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Structure, magnetic properties and Mössbauer spectra of La0.67Sr0.33FexMn1 − xO3 manganites oxide prepared by mechanical ball milling method

机译:机械球磨法制备La0.67 Sr0.33 Fex Mn1-x O3 锰氧化物的结构,磁性和Mössbauer谱

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La0.67Sr0.33FexMn1-xO3, with x = 0.0, 0.1, 0.2 and 1 have been elaborated by mechanical system. X-ray diffraction, Scanning electron microscopy, Magnetic measurements and Mössbauer spectroscopy for the systems have been investigated. Rietveld analysis of the X-ray powder diffraction show that the samples crystallise in the orthorhombic perovskite system with Pnma space group. The average particle size of about 60 nanometre was obtained from scanning electron microscopy and X-ray diffraction. The investigated samples exhibit a ferromagnetic to paramagnetic transition with increasing temperature. The presence of manganese in the structure leads to an increase of the Curie temperature as well as to spontaneous magnetization. The magnetization versus applied magnetic field shows a small coercive field and an unsaturated magnetization which indicates that the nanoparticles of all samples are superparamagnetic at around room temperature. Room temperature Mössbauer spectra show that the samples with x = 0.1 and x = 1.0 contain minority α-Fe2O3 and other spinel ferrite species. Also, they indicate that Fe3 + ions are present in slightly distorted octahedral sites in the samples with x = 0.1 and 0.2, while mixed Fe valency was observed for the sample with x = 1.0.
机译:通过机械系统对La0.67 Sr0.33 Fex Mn1-x O3 进行了阐述。对系统的X射线衍射,扫描电子显微镜,磁测量和Mössbauer光谱进行了研究。 X射线粉末衍射的Rietveld分析表明,样品在具有Pnma空间群的正交晶钙钛矿体系中结晶。通过扫描电子显微镜和X射线衍射获得约60纳米的平均粒度。研究的样品随着温度的升高呈现出铁磁到顺磁的转变。结构中锰的存在导致居里温度的升高以及自发磁化。磁化强度与施加磁场的关系显示出小的矫顽场和不饱和磁化强度,这表明所有样品的纳米粒子在室温附近都是超顺磁性的。室温Mössbauer光谱表明,x = 0.1和x = 1.0的样品中含有少数α-Fe2 O3 和其他尖晶石铁素体。同样,它们表明在x = 0.1和0.2的样品中,Fe3 +离子存在于稍微扭曲的八面体位置,而x = 1.0的样品中观察到混合的Fe价。

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