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Bi doped lanthanum manganites with the chemical composition of La0.67−xBixCa0.33MnO3 (x=0x=0, 0.05, 0.1, 0.2) were prepared by the standard solid-state process. The Curie temperatures were measured to be 267 K for x=0x=0, 248 K for x=0.05x=0.05, 244 K for x=0.1x=0.1 and 229 K for x=0.2x=0.2 samples. It was found that the maximum value of the magnetic entropy change ∣ΔSm∣ has reached the highest value of 6.08 J/kg K at 3 T for the composition with x=0.05x=0.05. Nearly the same maximum entropy change was observed for the x=0x=0 sample. A large decrease in the magnitude of the entropy change was observed for the x=0.2x=0.2 sample.  相似文献   

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The crystal structure and magnetocaloric effect of Gd5SixSn4−x   (with x=2.4x=2.4, 2.6 and 2.8) alloys were studied by means of X-ray power diffraction (XRD) and magnetic measurements. From the XRD results, these alloys adopt a Gd5Si4-type structure for x=2.8x=2.8, Gd5Si4-type and Gd5Si2Ge2-type mixed structures for x=2.4x=2.4 and 2.6, while some minor phases can also be found. The Curie temperatures of the Gd5SixSn4−x increases gradually when x increases from 276 K for x=2.4x=2.4, to 301.5 K for x=2.8x=2.8. Magnetic entropy changes of these alloys at a magnetic field change of 0–1.8 T are 1.88, 2.26 and 1.69 J/kg K for x=2.4x=2.4, 2.6 and 2.8, respectively. The temperature-dependent XRD analysis shows that there is no crystallographic transition for these alloys, which can explain their low magnetic entropy changes.  相似文献   

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FCC (Fe55Ni45)1−xCx   supersaturated solid solution was prepared in a wide concentration range (0?x?0.9)(0?x?0.9) by mechanical alloying of nanocrystalline Fe55Ni45 with graphite. The lattice constant of Fe55Ni45 increases linearly with increasing carbon content up to x=0.25x=0.25. At the same time, it is found that the magnetic moment per metal atom (Fe, Ni) decreases linearly with increasing carbon content for 0?x?0.250?x?0.25 with a slope of 1.2 μB/at. For high carbon content, x?0.5x?0.5, it is observed that the decrease of lattice constant and increase of moment per metal atom (Fe, Ni) with increasing C content, indicates that the dissolution of carbon is hindered by the high-volume fraction of graphite in the initial powder mixture. The complete amorphization of x=0.5x=0.5 does not occur after the extended ball milling. The alloying effect of carbon on the magnetization is compared with other metalloid B, P, and Si in Fe- and Ni-based binary system.  相似文献   

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We have studied the anisotropic two-dimensional nearest-neighbor Ising model with competitive interactions in both uniform longitudinal field HH and transverse magnetic field ΩΩ. Using the effective-field theory (EFT) with correlation in cluster with N=1N=1 spin we calculate the thermodynamic properties as a function of temperature with values HH and ΩΩ fixed. The model consists of ferromagnetic interaction JxJx in the xx direction and antiferromagnetic interaction JyJy in the yy direction, and it is found that for H/Jy∈[0,2]H/Jy[0,2] the system exhibits a second-order phase transition. The thermodynamic properties are obtained for the particular case of λ=Jx/Jy=1λ=Jx/Jy=1 (isotropic square lattice).  相似文献   

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Magnetic and optical properties of FexCo3−xO4 thin films grown by sol–gel method have been investigated as the Fe composition (x  ) increases from 0 to 2. X-ray diffraction measurements revealed that the normal- and inverse-spinel phases coexist for 0.76?x?0.930.76?x?0.93. The normal-spinel phase is dominant below x=0.76x=0.76 while the inverse-spinel phase above x=0.93x=0.93. The lattice constant of the inverse-spinel phase is found to be larger than that of the normal-spinel phase. For both phases the lattice constant increases with increasing x. The FexCo3−xO4 films containing the inverse-spinel phase exhibit net magnetization that increases with increasing x  . Conversion electron Mössbauer spectrum measured on the x=0.93x=0.93 sample showed that Fe2+ ions prefer the octahedral sites, indicating the formation of the inverse-spinel phase. Analysis on the measured optical absorption spectra for the samples by spectroscopic ellipsometry indicates a dominance of the normal-spinel phase for low x in which Fe3+ ions mostly occupy the octahedral sites. Observation of a crystal-field transition at 1.6 eV originating from tetrahedral Fe3+ ion confirms the existence of the inverse-spinel phase for high x.  相似文献   

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