The deviation from stoichiometry, delta, in (CrxFe1-x)(3-delta)O-4 was
measured by thermogravimetry at 1200 degrees C as a function of oxyge
n activity, a(02), and cationic composition, x. Moreover, cation trace
r diffusion coefficients, D-Me, for Me = Co, Cr, Fe and Mn, were expe
rimentally determined using radioactive isotopes, Co-60, Cr-51, Fe-59
and Mn-54. delta versus log a(02) plots for different (x) displayed S-
shaped curves. The experimental data suggested that cation vacancies a
nd cation interstitials were the majority defects at high and low oxyg
en activities, respectively. V-shaped curves were observed in D-Me ve
rsus log a(02) plots. The observed oxygen activity dependence indicate
d that the diffusion of Co, Cr, Fe and Mn in (CrxFe1-x)(3-delta)O-4 at
high oxygen activities is governed by cation vacancies and at low oxy
gen activities by cation interstitials. Mean cation mobilities were de
rived by combining non-stoichiometry and cation diffusion information.