Oxidation properties of Fe-3, 5 and 7 mass%Al alloys were investigated at 1
073 K in an oxygen gas atmosphere for up to 14.4 ks using thermo-gravimetry
, scanning electron microscope, electron probe microanalyzer, and X-ray dif
fraction analysis. Time dependence of oxidation amounts can be divided into
three regions, i.e., an initial stage with very high oxidation rate, a tra
nsient stage with a rapid decrease in the rate, and then a steady state oxi
dation. The critical times among these stages are 0.1 and 3.6 ks. The 7Al a
lloy oxidized very slowly, due to the formation of a duplex Al2O3 and Fe2O3
scale, in contrast to rapid oxidation of both 5Al and 3Al alloys. The 5Al
alloy oxidized faster than the 3Al alloy during the initial stage, while fo
r longer oxidation the 3Al alloy became faster. The 3Al alloy oxidized to f
orm a thick scale with a tripler structure of Fe2O3, Fe3O4 and FeAl2O4, acc
ompanied with an internal oxidation of duplex FeAl2O4 and Al2O3 zones. Thes
e internal oxides grew perpendicular to the alloy/scale interface. Oxidatio
n of the 5Al ahoy, close to the internal-external transition composition, i
s very complex depending on portions and oxidation times. It has a thin sca
le like the 7Al alloy and a thick scale with internal oxides like the 3Al a
lloy. Further, a precipitate free zone (PFZ) formed in the internal oxidati
on, sandwiched in between the FeAl2O4 and Al2O3 zones, and the formation me
chanism of PFZ was proposed.