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  • 1
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 73 (1993), S. 6731-6733 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: Chemical analysis and x-ray diffraction measurements of samples during the reaction of cobalt treatment were carried out to study the mechanism of reaction. X-ray diffraction, TEM observation, and magnetic measurements of core γ-Fe2O3 and the modified particles were performed to investigate the crystal growth of cobalt ferrite on core γ-Fe2O3 particles. From chemical analysis of Fe2+ and total-iron ions in the reacting suspension and x-ray diffraction measurements of samples during the reaction, it is clear that the lattice constant becomes larger due to the formation of cobalt ferrite on core γ-Fe2O3 without decrement of Fe2+/total-iron ratio. So, cobalt ferrite on core γ-Fe2O3 particles is formed not by the oxidation of added Fe2+ ions, but by the electron transfer from Fe(OH)2 to core material. From x-ray diffraction measurements, I400/I311, I220/I311, and I111/I311 were calculated. While I400/I311 and I220/I311 are almost constant, only I111/I311 increases with increasing the amount of cobalt and ferrous ions added. These results show that cobalt ferrite is preferentially grown on (111) plane which is the close-packed plane of spinel lattice.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 75 (1994), S. 5559-5561 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: Modification with magnetite on Ba-ferrite particles was carried out by heating alkaline suspension including Ba-ferrite particles and Fe2+ hydroxides as described by Kiyama et al. [J. Solid State Chem. 99, 329 (1992)] to get higher magnetization. As a result of x-ray powder diffraction measurements, reflection intensity of magnetoplumbite phase decreases and that of spinel phase increases with increase of Fe2+ quantity added, simultaneously. Coercive force goes down and magnetization increases as Fe2+ quantity added increases. The differential hysteresis loop of the mixed samples (Ba-ferrite particles and magnetite particles) has two peaks. And that of the modified samples has only one peak. From these results, it becomes clear that there exists strong magnetic interaction between Ba-ferrite core and magnetite shell. The measurements of temperature dependence of magnetization at the applied field of about 16.5 kA/m shows that the Hopkinson peak shifts toward higher temperature with increase of the modified amount. It also indicates the strong magnetic interaction between core and shell materials.
    Type of Medium: Electronic Resource
    Library Location Call Number Volume/Issue/Year Availability
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