“…For oxygen, several attempts to estimate the coefficients for both chemical diffusion and self-diffusion (i.e., diffusion in presence or absence of a concentration gradient, respectively) have been made, mostly with indirect approaches, e.g., measurements of electrical conductivity after reduction of oxidised samples [4], thermogravimetry following steam oxidation [5], or gas-solid isotopic exchange coupled with sample sectioning [6]. As well as the problem of the inconsistency in the reported values, the applicability of these data to the prediction of oxidation kinetics in final disposal scenarios is further constrained by the fact that all experiments have been performed in temperature ranges between 600 and 1800 K, whereas in a final repository the temperature can be expected to be in the range 290-370 K [7].…”