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Effect of Al_2O_3, SiO_2 and MgO on the Formation of Calcium Ferrites in Sinter using X-ray Diffraction Method

机译:X射线衍射法研究Al_2O_3,SiO_2和MgO对烧结矿中钙铁氧体形成的影响

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摘要

In order to elucidate the fundamental aspects of the minerals formation processes during sintering, the Fe_2O_3-CaO-Al_2O_3-SiO_2 system and the effect of MgO on synthesized iron ore sinter were studied by image analysis and X-ray diffraction method. Most existed calcium ferrite was identified to be a solid solution of CaO centre dot 2Fe_2O_3 with a small amount of solubility of Al_2O_3 and SiO_2. With an increase of the content of Al_2O_3 in the system, the amount of calcium ferrite was increased. On the other hand, the amount of calcium ferrite was decreased, and the amount of hematite was increased with increasing the content of SiO_2. Crystal structure of calcium ferrite with Al_2O_3 and SiO_2 was changed from monoclinic to triclinic as well as the unit cell volume shrank with fixing Al_2O_3 and increasing SiO_2. With increasing the content of MgO(1 approx 3 wt percent), the amount of magnetite was increased and hematite was decreased but calcium ferrite was not changed.
机译:为了阐明烧结过程中矿物形成过程的基本方面,通过图像分析和X射线衍射方法研究了Fe_2O_3-CaO-Al_2O_3-SiO_2体系以及MgO对合成铁矿石烧结体的影响。确定存在最多的铁氧体钙为CaO中心点2Fe_2O_3的固溶体,Al_2O_3和SiO_2的溶解度较小。随着体系中Al_2O_3含量的增加,铁素体钙的含量增加。另一方面,随着SiO 2含量的增加,铁素体钙的量减少,赤铁矿的量增加。 Al_2O_3和SiO_2组成的铁氧体钙的晶体结构从单斜晶变为三斜晶,并且随着Al_2O_3的固定和SiO_2的增加,晶胞体积减小。随着MgO(1约3 wt%)含量的增加,磁铁矿的数量增加,赤铁矿的数量减少,但铁素体钙不变。

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