Abstract
- and -NMR spectra demonstrate that the ground state of the -site-ordered perovskite manganite is a spatial mixture of the ferromagnetic and antiferromagnetic regions, which are assigned to the metallic and the insulating charge ordered state, respectively. This exotic coexisting state appears below 200 K via a first-order-like formation of the antiferromagnetic charge ordered state inside the ferromagnetic metal one. The Mn spin-spin relaxation rate indicates that the ferromagnetic region coexisting with the antiferromagnetic one in is identical to the bulk ferromagnetic metal phase of the disordered form in spite of the absence of -site disorder. This suggests a mesoscopic rather than nanoscopic nature of the ferromagnetic region in .
- Received 4 August 2005
DOI:https://doi.org/10.1103/PhysRevLett.96.037202
©2006 American Physical Society