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Operation of calcium-birnessite water-oxidation anodes: interactions of the catalyst with phosphate buffer anions

MPS-Authors
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Jones,  Travis
Inorganic Chemistry, Fritz Haber Institute, Max Planck Society;

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Sulzmann,  Frederic
Inorganic Chemistry, Fritz Haber Institute, Max Planck Society;

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Knop-Gericke,  Axel
Max-Planck-Institut für Chemische Energiekonversion;
Inorganic Chemistry, Fritz Haber Institute, Max Planck Society;

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Schlögl,  Robert
Max-Planck-Institut für Chemische Energiekonversion;
Inorganic Chemistry, Fritz Haber Institute, Max Planck Society;

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Skorupska,  Katarzyna
Max-Planck-Institut für Chemische Energiekonversion;
Inorganic Chemistry, Fritz Haber Institute, Max Planck Society;

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d1se01076j.pdf
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引用

Ronge, E., Ohms, J., Roddatis, V., Jones, T., Sulzmann, F., Knop-Gericke, A., Schlögl, R., Kurz, P., Jooss, C., & Skorupska, K. (2021). Operation of calcium-birnessite water-oxidation anodes: interactions of the catalyst with phosphate buffer anions. Sustainable Energy & Fuels. doi:10.1039/D1SE01076J.


引用: https://hdl.handle.net/21.11116/0000-0009-5D8A-4
要旨
Investigating the interfaces between electrolytes and electrocatalysts during electrochemical water oxidation is of great importance for an understanding of the factors influencing catalytic activity and stability. Here, the interaction of a well-established, nanocrystalline and mesoporous Ca-birnessite catalyst material (initial composition K0.2Ca0.21MnO2.21·1.4H2O, initial Mn-oxidation state ∼+3.8) with an aqueous potassium phosphate buffer electrolyte at pH 7 was studied mainly by using various electron microscopy and X-ray spectroscopy techniques. In comparison to electrolyte solutions not containing phosphate, the investigated Ca-birnessite electrodes show especially high and stable oxygen evolution activity in phosphate buffer. During electrolysis, partial ion substitutions of Ca2+ by K+ and OH/O2− by HnPO4(3−n)− were observed, leading to the formation of a stable, partially disordered Ca–K–Mn–HnPO4–H2O layer on the outer and the pore surfaces of the active electrocatalyst material. In this surface layer, Mn3+ ions are stabilized, which are often assumed to be of key importance for oxygen evolution catalysis. Furthermore, evidence for the formation of [Ca/PO4/H2O] complexes located between the [MnO6] layers of the birnessite was found using the soft Ca 2p and Ca L-edge X-ray spectroscopy. A possible way to interpret the observed, obviously very favorable “special relationship” between (hydrogen)phosphates and Ca-birnessites in electrocatalytic water oxidation would be that HnPO4(3−n)− anions are incorporated into the catalyst material where they act as stabilizing units for Mn3+ highly active centers and also as “internal bases” for the protons released during the water-oxidation reaction.