Author
Listed:
- Zoel Codolà
(Institut de Química Computacional i Catàlisi (IQCC) and Departament de Química, Universitat de Girona, Campus de Montilivi)
- Laura Gómez
(University of Minnesota)
- Scott T. Kleespies
(Serveis Tècnics de Recerca (STR), Parc Cientific i Tecnològic, Universitat de Girona)
- Lawrence Que Jr
(Serveis Tècnics de Recerca (STR), Parc Cientific i Tecnològic, Universitat de Girona)
- Miquel Costas
(Institut de Química Computacional i Catàlisi (IQCC) and Departament de Química, Universitat de Girona, Campus de Montilivi)
- Julio Lloret-Fillol
(Institut de Química Computacional i Catàlisi (IQCC) and Departament de Química, Universitat de Girona, Campus de Montilivi)
Abstract
The non-haem iron complex α-[FeII(CF3SO3)2(mcp)] (mcp=(N,N′-dimethyl-N,N′-bis(2-pyridylmethyl)-1,2-cis-diaminocyclohexane) reacts with CeIV to oxidize water to O2, representing an iron-based functional model for the oxygen evolving complex of photosystem II. Here we trap an intermediate, characterized by cryospray ionization high resolution mass spectrometry and resonance Raman spectroscopy, and formulated as [(mcp)FeIV(O)(μ-O)CeIV(NO3)3]+, the first example of a well-characterized inner-sphere complex to be formed in cerium(IV)-mediated water oxidation. The identification of this reactive FeIV–O–CeIV adduct may open new pathways to validate mechanistic notions of an analogous MnV–O–CaII unit in the oxygen evolving complex that is responsible for carrying out the key O–O bond forming step.
Suggested Citation
Zoel Codolà & Laura Gómez & Scott T. Kleespies & Lawrence Que Jr & Miquel Costas & Julio Lloret-Fillol, 2015.
"Evidence for an oxygen evolving iron–oxo–cerium intermediate in iron-catalysed water oxidation,"
Nature Communications, Nature, vol. 6(1), pages 1-10, May.
Handle:
RePEc:nat:natcom:v:6:y:2015:i:1:d:10.1038_ncomms6865
DOI: 10.1038/ncomms6865
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