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Journal of Solid State Chemistry; v. 4(3); p. 357-361
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[en] A new sodium and calcium iron phosphate, NaCaFe3(PO4)4, has been synthesized by a flux method and characterized by single crystal X-ray diffraction, magnetic susceptibility and Moessbauer spectroscopy. The compound crystallizes in the orthorhombic space group Pcab with the parameters a=8.706(4) A, b=9.410(1) A, c=29.211(6) A, V=2393 A3 and Z=8. The structure consists of discrete FeO6 octahedra and FeO5 trigonal bipyramids, corner-sharing with PO4 tetrahedra that form a [Fe3P4O16]n three-dimensional framework with two distinct cavities which are the Na+ and Ca2+ sites. Moessbauer spectroscopy results confirm those obtained from X-ray diffraction. Magnetic susceptibility indicates an antiferromagnetic behavior with a Neel temperature TN∼26 K
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S0925838803001294; Copyright (c) 2003 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.; Country of input: International Atomic Energy Agency (IAEA)
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ALKALI METAL COMPOUNDS, ALKALINE EARTH METAL COMPOUNDS, CALCIUM COMPOUNDS, CHARGED PARTICLES, COHERENT SCATTERING, CRYSTAL LATTICES, CRYSTAL STRUCTURE, CRYSTALS, DIFFRACTION, IONS, IRON COMPOUNDS, MAGNETIC PROPERTIES, MAGNETISM, OXYGEN COMPOUNDS, PHOSPHATES, PHOSPHORUS COMPOUNDS, PHYSICAL PROPERTIES, SCATTERING, SODIUM COMPOUNDS, SYMMETRY GROUPS, TEMPERATURE RANGE, THERMODYNAMIC PROPERTIES, TRANSITION ELEMENT COMPOUNDS, TRANSITION TEMPERATURE
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Gaudin, E.; Goglio, G.; Besnard, A.; Darriet, J., E-mail: darriet@icmcb.u-bordeaux.fr
arXiv e-print [ PDF ]2003
arXiv e-print [ PDF ]2003
AbstractAbstract
[en] The compound La2Ca2MnO6(O2) has been synthesized from La2Ca2MnO7 heated at 1123 K under high pressure (4 GPa) with KClO3 as oxygen source. The crystal structure has been refined from X-ray powder data in the R3-barm space group. The unit-cell parameters are a=5.6335(2) A and c=17.4879(8) A. Perpendicular to the c-axis, the structure is built up by the periodic stacking of two close packed [LaO3] layers separated by a layer of composition [Ca2O2] containing (O2)2- peroxide ions. This oxide belongs to the family of compounds formulated as [A'2O2-δ][AnBn-1O3n] for n=2 and δ=0. It is the first member of the series where the thickness of the perovskite slab corresponds to one [BO6] (B=Mn) octahedron. The structural relationships with La2Ca2MnO7 are discussed and the magnetic properties show that in both phases manganese is tetravalent
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ACS symposium on metal oxides; Boston, MA (United States); 18-22 Aug 2002; S0022459603000434; Copyright (c) 2003 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.; Country of input: International Atomic Energy Agency (IAEA)
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CALCIUM COMPOUNDS, CHEMICAL PREPARATION, CHLORATES, CRYSTAL STRUCTURE, HEATING, HEXAGONAL LATTICES, LANTHANUM COMPOUNDS, LANTHANUM OXIDES, LAYERS, MAGNETIC PROPERTIES, MANGANATES, PEROVSKITES, PEROXIDES, POTASSIUM COMPOUNDS, PRESSURE RANGE GIGA PA, STOICHIOMETRY, TEMPERATURE RANGE 1000-4000 K, X-RAY SPECTRA
ALKALI METAL COMPOUNDS, ALKALINE EARTH METAL COMPOUNDS, CHALCOGENIDES, CHLORINE COMPOUNDS, CRYSTAL LATTICES, CRYSTAL STRUCTURE, HALOGEN COMPOUNDS, LANTHANUM COMPOUNDS, MANGANESE COMPOUNDS, MINERALS, OXIDES, OXYGEN COMPOUNDS, PHYSICAL PROPERTIES, PRESSURE RANGE, RARE EARTH COMPOUNDS, SPECTRA, SYNTHESIS, TEMPERATURE RANGE, TRANSITION ELEMENT COMPOUNDS
