FexO-TiO2体系的固相反应机理

Solid state reaction mechanism of the FexO-TiO2 system

  • 摘要: 采用扩散偶法研究了1323~1473 K下FexO-TiO2体系的固相反应,反应过程中氧分压由一定比例的CO-CO2混合气体控制.扩散偶截面的微观形貌用电子探针进行观察,并对Fe2+、Ti4+和O2-离子的扩散浓度轮廓进行定量分析.结合FeO-TiO2体系相图确定了固相反应中有钛铁晶石、钛铁矿和假铁板钛矿相生成,且它们的生长受扩散控制.依据扩散组元的摩尔分数变化绘制了铁离子的扩散路径图,并在此基础上描述了该体系的固相反应机理.

     

    Abstract: The diffusion couple was used to study solid state reaction in the FexO-TiO2 system at a temperature range of 1323 to 1473 K,during which the oxygen partial pressure was controlled by CO-CO2 gas mixture. The cross-sections of the diffusion couple were observed by electron probe microanalysis(EPMA),and the diffusion concentration profiles of Fe2+,Ti4+,and O2- ions were also determined. In combination with the phase diagram of the Fe O-TiO2 system,it was found that ulvospinel,ilmenite,pseudobrookite phases formed during the reaction and their growth was diffusion-controlled. According to the concentration changes of diffusion ions,the diffusion path of Fe ions was plotted,based on which the solid state reaction mechanism of this system was reasonably proposed.

     

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