Source abstract
Abstract
High Resolution Image Download MS PowerPoint Slide Brownmillerite-type Ca 2 FeCoO 5 (CFCO) is a remarkable electrocatalyst for oxygen evolution reactions (OER) under alkaline and neutral conditions. In our recent study, crystalline CFCO nanoparticles with single-nanometer dimensions were formed on TiO 2 nanoparticles using a reverse-micelle (RM) deposition method. In this study, we report the RM deposition synthesis of ultrathin CFCO layers with varying interactions between the CFCO precursors, which were hydroxides formed in RM, and oxide supports during the loading process: CFCO ultrathin layers with several atomic thicknesses were formed on ZnO, Al 2 O 3, and PbO 2 with positive surface charges, whereas CFCO nanoparticles with diameters of ∼10 nm were formed on TiO 2 and SnO 2 with negative surface charges. The CFCO precursors formed in the RM had a negative charge, indicating that the CFCO precursors were uniformly loaded on ZnO, Al 2 O 3, and PbO 2 via strong interactions between the positive and negative charges, leading to ultrathin CFCO layers after calcination. The electrocatalytic activities of the ultrathin CFCO layers for the OER under concentrated alkaline conditions were higher than those of the CFCO nanoparticles. It is speculated that the calcium defects in the CFCO ultrathin layers easily and rapidly change to active cobalt iron species for the OER under concentrated alkaline conditions.
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Affiliations
Center for Research on Green Sustainable Chemistry, Tottori University, 4-101 Koyama-cho Minami, Tottori 680-8552, Japan
Department of Applied Chemistry, Kogakuin University, 2665-1 Nakano-cho, Hachioji, Tokyo 192-0015, Japan
Faculty of Engineering, Hokkaido University, Kita 13, Nishi 8, Kita-ku, Sapporo 060-8628, Japan
Institute for Catalysis, Hokkaido University, Kita21, Nishi10, Kita-ku, Sapporo 001-0021, Japan
Funding
Osaka University · Ministry of Education, Culture, Sports, Science and Technology · Tottori University · Japan Society for the Promotion of Science · JKA Foundation