Abstract
X-ray photoelectron (XPS) experiments at normal and grazing emission are performed, demonstrating the labile nature of the anatase TiO2(101) surface after argon cluster ion sputtering and the propensity of oxygen vacancies to migrate subsurface at room temperature. Near-ambient XPS (NAP-XPS) shows that molecular water adsorbs on the anatase TiO2(101) surface at pressures of 0.6 mbar and above, at room temperature, in a mixed molecular and dissociated state. Water adsorbs in a similar fashion on both sputtered and stoichiometric surfaces and reaches a saturation point between 0.6 and 1.8 mbar at room temperature. This means there is little difference in reactivity with regards to water adsorption on both sputtered and stoichiometric surfaces, giving credence to the theory that anatase has superior photocatalytic activity over rutile due to the tendency of oxygen vacancies to lie subsurface, therefore being able to contribute to photocatalysis without being quenched by adsorbates.
Highlights
The two most studied faces of TiO2 are the rutile (110) and the anatase (101) surfaces
We investigate the exposure of the stoichiometric and sputtered anatase TiO2(101) surfaces to water at pressures of 0.6, 1.8, and 6.0 mbar and show that water adsorbs in a similar fashion on both surfaces, both dissociative and molecular
We show the O 1s spectrum recorded following the water exposure experiments after the high-pressure cell had been evacuated and the pressure had returned to 1 × 10−8 mbar
Summary
The two most studied faces of TiO2 are the rutile (110) and the anatase (101) surfaces.
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