Fritz-Haber-Institut der Max-Planck-Gesellschaft, D-14195, Berlin, Germany
Abstract:
Experiments using photo emission electron microscopy (PEEM) reveal that regions on a Pt(110) surface covered by chemisorbed O atoms may be converted into a subsurface O-phase, provided that it is preceded by the interaction of CO initiating the 1 × 2 → 1 × 1 transformation of the surface structure. However, the presence of subsurface oxygen also favors lifting of the surface reconstruction. A mathematical model of this process is developed using parameters derived from previous independent experiments and numerical simulations fitting new data to experimental findings.