DI11C-2596
First-principles study on Jahn-Teller effect in Fe2+-bearing wadsleyite
Monday, 14 December 2015
Poster Hall (Moscone South)
Atsushi Kyono, University of Tsukuba, Tsukuba, Japan
Abstract:
Electronic structure of Fe2+-bearing wadsleyite b-(Mg,Fe2+)SiO4 has been investigated by first-principles calculations based on the density function theory. Crystal structure of wadsleyite is characterized by edge-sharing octahedra. The single chains of M1 and M2 octahedra running parallel to b-axis are cross-linked by the double columns of M3 octahedra parallel to a-axis. In the wadsleyite structure, Fe2+ cation orders preferentially into the M1 and M3 sites. Electron configuration analysis of the Fe2+ reveals that the dxy, dyz, dzx orbitals (lower energy orbital t2g) of Fe2+ are occupied by 0.430, 1.931, 1.923 electrons, while the dx2-y2 and dz2 orbitals (higher energy orbital eg) are filled with 1.809 and 0.434 electrons, respectively. The asymmetric electron occupations of the t2g and eg can lead to the Jahn-Teller distortion around the octahedrally coordinated Fe2+. The molecular orbital calculation shows that the electron orbitals in the Fe2+-bearing wadsleyite are completely localized at the Fe3d orbitals and O2p orbital in the M3 sites, which causes the repulsive interactions between the Fe3d orbitals and O2p orbital. The strong repulsion is responsible for the Jahn-Teller distortion in the structure. In contrast, little localization of electron orbitals is observable in the Fe2+-free wadsleyite. Therefore, the presence of Fe2+ appears to destabilize the wadsleyite structure. This is the reason that the stability of wadsleyite is limited to the Mg-rich portion of the (Mg,Fe)2SiO4 binary system. Since coordination polyhedra of Fe3+ exhibit no Jahn–Teller distortions, on the other hand, a continuous substitution of Fe3+ can occur in wadsleyite via a coupled substitution of 2Fe3+ = Si4+ + Fe2+ without structural change, which suggests that the Jahn–Teller effect of Fe2+ is critically important for the phase stability of wadsleyite.