EN
The oxygen and hydrogen atoms co-adsorption experiment on Pd(111) is modelled using kinetic Monte Carlo method. We consider O-O, H-H, and O-H interactions and several kinetic processes (diffusion, surface and subsurface H-atoms exchange and water-formation reaction) leading to the phase transition (2×2)_O → (√3×√3)_O with increase in H-coverage. We also demonstrate how reverse phase transition (√3×√3)_O → (2×2)_O occurs due to hydrogen dissolution into subsurface in the absence of hydrogen gas. At higher temperature we observe the disappearance of (2×2)_O oxygen islands due to water-formation reaction.