Abstract
Using x-ray photoelectron spectroscopy of the oxygen core level, the ratio between intact () and dissociated (OD) water in the hydrated stoichiometric surface is determined at varying coverage and temperature. In the submonolayer regime, both the ratio and the core-level binding energy of () decrease with temperature. The observed variations in are shown with density functional theory to be governed crucially and solely by the local hydrogen bonding environment, revealing a generally applicable classification and details about adsorption motifs.
- Received 9 September 2020
- Accepted 3 December 2020
DOI:https://doi.org/10.1103/PhysRevLett.126.016102
Published by the American Physical Society under the terms of the Creative Commons Attribution 4.0 International license. Further distribution of this work must maintain attribution to the author(s) and the published article’s title, journal citation, and DOI.
Published by the American Physical Society