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On the Sr_1-xBa_xFeO₂F Oxyfluoride Perovskites: Structure and Magnetism from Neutron Diffraction and Mossbauer Spectroscopy.

ABSTRACT: Four oxyfluorides of the title series (x = 0.00, 0.25, 0.50, 0.75) have been stabilized by topotactic treatment of perovskite precursors Sr_1-xBa_xFeO_3-δ prepared by soft-chemistry procedures, yielding reactive materials that can easily incorporate a substantial amount of F atoms at moderate temperatures, thus avoiding the stabilization of competitive SrF₂ and BaF₂ parasitic phases. XRD and Neutron Powder Diffraction (NPD) measurements assess the phase purity and yield distinct features concerning the unit cell parameters' variation, the Sr and Ba distribution, the stoichiometry of the anionic sublattice and the anisotropic displacement factors for O and F atoms. The four oxyfluorides are confirmed to be cubic in all of the compositional range, the unit cell parameters displaying Vergard's law. All of the samples are magnetically ordered above room temperature; the magnetic structure is always G-type antiferromagnetic, as shown from NPD data. The ordered magnetic moments are substantially high, around 3.5 μ_B, even at room temperature (RT). Temperature-dependent Mössbauer data allow identifying Fe³⁺ in all of the samples, thus confirming the Sr_1-xBa_xFeO₂F stoichiometry. The fit of the magnetic hyperfine field vs. temperature curve yields magnetic ordering T_N temperatures between 740 K (x = 0.00) and 683 K (x = 0.75). These temperatures are substantially higher than those reported before for some of the samples, assessing for stronger Fe-Fe superexchange interactions for these specimens prepared by fluorination of citrate precursors in mild conditions.

SUBMITTER: Garcia-Ramos CA

PROVIDER: S-EPMC5456977 | biostudies-literature |

REPOSITORIES: biostudies-literature

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Project description:We report high-pressure neutron powder diffraction measurements of the most hydrated phase in the MgSO4–H2O system, magnesium sulfate undecahydrate, including an analysis of the elastic strain tensor and observations concerning phase changes that occur at high pressure. We have collected neutron powder diffraction data from MgSO4·11D2O (the deuterated analogue of meridianiite), a highly hydrated sulfate salt that is thought to be a candidate rock-forming mineral in some icy satellites of the outer solar system. Our measurements, made using the PEARL/HiPr and OSIRIS instruments at the ISIS neutron spallation source, covered the range 0.1 < P < 800?MPa and 150 < T < 280?K. The refined unit-cell volumes as a function of P and T are parameterized in the form of a Murnaghan integrated linear equation of state having a zero-pressure volume V0 = 706.23?(8)?Å3, zero-pressure bulk modulus K0 = 19.9?(4)?GPa and its first pressure derivative, K? = 9?(1). The structure’s compressibility is highly anisotropic, as expected, with the three principal directions of the unit-strain tensor having compressibilities of 9.6?×?10?3, 3.4?×?10?2 and 3.4?×?10?3 GPa?1, the most compressible direction being perpendicular to the long axis of a discrete hexadecameric water cluster, (D2O)16. At high pressure we observed two different phase transitions. First, warming of MgSO4·11D2O at 545?MPa resulted in a change in the diffraction pattern at 275?K consistent with partial (peritectic) melting; quasielastic neutron spectra collected simultaneously evince the onset of the reorientational motion of D2O molecules with characteristic time-scales of 20–30?ps, longer than those found in bulk liquid water at the same temperature and commensurate with the lifetime of solvent-separated ion pairs in aqueous MgSO4. Second, at ??0.9?GPa, 240?K, MgSO4·11D2O decomposed into high-pressure water ice phase VI and MgSO4·9D2O, a recently discovered phase that has hitherto only been formed at ambient pressure by quenching small droplets of MgSO4(aq) in liquid nitrogen. The fate of the high-pressure enneahydrate on further compression and warming is not clear from the neutron diffraction data, but its occurrence indicates that it may also be a rock-forming mineral in the deep mantles of large icy satellites.

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On the Sr_1-xBa_xFeO₂F Oxyfluoride Perovskites: Structure and Magnetism from Neutron Diffraction and Mossbauer Spectroscopy.

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On the Sr_1-xBa_xFeO₂F Oxyfluoride Perovskites: Structure and Magnetism from Neutron Diffraction and Mossbauer Spectroscopy.