paper

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

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