The kinetics of the oxygen exchange reaction between carbon dioxide and carbon monoxide were measured on iron, wu¨stite, and magnetite surfaces. This was done through the use of an isotope exchange technique. The measured rate constants are dependent on the oxygen activity. This dependence is expressed by k a = k o a O Àm . The parameter m was found to have values between 0 and 1. It was found that, in the iron region, the apparent rate constant was independent of the oxygen partial pressure (i.e., m = 0) at 1123 K (850°C) and that it was inversely dependent on the oxygen partial pressure (i.e., m = 1) for the magnetite region at 1123 K (850°C) and 1268 K (995°C). In the wu¨stite region, m was found to be equal to 0.51, 0.66, and 1.0 for the w 1 , w 2 , and w 3 pseudo phases, respectively, at 1268 K (995°C). At 1123 K (850°C), in wu¨stite, m was found to be equal to 0.59 and to 1.0 for the w 1 ¢ and w 3 ¢ pseudo phases, respectively.