Physical properties of Sr2FeIrO6 and Sr1.2La0.8FeIrO6 double perovskites obtained by a new synthesis route
Creators
- 1. Instituto de Física, Universidade Federal de Goiás, 74001-970, Goiânia, GO (Brazil)
- 2. Instituto de Física "Gleb Wataghin", UNICAMP, 13083-859, Campinas, SP (Brazil)
- 3. Centro Brasileiro de Pesquisas Físicas, Rua Dr. Xavier Sigaud 150, 22290-180, Rio de Janeiro, RJ (Brazil)
Description
Previous works on Sr2-xLaxFeIrO6 double perovskite (DP) series reported a possible ferromagnetic transition at T ∼ 700 K for the x = 0.8 concentration, for which was observed the presence of spurious Fe2O3 phase. In order to prevent the formation of this impurity phase and check if this high temperature magnetic transition is intrinsic of the material, different synthesis routes became necessary. In this work, polycrystalline samples of Sr2-xLaxFeIrO6 (x = 0.0 and 0.8) have been synthesized by solid state reaction using a new heating treatment. The sample's properties were investigated by synchrotron x-ray powder diffraction (SXRD), transmission electron microscopy (TEM), magnetic susceptibility, specific heat and electrical resistivity, and compared with the previously reported results. The SXRD data revealed a structural transition induced by La to Sr substitution (I2/m↔P21/n). Moreover, it was not detected the presence of Fe2O3 on the samples obtained by the new route, which might be related to the absence of high temperature magnetic ordering. The magnetometry results indicated the emergence of Ir4+ with La doping, being corroborated by specific heat measurements which suggest Fe3+/Ir5+ and Fe3+/Ir4+ configurations for x = 0.0 and 0.8 compounds, respectively. Temperature dependent electrical resistivity measurements showed that Sr2+ to La3+ substitution leads to a decrease of electrical resistivity, possibly associated with the increase in the number of Ir valence electrons. - • Sr2−xLaxFeIrO6 (x = 0.0 and 0.8) samples were synthesized using a new heating route. • La3+ to Sr2+ substitution induces the structural transition from I2/m → P21/n. • The high temperature magnetic transition previously reported for x = 0.8 is probably due to impurity. • Fe3+–Ir5+ to Fe3+–Ir4+ valence configuration changes govern the physical properties.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.matchemphys.2016.07.057Additional details
Identifiers
- DOI
- 10.1016/j.matchemphys.2016.07.057;
- PII
- S0254-0584(16)30577-6;
Publishing Information
- Journal Title
- Materials Chemistry and Physics
- Journal Volume
- 182
- Journal Page Range
- p. 459-465
- ISSN
- 0254-0584
- CODEN
- MCHPDR
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 48073533
- Subject category
- S75: CONDENSED MATTER PHYSICS, SUPERCONDUCTIVITY AND SUPERFLUIDITY;
- Descriptors DEI
- CONCENTRATION RATIO; ELECTRIC CONDUCTIVITY; HEAT TREATMENTS; IMPURITIES; IRIDIUM COMPOUNDS; IRON COMPOUNDS; LANTHANUM COMPOUNDS; MAGNETIC SUSCEPTIBILITY; MAGNETIZATION; MONOCLINIC LATTICES; OXIDES; PEROVSKITE; POLYCRYSTALS; SOLIDS; SPECIFIC HEAT; STRONTIUM COMPOUNDS; SYNTHESIS; TEMPERATURE DEPENDENCE; TRANSMISSION ELECTRON MICROSCOPY; X-RAY DIFFRACTION
- Descriptors DEC
- ALKALINE EARTH METAL COMPOUNDS; CHALCOGENIDES; COHERENT SCATTERING; CRYSTAL LATTICES; CRYSTAL STRUCTURE; CRYSTALS; DIFFRACTION; DIMENSIONLESS NUMBERS; ELECTRICAL PROPERTIES; ELECTRON MICROSCOPY; MAGNETIC PROPERTIES; MICROSCOPY; MINERALS; OXIDE MINERALS; OXYGEN COMPOUNDS; PEROVSKITES; PHYSICAL PROPERTIES; RARE EARTH COMPOUNDS; REFRACTORY METAL COMPOUNDS; SCATTERING; THERMODYNAMIC PROPERTIES; THREE-DIMENSIONAL LATTICES; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2016 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.