Abstract
We report a comprehensive high-pressure study on the triple-layer with a suite of experimental probes, including structure determination, magnetic, and transport properties up to 50 GPa. Consistent with a recent ab inito calculation, application of hydrostatic pressure suppresses an insulator-metal spin-state transition at . However, a low-spin metallic phase does not emerge after the high-spin state is suppressed to the lowest temperature. For , the ambient structure transforms gradually to a -type structure, which involves a structural reconstruction from fluorite blocks under low pressures to rock-salt LaO-LaO blocks under high pressures. Absence of the metallic phase under pressure has been discussed in terms of local displacements of ions in the fluorite block under pressure before a global phase is established.
- Received 2 February 2012
DOI:https://doi.org/10.1103/PhysRevLett.108.236403
© 2012 American Physical Society