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Defects characterisation and studies of structural properties of sol-gel synthesised MgFe2O4 nanocrystals through positron annihilation and supportive spectroscopic methods

机译:通过正电子湮没和支持性光谱方法缺陷溶胶 - 凝胶合成MgFe2O4纳米晶体的结构性质的表征及研究

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Magnesium ferrite (MgFe_2O_4) nanocrystalline samples were prepared by sol-gel method and by sintering at temperatures from 300°C to 1000°C. X-ray diffraction and electron microscopic studies showed an increase in crystallite sizes and a decrease in lattice constants at higher sintering temperatures. UV-Vis absorption measurements depicted blue shift for samples of smaller crystallite sizes (d_c) with a resultant increase of the band gap energies (E_g. = 2.07 eV at d_c = 49 nm to 3.10 eV at d_c = 6 nm, for samples sintered at 1000°C and 300°C, respectively). Fourier transform infrared spectroscopy of the samples proved the formation of the spinel structure while energy dispersive X-ray analysis pointed out the non-stoichiometric composition, which implied the presence of vacancy type defects that could modify the structural and magnetic characteristics of the compounds. This necessitated the use of positron annihilation lifetime and coincidence Doppler broadening spectroscopic studies for defect characterisation and the results indicated distinct redistribution of cations within the unit cells, making the compound overwhelmingly turn towards a normal spinel configuration at smaller nanocrystalline sizes. Positrons were trapped in larger vacancies of increasing numbers in smaller crystallites. The vacancies turned out to be formed at the octahedral sites where the increased ionic radius of Fe3+ became large enough to reduce the occupancy significantly. Mossbauer spectra analysis indicated an increase of the ferromagnetic properties in samples sintered at higher temperatures. At 300°C and 400°C, the samples dominantly showed paramagnetic behaviour.
机译:通过溶胶 - 凝胶法制备镁铁氧体(MgFe_2O_4)纳米晶样品,并在300℃至1000℃的温度下烧结。 X射线衍射和电子显微镜研究表明微晶尺寸的增加和较高烧结温度下的晶格常数减少。 UV-Vis吸收测量,描绘了用于较小晶体尺寸(D_c)的样品的蓝色转移,其产生的带隙能量(e_c。= 2.07eV在d_c = 49nm至3.10ev处,在d_c = 6nm处,用于样品烧结在1000°C和300°C)。傅里叶变换的样品的红外光谱证明了尖晶石结构的形成,同时能量分散X射线分析指出非化学计量组合物,其暗示存在可改变化合物的结构和磁性的空位型缺陷的存在。这需要使用正电子湮没寿命和重合多普勒拓宽的光谱研究,用于缺陷表征,结果表明单位细胞内的阳离子明显再分布,使得化合物在较小的纳米晶体尺寸下压倒性地朝向正常尖晶石构型。正数被困在较小的微晶中增加数量的更大空位。原因是在八面体的位点形成的空缺,其中Fe3 +的增加的离子半径变得足够大,以显着降低占用率。 Mossbauer光谱分析表明在较高温度下烧结的样品中的铁磁性性质的增加。在300°C和400°C时,样品占主导地位的顺磁性行为。

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