We analyze data of isotope tracer studies of the interaction of
18O2
gas with
Si16O2
films thermally grown on silicon substrates in dry oxygen. We find that the results of the tracer studies are consistent with a model which includes (i) isotopic exchange between the
18O2
gas molecules and the 16O atoms of the original oxide, and (ii) diffusion of network atoms by an interstitialcy defect mechanism involving
O2
molecules. These findings show that the incorporation of 18O into the surface region of the oxide does not indicate that new oxide has grown at the surface, as has been previously suggested. Thus, there is no need to hypothesize the existence of such a defect, as oxygen vacancies, to be involved in oxide growth.