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首页> 外文期刊>Current Nanoscience >A Non-Alkoxide Sol-Gel Method for the Preparation of Magnetite (Fe_3O_4) Nano-particles
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A Non-Alkoxide Sol-Gel Method for the Preparation of Magnetite (Fe_3O_4) Nano-particles

机译:一种非醇盐溶胶-凝胶法制备磁铁矿(Fe_3O_4)纳米粒子

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摘要

Magnetite (Fe_3O_4) nanoparticles in the interval of 9~12nm have been synthesized by an non-alkoxide sol-gel method. Through this simple technique, sol-gel materials were prepared from ethanolic solutions of metal chlorides without the need for alkoxides, polymeric gel agents, or elaborate reaction schemes. The gel formation has been studied, and the research shows that gel formation appears to be driven primarily by the formation of an Fe(III)-based network which incorporates Fe(II) into its nanoscale solid domains. The research of the annealing process indicates that magnetite (Fe_3O_4) nanoparticles can be obtained by annealing only under vacuum, but not in air. Future, Fe_3O_4 can be oxidized to Fe_2O_3, as evidenced by XRD, and VSM. The phase structures, morphologies, and particle sizes of Fe_3O_4 nanoparticles were characterized by thermogravimetric-differential thermal analysis (TG-DTA), X-ray Diffraction (XRD) and Transmission Electron Microscopy (TEM). The results indicate that magnetite (Fe_3O_4) nanoparticles are homogeneous and have near-spherical shape with a narrow distribution in particle size. Finally, an investigation of the possible mechanism of Fe_3O_4 nanoparticles formation was performed. Both TG-DTA and X-ray Diffraction (XRD) studies suggest that the reaction of the decomposition of the precursor under vacuum conditions leads to Fe_3O_4 nanoparticles, while the precursors in air atmosphere is directly oxidized to gamma iron oxide. In addition, this approach may suggest a general route to produce complex multicomponent metal oxide in which the nanoscale oxide is stabilized and spatially distributed.
机译:采用非醇盐溶胶-凝胶法合成了9〜12nm范围的磁铁矿(Fe_3O_4)纳米粒子。通过这种简单的技术,无需使用醇盐,聚合凝胶剂或复杂的反应方案,即可从金属氯化物的乙醇溶液制备溶胶-凝胶材料。已经研究了凝胶的形成,并且研究表明凝胶的形成似乎主要是由基于Fe(III)的网络的形成驱动的,该网络将Fe(II)结合到其纳米级固态域中。退火过程的研究表明,磁铁矿(Fe_3O_4)纳米粒子只能通过在真空下退火而不能在空气中退火而获得。未来,X射线衍射和VSM可以证明Fe_3O_4可以被氧化为Fe_2O_3。 Fe_3O_4纳米粒子的相结构,形貌和粒径通过热重差热分析(​​TG-DTA),X射线衍射(XRD)和透射电子显微镜(TEM)表征。结果表明,磁铁矿(Fe_3O_4)纳米粒子是均质的,具有接近球形的形状,粒径分布较窄。最后,对Fe_3O_4纳米颗粒形成的可能机理进行了研究。 TG-DTA和X射线衍射(XRD)研究均表明,前驱物在真空条件下的分解反应会生成Fe_3O_4纳米粒子,而空气中的前驱物则被直接氧化为γ-氧化铁。另外,该方法可以建议一种生产复杂的多组分金属氧化物的通用途径,其中纳米级氧化物被稳定化并在空间上分布。

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