Abstract
Conductivity data for () show a first-order transition from an orbital- or charge-ordered insulator to a metal as the temperature falls below . The change in conductivity is 100 times larger than that seen previously in any single-phase manganite in zero field. The metallic low-temperature state is similar to , but shows no evidence of orbital or charge order. This result supports a conclusion that strongly coupled magnetic-conductive transitions are first order.
- Received 29 November 2005
DOI:https://doi.org/10.1103/PhysRevLett.96.087201
©2006 American Physical Society