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Climbing with support: scaling the volcano relationship through support–electrocatalyst interactions in electrodeposited RuO2for the oxygen evolution reactionElectronic supplementary information (ESI) available: Computational details; physiochemical characterization; electrochemical characterization; LSV curves of thick and thin films of RuO2on different metal-modified carbon supports; XRD of electrodeposited metallic interlayers on a carbon support (Au-, Pt-, Cu, Ti-, Ru); XPS spectra of the O-1s (520–550 eV) zone for Au-, Pt-, Cu- and Ti-interlayered carbon supports; loading and approximate thickness of thin-RuO2and thick-RuO2on different metal-interlayered carbon supports; electrochemical surface area of electrodeposited thin film RuO2and thick film RuO2on different metal-modified carbon supports; Tafel slope of electrodeposited thin film RuO2and thick film RuO2on different metal-modified carbon supports. See DOI: 10.1039/d1cy00375e

Authors :
Saha, Sulay
Kishor, Koshal
Pala, Raj Ganesh S.
Source :
Catalysis Science & Technology; 2021, Vol. 11 Issue: 13 p4342-4352, 11p
Publication Year :
2021

Abstract

We demonstrate an approach towards modulating electrocatalysis in an ultrathin RuO2oxygen electrocatalytic overlayer viaoptimal charge transfer between the support and the electrocatalyst. The governing heuristics for the choice of support that would result in ‘climbing up’ the volcano curve for oxygen evolution reaction (OER) electrocatalysts are delineated. Ultrathin Ru is deposited on metal coated over porous carbon supports, denoted by M/C, where M = Au, Cu, Pt, Ti and Ru, followed by the electrochemical oxidation of the Ru overlayer, which makes it possible for the support to retain its metallic character without getting oxidized to the less conductive metal oxide. An increase in the specific activity of thin RuO2is achieved with Au/C and Pt/C-supports against the Ru/C-support. The consolidated experimental and computational results suggest that the increase of the specific activity and subsequent ‘climbing up’ the volcano map for OER electrocatalysts is due to the interfacial charge transfer and support-induced electrocatalyst faceting. With the increase of the thickness, the support effect on the electrocatalyst activity gets reduced and only the conductivity of the support plays a dominant role in determining the OER activity.

Details

Language :
English
ISSN :
20444753 and 20444761
Volume :
11
Issue :
13
Database :
Supplemental Index
Journal :
Catalysis Science & Technology
Publication Type :
Periodical
Accession number :
ejs56993903
Full Text :
https://doi.org/10.1039/d1cy00375e