4.6 Article

First-Principles Fe L2,3-Edge and O K-Edge XANES and XMCD Spectra for Iron Oxides

Journal

JOURNAL OF PHYSICAL CHEMISTRY A
Volume 121, Issue 40, Pages 7613-7618

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acs.jpca.7b08392

Keywords

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Funding

  1. U.S. Department of Energy (DOE), Office of Science, Office of Basic Energy Sciences (OBES), Division of Chemical Sciences, Geosciences and Biosciences, through its Geosciences program at Pacific Northwest National Laboratory (PNNL)
  2. DOE's Office of Biological and Environmental Research at PNNL
  3. Office of Science, OBES of the DOE [DE-AC02-05CH11231]

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X-ray absorption near-edge structure (XANES) and X-ray magnetic circular dichroism (XMCD) spectroscopies are tools in widespread use for providing detailed local atomic structure, oxidation state, and magnetic structure information for materials and organometallic complexes. The analysis of these spectra for transition-metal L-edges is routinely performed on the basis of ligand-field multiplet theory because one-and two particle mean-field ab initio methods typically cannot describe the multiplet structure. Here we show that multireference configuration interaction (MRCI), calculations can satisfactorily reproduce measured XANES spectra for a range of complex iron oxide materials including hematite and magnetite. MRCI Fe L-2,L-3- edge XANES and XMCD spectra of Fe(II)O-6, Pe(III)O-6, and Fe(III)O-4 in magnetite are found to, be in very good qualitative agreement with experiment and multiplet calculations. Point charge embedding and Small distortions of the first-shell oxygen ligands have only small effects. Oxygen K-edge XANES/XMCD spectra for magnetite investigated by a reahspace Green's function approach complete the, very good qualitative agreement with experiment. Material-specific differences in local coordination and site symmetry are well reproduced, making the approach useful for assigning spectral features to specific oxidation states and coordination environments:

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