We have investigated the electronic structure of polycrystalline
Ca2FeReO6 using photoemission spectroscopy and band-structure
calculations within the local-density approximation+U (LDA+U) scheme. In
valence-band photoemission spectra, a double-peak structure which is
characteristic of the metallic double perovskite series has been observed near
the Fermi level (EF), although it is less distinct compared to the
Sr2FeMoO6 case. The leading near-EF structure has a very weak
spectral weight at EF above the metal-insulator transition (MIT)
temperature TMI of ∼140 K, and it loses the EF weight
below TMI, forming a small energy gap.
To reproduce this small energy gap in the calculation, we require a very
large effective U (Ueff) for Re (4 eV) in addition to a relatively
large Ueff for Fe (4 eV). Although the most of the experimental
features can be interpreted with the help of the band theory, the overall
agreement between the theory and the experiment was not satisfactory. We
demonstrate that the effective transfer integral between Fe and Re is actually
smaller than that between Fe and Mo in Ca2FeMoO6, which can explain both
MIT and very high ferrimagnetic transition temperature.Comment: 7 pages text, 5 figures, to be pulished in Phys. Rev.