Apparent activation energies are determined for oxygen-isotope
exchange reactions between O2, CO, or NO
and preoxidized or prereduced CaO surfaces. Oxygen exchange
between N16O or C16O and isotope
labeled
Ca18O surfaces produced an apparent activation energy of 2
kcal/mol. Similar values are obtained for single-
isotope-exchange between 18O18O and prereduced
Ca16O surfaces. Apparent activation energies of
15−18
kcal/mol are found for single and double exchange between
18O18O and preoxidized Ca16O
surfaces, as well
as for double exchange between 18O18O and
prereduced Ca16O surfaces. The low apparent activation
energies
are believed to result from adsorbed intermediates, whereas the high
values may involve the formation of a
singlet O2 transient. It is shown that eventually the
self-diffusion of oxygen ions in the bulk becomes the
rate-determining step in the isotope-exchange reaction. Apparent
activation energies are determined, and the
values are found to depend on surface treatment, (i.e., 44 kcal/mol
under reducing and 78 kcal/mol under
oxidizing conditions). The involvement of oxygen vacancies under
reducing conditions is discussed.