Abstract
A pressure-induced phase transition, associated with the formation of cation-cation bonding, occurs in by combining synchrotron x-ray diffraction in a diamond anvil cell and ab initio evolutionary calculations. The high-pressure phase has a monoclinic structure with a space group, and it is both energetically and dynamically stable at pressures above 47 GPa to at least 105 GPa. This phase transition can be viewed as a two-dimensional Peierls-like distortion, where the cation-cation dimer chains are connected along the axis of the monoclinic cell. This finding provides insights into the interplay of electron correlation and lattice distortion in , and it may also help to understand novel properties of other early transition-metal oxides.
- Received 9 January 2014
- Revised 17 June 2015
DOI:https://doi.org/10.1103/PhysRevB.92.134106
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