We investigated the dynamics of the adsorption of O₂ on Ag(110) with the molecular beam technique combined with EEL spectroscopy and with the method of King and Wells. The initial sticking coefficient S₀ is reported for molecules impinging along both high symmetry azimuthal directions 〈001〉 and 〈11̄0〉 as a function of total energy and angle of incidence of the molecules and crystal temperature. The initial sticking coefficient is anisotropic for low as well as for room temperature adsorption. The dependence of the sticking coefficient on the temperature of the sample, T_s, indicates that adsorption takes place directly into the molecular well. Dissociation is eventually induced thermally for T_s≳150 K. The physisorbed state plays no role in the chemisorption process in the investigated impact energy range.

We show that dissociative oxygen adsorption on Ag(001) induces below room temperature a missing row $2\sqrt{2}\times \sqrt{2}$ reconstruction of the substrate. As demonstrated by the analysis of the photoelectron diffraction patterns, the oxygen atoms sit thereby in a $c(2\mathrm{}\times 2)$ arrangement in the previous fourfold hollow sites nearly coplanar with the Ag atoms, while rows of substrate atoms are removed along the $\left[100\right]$ directions. Annealing the crystal above 350 K restores the $p(1\mathrm{}\times 1)$ symmetry and the oxygen moves to $0.6\hspace{0.5em}\AA$ above the fourfold hollow site. It becomes then more oxidic in nature, as demonstrated by the shift of the $\mathrm{O}1s$ level from 530.3 eV to 528.3 eV. The phase transition affects also the $\mathrm{O}2s$ and $\mathrm{O}2p$ levels as well as the surface component of $\mathrm{Ag}{3d}_{5/2}.$ The vibrational frequency of the oxygen adatoms against the surface decreases at the phase transition, in accord with the larger adsorption distance. The higher temperature phase is active towards CO and ${\mathrm{C}}_2{\mathrm{H}}_4$ oxidation, while the low-temperature phase is not. When cooling the sample below room temperature the reconstructed phase is restored. The time constant of this process as well as the chemical reactivity of the high-temperature phase are weakly reproducible since they depend on the previous history, i.e., presumably on the subsurface oxygen content of the sample.