Fe(I)-mediated reductive cleavage and coupling of CO2: An FeII(μ-O,μ-CO)FeII core

Connie C. Lu; Caroline T. Saouma; Michael W. Day; Jonas C. Peters

doi:10.1021/ja065524z

Fe(I)-mediated reductive cleavage and coupling of CO₂: An Fe^II(μ-O,μ-CO)Fe^II core

Connie C. Lu, Caroline T. Saouma, Michael W. Day, Jonas C. Peters

Chemistry (Twin Cities)

Research output: Contribution to journal › Article › peer-review

141 Scopus citations

Abstract

THF solutions of a new iron(I) source, [PhBP^CH₂^Cy₃]Fe ([PhBP^CH₂Cy₃] = [PhBP(CH₂P(CH₂Cy)₂)₃]-), effect the reductive cleavage of CO₂ via O-atom transfer at ambient temperature. The dominant reaction pathway is bimetallic and leads to the formation of a structurally unprecedented diiron Fe^II(μ-O)(μ-CO)Fe^II core. X-ray data are also available to suggest that bimetallic reductive CO_2M coupling to generate oxalate occurs as a minor reaction pathway. These initial observations forecast a diverse reaction landscape between CO₂ and iron(I) synthons.

Original language	English (US)
Pages (from-to)	4-5
Number of pages	2
Journal	Journal of the American Chemical Society
Volume	129
Issue number	1
DOIs	https://doi.org/10.1021/ja065524z
State	Published - Jan 10 2007

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title = "Fe(I)-mediated reductive cleavage and coupling of CO2: An FeII(μ-O,μ-CO)FeII core",

abstract = "THF solutions of a new iron(I) source, [PhBPCH2Cy3]Fe ([PhBPCH2Cy3] = [PhBP(CH2P(CH2Cy)2)3]-), effect the reductive cleavage of CO2 via O-atom transfer at ambient temperature. The dominant reaction pathway is bimetallic and leads to the formation of a structurally unprecedented diiron FeII(μ-O)(μ-CO)FeII core. X-ray data are also available to suggest that bimetallic reductive CO2M coupling to generate oxalate occurs as a minor reaction pathway. These initial observations forecast a diverse reaction landscape between CO2 and iron(I) synthons.",

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AU - Saouma, Caroline T.

AU - Day, Michael W.

AU - Peters, Jonas C.

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N2 - THF solutions of a new iron(I) source, [PhBPCH2Cy3]Fe ([PhBPCH2Cy3] = [PhBP(CH2P(CH2Cy)2)3]-), effect the reductive cleavage of CO2 via O-atom transfer at ambient temperature. The dominant reaction pathway is bimetallic and leads to the formation of a structurally unprecedented diiron FeII(μ-O)(μ-CO)FeII core. X-ray data are also available to suggest that bimetallic reductive CO2M coupling to generate oxalate occurs as a minor reaction pathway. These initial observations forecast a diverse reaction landscape between CO2 and iron(I) synthons.

AB - THF solutions of a new iron(I) source, [PhBPCH2Cy3]Fe ([PhBPCH2Cy3] = [PhBP(CH2P(CH2Cy)2)3]-), effect the reductive cleavage of CO2 via O-atom transfer at ambient temperature. The dominant reaction pathway is bimetallic and leads to the formation of a structurally unprecedented diiron FeII(μ-O)(μ-CO)FeII core. X-ray data are also available to suggest that bimetallic reductive CO2M coupling to generate oxalate occurs as a minor reaction pathway. These initial observations forecast a diverse reaction landscape between CO2 and iron(I) synthons.

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Fe(I)-mediated reductive cleavage and coupling of CO₂: An Fe^II(μ-O,μ-CO)Fe^II core

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