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[en] A new potassium iron phosphate K11Fe15(PO4)18O has been synthesized by the flux method and characterized by single-crystal X-ray diffraction. The compound crystallizes in the cubic system with the space group P213 and the cell parameter a=9.917(2) A. The unit cell contains one formula unit K7.33Fe10(PO4)12O0.66. The structure is closely related to that of the Langbeinite-like compounds, the main difference being the existence of a four-coordinated iron atom in the structure of the oxyphosphate. K11Fe15(PO4)18O adopts a complex three-dimensional network involving corner- and edge-linkage between iron polyhedra, and corner-sharing between phosphorus tetrahedra and iron polyhedra. The Moessbauer spectral parameters are consistent with the structure and reveal the presence of octahedral and tetrahedral sites for the iron(III) in the expected 4:1 ratio. The thermal variation of the magnetic susceptibility shows that the title compound is antiferromagnetic with a Neel temperature TN=6 K. At high temperature, the susceptibility follows a Curie-Weiss law with C=58.82 emu K mol-1 and θp=-88.39 K. The relationship between the structure of K11Fe15(PO4)18O and the previous reported trivalent vanadium phosphate K11V15(PO4)18O will be discussed
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S0925838803004122; Copyright (c) 2003 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.; Country of input: International Atomic Energy Agency (IAEA)
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ALKALI METAL COMPOUNDS, COHERENT SCATTERING, CRYSTAL LATTICES, CRYSTAL STRUCTURE, CRYSTALS, DIFFRACTION, IRON COMPOUNDS, MAGNETIC PROPERTIES, MAGNETISM, OXYGEN COMPOUNDS, PHOSPHATES, PHOSPHORUS COMPOUNDS, PHYSICAL PROPERTIES, SCATTERING, SYMMETRY GROUPS, THERMODYNAMIC PROPERTIES, TRANSITION ELEMENT COMPOUNDS, TRANSITION TEMPERATURE, VANADIUM COMPOUNDS
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[en] Above 8500C Cs4Ni3CdF12 (which corresponds to the x = 0.25 composition of the CsNi/sub 1-x/Cd/sub x/F3 solid solution) shows an allotropic transformation from a 12 R to a 10 H-type structure. The high temperature form crystallizes in the hexagonal P63/mmc space group with a = 6.238 A and c = 25.362 A. A crystal structure determination shows that the 10-layer packing sequence corresponds to a new structural arrangement of CsF3 layers and divalent cations. The structure is characterized by units of four octahedra linked by faces and connected to each other by an octahedron sharing only corners. Ni and Cd atoms are partially disordered in the tetrameric units, while the unique octahedron is occupied by cadmium. A phase corresponding to the Cs5Ni4CdF15 formula has been isolated, which shows an isostructural powder pattern. (author)
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Zeitschrift fuer Anorganische und Allgemeine Chemie (1950); ISSN 0044-2313; ; v. 508 p. 93-99
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ALKALI METAL COMPOUNDS, CADMIUM COMPOUNDS, CADMIUM HALIDES, CESIUM COMPOUNDS, COHERENT SCATTERING, CRYSTAL LATTICES, CRYSTAL STRUCTURE, DIFFRACTION, DISPERSIONS, DISTANCE, FLUORIDES, FLUORINE COMPOUNDS, HALIDES, HALOGEN COMPOUNDS, HOMOGENEOUS MIXTURES, MIXTURES, NICKEL COMPOUNDS, SCATTERING, SOLUTIONS, SYMMETRY GROUPS, TRANSITION ELEMENT COMPOUNDS
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[en] New ternary oxides of formulas Na5NbO5 and Na5TaO5 have been prepared. They crystallize in the monoclinic system (space group C2/c). The crystal structure of Na5NbO5 has been determined. It derives from a NaCl-type structure by ordering of the cations and of the oxygen vacancies in the anionic sublattice, the corresponding formula being Nasub(5/6)Nbsub(1/6)Osub(5/6)vacant sub(1/6). Sodium and niobium have a distorted square-pyramidal surrounding. (author)
Original Title
Les Phases Na5NbO5 et Na5TaO5
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Numerical Data
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Zeitschrift fuer Anorganische und Allgemeine Chemie (1950); ISSN 0044-2313; ; v. 485 p. 115-121
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[en] The title compounds were synthesized and subsequently studied by inelastic neutron scattering (INS). Energy splittings due to the crystalline electric field (CEF) were directly observed for the octahedral LnX63- units in the Cs2ALnX6 series. They can be rationalized in terms of crystal-field theory. In the dimer compounds Cs3Ln2Br9 (Ln3+ = Tb, Yb) the energy splitting is the result of the combined action of CEF and exchange interactions. (Auth.)
