EVIDENCE FOR OXYGEN ADATOMS ON TIO2(110) RESULTING FROM O-2 DISSOCIATION AT VACANCY SITES

Citation
Ws. Epling et al., EVIDENCE FOR OXYGEN ADATOMS ON TIO2(110) RESULTING FROM O-2 DISSOCIATION AT VACANCY SITES, Surface science, 413, 1998, pp. 333-343
Citations number
23
Categorie Soggetti
Chemistry Physical
Journal title
ISSN journal
00396028
Volume
413
Year of publication
1998
Pages
333 - 343
Database
ISI
SICI code
0039-6028(1998)413:<333:EFOAOT>2.0.ZU;2-C
Abstract
Annealing TiO2(110) in vacuum at high temperature (above about 800 K)g enerates oxygen vacancy sites that are associated with reduced surface cations. Numerous studies have shown that these sites can be oxidized by exposure to molecular oxygen, but the mechanism and temperature de pendence of this oxidation process are not well understood. We present results that suggest low temperature (1600 K) O-2 exposure oxidizes o xygen vacancies but also leaves oxygen-containing species on the surfa ce that we propose are oxygen adatoms, The presence of these oxygen ad atoms is evident in the temperature-programmed desorption (TPD) spectr um of water. Oxidizing the vacuum annealed surface at 700 K produces a fully oxidized TiO2(110) surface that gives a single monolayer TPD st ate for water at 270 K, Exposing the vacuum annealed surface to O-2 at temperatures between 90 and 600 K followed by water adsorption at 90 K results in a new water TPD state 25 K higher in temperature. Similar results were obtained using ammonia instead of water. Isotopic labeli ng experiments, in which the vacuum annealed surface was dosed with O- 18(2) at 135 K followed by (H2O)-O-16 at 135 K, indicate that the new water TPD state results from recombinative desorption, whereas no such effect is observed for the surface exposed to O-18(2) at 700 K. The e ffect on water is also absent in TPD if the low temperature O-2 treate d surface is heated to 600 K prior to water adsorption at 90 K, sugges ting that the oxygen adatoms desorb from the surface or diffuse into t he bulk. We propose that at low temperatures, O-2 dissociates at oxyge n vacancies filling each defect site with one O atom and depositing a second O adatom at a five-coordinate Ti4+ site or that O-2 interacts w ith surface hydroxyl groups resulting in O-2 dissociation and the pres ence of the O adatom. The new dissociative water chemistry results fro m the interaction of water molecules with these oxygen adatoms. After high temperature (1600 K) O-2 exposure, no dissociative water chemistr y is observed, suggesting that these oxygen adatoms are not present on the surface. The presence of surface O adatoms may explain inconsiste ncies in the literature regarding the reactivity of water, and potenti ally other species, on TiO2(110). These results also detail the import ance of sample preparation techniques on the chemistry which can occur at a solid surface. (C) 1998 Elsevier Science B.V. All rights reserve d.