Abstract
High pressure effects on the crystal structure and magnetic state of manganite up to 31 and have been studied by means of the x-ray and neutron powder diffraction, respectively. At ambient pressure, has a tetragonal crystal structure (space group ) and exhibits a ferromagnetic state below . The lattice compression at ambient temperature is anisotropic at with the most compressible axis and it becomes isotropic with nearly equal compressibilities of and axes at higher pressures. At , an -type antiferromagnetic ground state is stabilized in instead of the ferromagnetic one. Its onset is accompanied by the structural transformation from the tetragonal structure of symmetry to the orthorhombic structure of symmetry. The role of orbital polarization in the pressure-induced structural and magnetic response of is discussed. The observed high pressure effects are compared with chemical substitution effects in compounds with .
- Received 22 March 2007
DOI:https://doi.org/10.1103/PhysRevB.76.094408
©2007 American Physical Society