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Tsai, T.M.; Yang, K.C.; Shen, P., E-mail: pshen@mail.nsysu.edu.tw2004
AbstractAbstract
[en] MgO and Co1-xO powders in 9:1 and 1:9 molar ratio (denoted as M9C1 and M1C9, respectively) were sintered and homogenized at 1600 deg. C followed by annealing at 850 deg. C and 800 deg. C, respectively to form defect clusters and precipitates. Analytical electron microscopic observations indicated the protoxide remained as rock salt structure with complicated planar diffraction contrast for M9C1 sample, however with spinel paracrystal precipitated from the M1C9 sample due to the assembly of charge- and volume-compensating defects of the 4:1 type, i.e., four octahedral vacant sites surrounding one Co3+-filled tetrahedral interstitial site. The spacing of such defect clusters is 4.5 times the lattice spacing of the average spinel structure of Mg-doped Co3-δO4, indicating a higher defect cluster concentration than undoped Co3-δO4. The {111} faulting of Mg-doped Co3-δO4/Co1-xO in the annealed M1C9 sample implies the possible presence of zinc blend-type defect clusters with cation vacancies assembled along oxygen close packed (111) plane
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S0022459604002865; Copyright (c) 2004 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.; Country of input: International Atomic Energy Agency (IAEA)
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Journal Article
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ALKALINE EARTH METAL COMPOUNDS, CHALCOGENIDES, CHARGED PARTICLES, CHEMICAL REACTIONS, COBALT COMPOUNDS, COHERENT SCATTERING, CRYSTAL DEFECTS, CRYSTAL STRUCTURE, DISPERSIONS, ELEMENTS, HEAT TREATMENTS, HOMOGENEOUS MIXTURES, IONS, MAGNESIUM COMPOUNDS, METALS, MICROSCOPY, MINERALS, MIXTURES, NONMETALS, OXIDE MINERALS, OXIDES, OXYGEN COMPOUNDS, POINT DEFECTS, SCATTERING, SEPARATION PROCESSES, SOLUTIONS, TRANSITION ELEMENT COMPOUNDS
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