Abstract
The electronic structure of the series of perovskites is examined with the aid of density-functional calculations. A range of possible crystal structures is examined for each compound, and in each case the calculated lowest-energy structure is that observed at low temperature. The factors that control the variation in structure with the alkaline-earth ion are discussed. consists of corner-sharing octahedra but is orthorhombically distorted consistent with being too small for the 12-fold site within a perfect cubic polyhedral framework. When the size of the alkaline-earth cation increases, a transformation from corner-sharing to face-sharing octahedra is induced since the alkaline-earth cation now becomes too large for the 12-fold site. While at has the four-layered hexagonal () structure with corner-sharing dimers, at adopts the two-layered hexagonal structure with infinite chains of face-sharing octahedra. The Mn charge is much lower than the conventional ionic model charge due to Mn-O covalence, and this reduces the Mn-Mn repulsion and favors sharing of the octahedral faces. We see no evidence for direct Mn-Mn metal bonding which has often been invoked to rationalize the adoption of this type of structure. We also discuss the atomistic origins of acid-base stabilization of ternary oxides from their binary constituents. A link between cation size and acid-base properties is suggested for .
2 More- Received 20 December 2006
DOI:https://doi.org/10.1103/PhysRevB.75.184105
©2007 American Physical Society