Ferrous alloys containing significant volume fractions of chromium car
bides were formulated so as to contain an overall chromium level of 15
% (by weight) but a nominal metal matrix chromium concentration of onl
y 11%. Their oxidation at 850 degrees C in pure oxygen led to either p
rotective Cr2O3 scale formation accompanied by subsurface carbide diss
olution or rapid growth of iron-rich oxide scales associated with rapi
d alloy surface recession, which engulfed the carbides before they cou
ld dissolve. Carbide size was important in austenitic alloys: an as-ca
st Fe-15Cr-0.5C alloy contained relatively coarse carbides and failed
to form a Cr2O3 scale, whereas the same alloy when hot-forged to produ
ce very fine carbides oxidized protectively. In ferritic alloys, howev
er, even coarse carbides dissolved sufficiently rapidly to provide the
chromium flux necessary to form and maintain the growth of a Cr2O3 sc
ale, a result attributed to the high diffusivity of the ferrite phase,
Small additions of silicon to the as-cast Fe-15Cr-0.5C alloy rendered
it ferritic and led to protective Cr2O3 growth. However, when the sil
icon-containing alloy was made austenitic (by the addition of nickel),
it still formed a protective Cr2O3 scale, showing that the principal
function of silicon was in modifying the scale-alloy interface.