (1)where p denotes partial pressure and A, B are constants. A model based on simultaneous diffusion of singly charged vacancies on cation sites and hydroxyl ions on anion sites is shown to account for this relationship. Scaling rates in O2/H2O also increased with water vapour level, a result attributed to gas phase transport within oxide pores which were present in the scales, but absent in wüstite grown in H2/H2O. Rates for iron and the steel were the same, in each case reflecting mainly the growth of a thick wüstite layer. The lack of impurity effects on the steel oxidation is attributed to the failure of hydrogen-bearing species to penetrate the outer layers of magnetite and hematite which form in these gases.