Issue 17, 2021

Intermetallic Fe6Ge5 formation and decay of a core–shell structure during the oxygen evolution reaction

Abstract

Herein, we report on intermetallic iron germanide (Fe6Ge5) as a novel oxygen evolution reaction (OER) precatalyst with a Tafel slope of 32 mV dec−1 and an overpotential of 272 mV at 100 mA cm−2 in alkaline media. Furthermore, we uncover the in situ formation of a core–shell like structure that slowly collapses under OER conditions.

Graphical abstract: Intermetallic Fe6Ge5 formation and decay of a core–shell structure during the oxygen evolution reaction

Supplementary files

Article information

Article type
Communication
Submitted
10 Dec 2020
Accepted
22 Jan 2021
First published
22 Jan 2021
This article is Open Access
Creative Commons BY-NC license

Chem. Commun., 2021,57, 2184-2187

Intermetallic Fe6Ge5 formation and decay of a core–shell structure during the oxygen evolution reaction

J. N. Hausmann, R. A. Khalaniya, C. Das, I. Remy-Speckmann, S. Berendts, A. V. Shevelkov, M. Driess and P. W. Menezes, Chem. Commun., 2021, 57, 2184 DOI: 10.1039/D0CC08035G

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