Orbital-order melting in rare-earth manganites: Role of superexchange

Andreas Flesch, Guoren Zhang, Erik Koch, and Eva Pavarini
Phys. Rev. B 85, 035124 – Published 26 January 2012

Abstract

We study the mechanism of orbital-order melting observed at temperature TOO in the series of rare-earth manganites. We find that the purely electronic many-body super-exchange mechanism yields a transition temperature TKK that decreases with decreasing rare-earth radius and increases with pressure, opposite to the experimental TOO. We show that the tetragonal crystal-field splitting reduces TKK 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.

  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Received 4 November 2011

DOI:https://doi.org/10.1103/PhysRevB.85.035124

©2012 American Physical Society

Authors & Affiliations

Andreas Flesch1, Guoren Zhang1, Erik Koch2, and Eva Pavarini1,*

  • 1Institute for Advanced Simulation and JARA, Forschungszentrum Jülich, 52425 Jülich, Germany
  • 2German Research School for Simulation Sciences, 52425 Jülich, Germany

  • *e.pavarini@fz-juelich.de

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 85, Iss. 3 — 15 January 2012

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review B

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×