Author:
Yamanaka Takamitsu,Hirao Naohisa,Nakamoto Yuki,Mikouchi Takashi,Hattori Takanori,Komatsu Kazuki,Mao Ho-kwang
Abstract
AbstractMagnetic and structure transitions of Mn3–xFexO4 solid solutions under extreme conditions are clarified by neutron time-of-flight scattering diffraction and X-ray Mössbauer measurement. The ferrimagnetic-to-paramagnetic transition temperature (100 °C) of Mn2FeO4 spinel is different from the tetragonal-to-cubic structure transition temperature (180 °C). The structure transition temperature decreases with increasing pressure. The transition is not coupled with the magnetic transition. Synchrotron X-ray Mössbauer experiments have revealed the pressure effects on the distribution of Fe2+ and Fe3+ at the tetrahedral and octahedral sites in the spinel structure. Ferrimagnetic MnFe2O4 and Mn2FeO4 spinels show sextet spectral features with hyperfine structure elicited by internal magnetic fields. Cubic MnFe2O4 spinel and tetragonal Mn2FeO4 transform to high-pressure orthorhombic postspinel phase above pressures of 18.4 GPa and 14.0 GPa, respectively. The transition pressure decreases with increasing Mn content. The postspinel phase has a paramagnetic property. Mn2O10 dimers of two octahedra are linked via common edge in three dimentional direction. The occupancy of Fe2+ in the tatrahedral site is decreased with increasig pressure, indicating more oredered structure. Consequently, the inverse parameter of the spinel structure is increased with increasing pressure. The magnetic structure refinements clarify the paramagnetic and ferrimagnetic structure of MnFe2O4 and Mn2FeO4 spinel as a function of pressure. The magnetic moment is ordered between A and B sites with the anti-parallel distribution along the b axis. The nuclear tetragonal structure (aN, aN, cN) has the ferrimagnetic structure but the orthorhombic magnetic structure has the ferrimagnetic structure with the lattice constants (aM, bM, cM). The magnetic moment is ordered between A and B sites with the anti-parallel distribution along the bM axis.
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,General Materials Science