Abstract
We have studied the bandwidth–temperature–magnetic-field phase diagram of colossal magnetoresistance manganites with ferromagnetic metal (FM) ground state. The bandwidth was controlled both via chemical substitution and hydrostatic pressure with a focus on the vicinity of the critical pressure where the character of the zero-field FM transition changes from first to second order. Below the first-order FM transition extends up to a critical magnetic field. It approaches zero on the larger bandwidth side where the surface of the first-order FM phase boundary is terminated by a multicritical end point. The change in the character of the transition and the decrease of the colossal magnetoresistance effect is attributed to the reduced charge-order and orbital-order fluctuations.
- Received 30 November 2007
DOI:https://doi.org/10.1103/PhysRevLett.101.037206
©2008 American Physical Society