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International rare earth conference; Zurich (Switzerland); 4-8 Mar 1985
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[en] A number of new hexagonal perovskite-like oxides have been obtained by reacting La4Ti3O12 and LaTiO3. Their crystal structure is based on close-packed stacking of LaO3 layers and can also be described as consisting of blocks of corners-sharing (TiO6) octahedra perpendicular to the c-axis, separated by layers of vacant octahedra. The first phase, La5Ti4O15, corresponds to the 10H polytypoid with a (hccchhccch) sequence along the c-axis. The second phase, La6Ti5O18, corresponds to the 18R polytypoid with a (hcccch)3 stacking of the LaO3 layers. La9Ti7O27 belongs to the 54R polytipoid with a (hccchhcch)6 layers stacking. The structure consists of an alternating sequence of La5Ti4O15 and La4TiO12 blocks along the c-axis and thus can be considered as a regular intergrowth between these two phases. The main feature of these new phases is that in each structural unit one of the possible octahedral positions remains unoccupied. These results have been confirmed by refinement of powder XRD data as well as by electron microscopy (SAED, HRTEM) methods
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European Journal of Solid State and Inorganic Chemistry; ISSN 0992-4361; ; CODEN EJSCE5; v. 30(5); p. 521-537
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[en] Sodium tetracalcium pentaniobium heptadecaoxide, NaCa4Nb5O17, corresponds to the n = 5 term of the homologous AnBnO3n+2 family of structures composed of ABX3 perovskite layers. The structure consists of perovskite-type blocks of n = 5 layers of NbO6 octahedra, separated by an interblock region. Successive blocks along the b axis are displaced by 1/2c with respect to each other. The deformation of the NbO6 octahedra is a minimum at the middle of each block, and increases along the direction of the axis to a maximum at each end of the block. Ca and Na share the same intrablock sites, coordinated by 12 O atoms, whereas only Ca atoms are found in the interblock cavities, at sites with different coordination geometries. (orig.)
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Acta Crystallographica. Section C: Crystal Structure Communications; ISSN 0108-2701; ; CODEN ACSCEE; v. 59(2); p. i18-i20
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[en] The new perovskite-type phases have been isolated in the BaRuO3 -BaBiO3 system. The first one, Ba3Ru2Bi09 crystallizes with a monoclinic symmetry (C2/c S.G.) and can be considered as a slightly distorted hexagonal perovskite of the 6H polytype. The second phase corresponds to a solid solution with the general formula Ba2RuxBi2-xO6 (O< x≤0.67) and is isostructural with the monoclinic form of BaBiO3 (12/m S.G.). The main feature of these phases is that they include not only an atomic rearrangement, but also a charge transfer. In both phases, the Bi3+ cations occupy only one type of the possible independent positions and thus force a cationic ordering among the octahedral sites. These new structures have been confirmed by refinements of the X-ray powder data using the Rietveld's method. The valence state of the ruthenium has been confirmed by magnetic measurements. Resistivity measurements have shown that these compounds are semiconductors
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European Journal of Solid State and Inorganic Chemistry; CODEN EJSCE5; v. 30(3); p. 273-286
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ALKALINE EARTH METAL COMPOUNDS, BARIUM COMPOUNDS, BISMUTH COMPOUNDS, CHALCOGENIDES, CRYSTAL LATTICES, CRYSTAL STRUCTURE, DISPERSIONS, ELECTRICAL PROPERTIES, HOMOGENEOUS MIXTURES, MIXTURES, OXIDES, OXYGEN COMPOUNDS, PHASE TRANSFORMATIONS, PHYSICAL PROPERTIES, RUTHENIUM COMPOUNDS, SOLUTIONS, TRANSITION ELEMENT COMPOUNDS
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