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The Topotactic Reduction of Sr<sub>3</sub>Fe<sub>2</sub>O<sub>5</sub>Cl<sub>2</sub>—Square Planar Fe(II) in an Extended Oxyhalide
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Citations
15
References
2010
Year
Magnetic PropertiesEngineeringCorner-sharing FeChemistryOxychloride SrInorganic MaterialRedox BiologyInorganic CompoundMagnetismRedox ChemistryMaterials ScienceInorganic ChemistrySpectroelectrochemistryCatalysisExtended OxyhalideCrystallographyOxygen Reduction ReactionFerromagnetismNatural SciencesTopotactic Reduction
The topotactic reduction of the oxychloride Sr(3)Fe(2)O(5)Cl(2) with LiH results in the formation of Sr(3)Fe(2)O(4)Cl(2). Neutron powder diffraction data show that Sr(3)Fe(2)O(4)Cl(2) adopts a body-centered tetragonal crystal structure (I4/mmm, a = 4.008(1) Å, c = 22.653(1) Å at 388 K) with anion vacancies located within the SrO layer of the phase. This leads to a structure consisting of infinite sheets of corner-sharing Fe(II)O(4) square planes. Variable-temperature neutron diffraction data show that Sr(3)Fe(2)O(4)Cl(2) adopts G-type antiferromagnetic order below T(N) ∼ 378(10) K with an ordered moment of 2.81(9) μ(B) per iron center at 5 K consistent with the presence of high-spin Fe(II). The observed structural and chemical selectivity of the reduction reaction is discussed. The contrast between the structure of Sr(3)Fe(2)O(4)Cl(2) and the isoelectronic all-oxide analogue (Sr(3)Fe(2)O(5)) suggests that by careful selection of substrate phases, the topotactic reduction of complex transition metal oxychlorides can lead to the preparation of novel anion-deficient phases with unique transition metal-oxygen sublattices which cannot be prepared via the reduction of all-oxide substrates.
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