Abstract
We study the mechanism of orbital-order melting observed at temperature in the series of rare-earth manganites. We find that the purely electronic many-body super-exchange mechanism yields a transition temperature that decreases with decreasing rare-earth radius and increases with pressure, opposite to the experimental . We show that the tetragonal crystal-field splitting reduces further increasing the discrepancies with experiments. This proves that super-exchange effects, although very efficient, in the light of experimentally observed trends play a minor role for the melting of orbital ordering in rare-earth manganites.
- Received 4 November 2011
DOI:https://doi.org/10.1103/PhysRevB.85.035124
©2012 American Physical Society