We show that in presence of subsurface oxygen, CO oxidation of oxygen preco
vered Ag(001) modifies the surface in such a way that CO adsorption is stab
ilized up to crystal temperatures of 160 K. When diffusion is activated new
surface oxide phases form, characterized by oxygen both in surface and in
subsurface sites and by a high density of slates just below the Fermi level
. Subsurface oxygen accumulation might therefore be relevant for the unders
tanding of the origin of the pressure gap observed for ethylene epoxidation
and other important catalytic reactions.