Abstract
Two magnetic phase transitions have been noted for for near-stoichiometric oxygen concentrations (small ). Using muon-spin rotation and neutron scattering experiments, we have established that the two transitions represent separate, spatially distinct magnetic phases that coexist in a two-phase equilibrium mixture. The two phases most likely represent areas of the sample with different effective valence charge densities. Further, the phases exist over regions with a length scale intermediate between nanoscale charge inhomogeneity and systems such as manganites or superoxygenated cuprates with large length scale phase separations.
- Received 26 October 2015
DOI:https://doi.org/10.1103/PhysRevB.93.224412
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