A crystal and magnetic structure of manganites Pr0.7Ca0.3Mn1−y Fe y O3 (y = 0, 0.1) has been studied by means of powder neutron diffraction at pressures up to 4 GPa in the temperature range 15-300 K. Under high pressure, an appearance of A-type antiferromagnetic state in both systems was observed. Both compounds exhibit anisotropic compression of the lattice which leads to the apical compression of MnO6 octahedra along the crystallographic b-axis. The calculated from obtained structural data pressure dependence of the charge-carrier bandwidth is in a qualitative agreement with observed pressure behavior of insulator-metal transition temperature within the framework of the double-exchange model.
Structural study of pressure-induced magnetic phase transitions in manganites Pr0.7Ca0.3Mn1-yFeyO3 (y?=?0, 0.1)
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