Towards identifying the active sites on RuO(110) in catalyzing oxygen evolution

• Published in: Energy & environmental science 2017-12, Vol.1 (12), p.2626-2637
• Main Authors: Rao, Reshma R, Kolb, Manuel J, Halck, Niels Bendtsen, Pedersen, Anders Filsøe, Mehta, Apurva, You, Hoydoo, Stoerzinger, Kelsey A, Feng, Zhenxing, Hansen, Heine A, Zhou, Hua, Giordano, Livia, Rossmeisl, Jan, Vegge, Tejs, Chorkendorff, Ib, Stephens, Ifan E. L, Shao-Horn, Yang
• Format: Article
• ISSN: 1754-5692; 1754-5706
• DOI: 10.1039/c7ee02307c

While the surface atomic structure of RuO 2 has been well studied in ultra high vacuum, much less is known about the interaction between water and RuO 2 in aqueous solution. In this work, in situ surface X-ray scattering measurements combined with density functional theory (DFT) were used to determine the surface structural changes on single-crystal RuO 2 (110) as a function of potential in acidic electrolyte. The redox peaks at 0.7, 1.1 and 1.4 V vs. reversible hydrogen electrode (RHE) could be attributed to surface transitions associated with the successive deprotonation of -H 2 O on the coordinatively unsaturated Ru sites (CUS) and hydrogen adsorbed to the bridging oxygen sites. At potentials relevant to the oxygen evolution reaction (OER), an -OO species on the Ru CUS sites was detected, which was stabilized by a neighboring -OH group on the Ru CUS or bridge site. Combining potential-dependent surface structures with their energetics from DFT led to a new OER pathway, where the deprotonation of the -OH group used to stabilize -OO was found to be rate-limiting. Surface structural transitions and active sites are identified using X-ray scattering and density functional theory.