Effect of oxygen isotope substitution and crystal micro-structure on magnetic ordering and phase separation in {}
arXiv:cond-mat/0701244 · doi:10.1103/PhysRevB.75.054410
Abstract
The crystal and magnetic structures of the specified CMR manganite system have been studied as a function of across the metal-insulator (MI) transition, and of the oxygen mass (O, O). We quantitatively show how the polaronic narrowing of the carrier bandwidth and the crystal lattice micro-strains control the volume fractions of the mesoscopic ferro- and antiferromagnetic clusters. A well-defined dip in the transition temperatures and the suppression of all the types of long range ordering seen near the MI-transition at indicate a key role of the quenched disorder for the formation of the long-scale phase separated state.
21 pages (REVTeX preprint), 1 Table, 13 Figures, accepted in PRB
References in corpus (4)
- Relevance of Cooperative Lattice Effects and Correlated Disorder in Phase-Separation Theories for CMR Manganites
- Orbital domain state and finite size scaling in ferromagnetic insulating manganites
- Crystal and magnetic structure of LaCaMnO compound $(0.11\leq x\leq 0.175
- Structural and magnetic ordering in Pr0.65(CaySr1-y)0.35MnO3: "quantum critical point" versus phase segregation scenarios
Cited by in corpus (3)
- Correlation Between Phase Competition and the Nucleation of a Griffiths Phase in (La1-yPry)0.7Ca0.3Mn16/18O3
- Effect of Sr doping on the magnetic exchange interactions in manganites
- Evidence for strong effect of quenched correlated disorder on phase separation and magnetism in (La_{1-y}Pr_{y})_{0.7}Ca_{0.3}MnO_3