反应烧结法合成海方石中SiO_2的赋存状态

Chen Junhong, M. Yan, Jin-dong Su, Bin Li, Yong Li, Zhihui Li, Jia-lin Sun, L. Dongfang
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引用次数: 0

摘要

以Fe2O3、Al2O3和Si O2粉末为原料,按Fe O:Al2O3的质量比为40.8:59.2,在合成体系中加入1%的Si O2,在1 600℃的高纯氮气气氛下烧结4 h,对样品进行了x射线衍射、扫描电镜、能量色散光谱和透射电镜的分析和表征。基于Fe o - al2o3 - sio2三元相图,研究了二氧化硅的存在性。结果表明,二氧化硅并未进入海方石晶体,而是以非晶态存在于海方石晶体中。当合成体系中加入一定比例的Si O2时,含Si O2的非晶态相不连续分布,并没有改变硅尖晶石晶体之间的直接接触。
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Occurrence State of SiO_2 in Hercynite Synthesized by Reaction Sintering
Sample was prepared using Fe2O3, Al2O3 and Si O2 powders as raw materials according to mass ratio Fe O:Al2O3 of 40.8:59.2 and adding a percent of Si O2 in the synthetic system, and being sintered under high purity nitrogen atmosphere at 1 600 ℃for 4 h. The sample was analyzed and characterized by X-ray diffraction, scanning electron microscope, energy dispersive spectroscopy and transmission electron microscope. Based on Fe O-Al2O3-Si O2 ternary phase diagram, the existence of silicon dioxide was investigated. The results indicate that silicon dioxide didn't enter into hercynite crystals, but existed among hercynite crystals as amorphous phase. When a percent of Si O2 was added into the synthetic system, amorphous phase containing Si O2 was discontinuously distributed and the direct contact among hercynite crystals wasn't changed.
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