posted on 2013-11-08, 00:00authored byRobert Klie, Peter Zapol, Serdar Öğüt, Alejandro Rébola
The atomic and electronic structures of the misfit-layered thermoelectric oxide material Ca3Co4O9 are
investigated using detailed first-principles computations performed within the framework of density functional
theory (DFT) and its DFT+U extension to account for electron correlations. The structure of Ca3Co4O9,
composed of two incommensurate subsystems—a distorted rocksalt-type Ca2CoO3 layer sandwiched between
hexagonal CoO2 layers—is modeled by means of Fibonacci rational approximants with systematically increasing
unit cells.We show that good agreement with photoemission and transport experiments can be obtained regarding
the contribution of the two subsystems to states near the Fermi level, when electron correlations are taken into
account with a Hubbard U. The size of the rational approximant plays a secondary role in the analysis; the
relatively “small” structure of composition (Ca2CoO3)6(CoO2)10 represents a good model for investigating the
atomic and electronic properties of Ca3Co4O9. Within the DFT+U formalism, the metallic conductivity of
Ca3Co4O9 is shown to result from itinerant holes in the hexagonal CoO2 layers, in which the Co atoms are
predicted to have a mixed valence of Co4+ with ∼30% concentration and Co3+ with ∼70% concentration, both
in low-spin configurations. In most cases, the resulting electronic structures show very good agreement with
available data from transport and magnetic measurements.
Funding
We acknowledge support for this work by the National
Science Foundation under Grant No. DMR-0846746 (R.F.K.)
and partial support by the Department of Energy under
Grant No. DE-FG02-09ER16072 (A.R.). P.Z. acknowledges
support from the US Department of Energy BES-Materials
Sciences under Contract No. DE-AC0206CH11357. S. O¨ .
acknowledges support by the National Science Foundation
under the Independent Research/Development program while
working at the Foundation. This research used resources of
NERSC, which is supported by the Office of Science of the
US Department of Energy.
1A. Ohtomo,