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Zn 0.35 Co 0.65 O – A Stable and Highly Active Oxygen Evolution Catalyst Formed by Zinc Leaching and Tetrahedral Coordinated Cobalt in Wurtzite Structure
Author(s) -
Wahl Sebastian,
ElRefaei Sayed M.,
Buzanich Ana Guilherme,
Amsalem Patrick,
Lee KugSeung,
Koch Norbert,
Doublet MarieLiesse,
Pinicola
Publication year - 2019
Publication title -
advanced energy materials
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 10.08
H-Index - 220
eISSN - 1614-6840
pISSN - 1614-6832
DOI - 10.1002/aenm.201900328
Subject(s) - overpotential , oxygen evolution , catalysis , cobalt , materials science , wurtzite crystal structure , zinc , water splitting , leaching (pedology) , inorganic chemistry , electrochemistry , chemical engineering , chemistry , metallurgy , electrode , photocatalysis , environmental science , soil science , engineering , soil water , biochemistry
To arrive to sustainable hydrogen‐based energy solutions, the understanding of water‐splitting catalysts plays the most crucial role. Herein, state‐of‐the‐art hypotheses are combined on electrocatalytic active metal sites toward the oxygen evolution reaction (OER) to develop a highly efficient catalyst based on Earth‐abundant cobalt and zinc oxides. The precursor catalyst Zn 0.35 Co 0.65 O is synthesized via a fast microwave‐assisted approach at low temperatures. Subsequently, it transforms in situ from the wurtzite structure to the layered γ‐Co(O)OH, while most of its zinc leaches out. This material shows outstanding catalytic performance and stability toward the OER in 1 m KOH (overpotential at 10 mA cm −2 η initial = 306 mV, η 98 h = 318 mV). By comparing the electrochemical results and ex situ analyses to today's literature, clear structure‐activity correlations are able to be identified. The findings suggest that coordinately unsaturated cobalt octahedra on the surface are indeed the active centers for the OER.
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