Oxygen-induced surface phase transformation of Pd(111): sticking, adsorption and desorption kinetics

B. Klötzer1, K. Hayek1, C. Konvicka2, E. Lundgren2*, P. Varga2

1Institut für Physikalische Chemie, Universität Innsbruck, A-6020 Innsbruck, Austria
2Institut für Allgemeine Physik, Technische Universität Wien, A-1040 Wien, Austria
*Present address: Department of Synchrotron Radiation Research, Institute of Physics, University of Lund, S-22100 Lund, Sweden

Surf. Sci. 482-485 (2001) 237-242

Adsorption and desorption of oxygen on Pd(111) were studied by high-flux molecular beam adsorption, LEED, TDS and scanning tunnelling microscopy (STM) between 300 and 623 K sample temperature for oxygen coverages THETA_O up to 1 ML. While adsorption below THETA_O = 0.25 is precursor mediated and proceeds without changes of the Pd substrate, it is activated for THETA_O > 0.25 and induces a massive change of the surface structure. STM reveals the formation of a new surface phase which consists of islands with a local oxygen coverage of 1 ML but less Pd atoms than the bulk-terminated (111) layer. Its formation and decay require activated mass transport of Pd and O atoms over mesoscopic distances. Due to island growth of this phase the oxygen sticking decreases linearly between THETA_O = 0.25 and 1 ML. For THETA_O > 0.25 ML the TPD rate maxima are shifted towards higher temperature with increasing initial coverage, indicating autocatalytic desorption kinetics. Desorption occurs preferentially from a dilute chemisorbed phase on Pd(111) terraces, with the islands of the high oxygen-density phase acting as a reservoir for O. The experimental TPD data can be well described by a simple mathematical model considering phase equilibrium during desorption.

Corresponding author: B. Klötzer. (Universität Innsbruck). Reprints also available from P. Varga (varga< encoded email address >).

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