The time dependence of the wet oxidation of high-Al-content AlGaAs can be e
ither linear, indicating reaction-rate limitation, or parabolic, indicating
diffusion-limited rates. The transition from linear to parabolic time depe
ndence can be explained by the increased rate of the formation of intermedi
ate As2O3 versus its reduction to elemental As. A steadily increasing thick
ness of the As2O3-containing region at the oxidation front will shift the p
rocess from the linear to the parabolic regime. This shift from reaction-ra
te limited (linear) to diffusion-limited (parabolic) time dependence is fav
ored by increasing temperature or increasing Al mole fraction. (C) 1999 Ame
rican Institute of Physics. [S0003-6951(99)01527-2].