Abstract
We systematically investigate the effect of the oxygen isotope in which shows a crossover with from ferromagnetic metal to the insulator with spin-state transition. A striking feature is that effect of oxygen isotope on the ferromagnetic transition is negligible in the metallic phase, while replacing with leads to a giant up shift of the spin-state transition temperature in the insulating phase, especially shifts from 36 to with isotope component for the sample with . A metal-insulator transition is induced by oxygen isotope exchange in the sample being close to the insulating phase. The contrasting behaviors observed in the two phases can be well explained by occurrence of static Jahn-Teller distortions in the insulating phase, while the absence of them in the metallic phase.
- Received 6 July 2006
DOI:https://doi.org/10.1103/PhysRevB.74.165113
©2006 American Physical Society