M. Legall et al., SELF-DIFFUSION IN ALPHA-AL2O3 AND GROWTH-RATE OF ALUMINA SCALES FORMED BY OXIDATION - EFFECT OF Y2O3 DOPING, Journal of Materials Science, 30(1), 1995, pp. 201-211
In many cases, alumina scales are assumed to grow predominantly by oxy
gen diffusion, but some authors have found that the growth can be cont
rolled by aluminium diffusion. These mechanisms can be modified by act
ive elements. The problem with alumina is that there is a lack of data
about self-diffusion coefficients, and, due to the stoichiometry of a
lumina, diffusion data correspond to an extrinsic diffusion mechanism
so that it is not possible to compare oxygen and aluminium diffusion c
oefficients. In order to obtain information about the alumina scale gr
owth mechanism, oxygen (O-18) and aluminium (Al-26) self-diffusion coe
fficients in Al2O3 were determined in the same materials and in the sa
me experimental conditions, thus allowing a direct comparison. For bot
h isotopes, bulk and sub-boundary diffusion coefficients were determin
ed in single crystals of undoped alumina. Grain-boundary diffusion coe
fficients have been computed only for oxygen diffusion in polycrystals
. Oxygen diffusion has been also studied for yttria-doped alpha-alumin
a in the lattice, sub-boundaries and grain boundaries. Oxygen and alum
inium bulk diffusion coefficients are of the same order of magnitude.
In the sub-boundaries, aluminium diffusion is slightly faster than oxy
gen diffusion. Yttria doping induces a slight increase of the oxygen b
ulk diffusion, but decreases the grain-boundary diffusion coefficients
on account of segregation phenomena. These results are compared with
the oxidation constants of alumina former alloys (alloys which develop
an alumina scale by oxidation). It appears that neither lattice self-
diffusion nor grain boundary self-diffusion can explain the growth rat
e of alumina scales. Such a situation is compared to the case of Cr2O3
.