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Degradation of Iron Oxide Caused by Alumina during Reduction from Magnetite

机译:磁铁矿还原过程中氧化铝引起的氧化铁降解

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The degradation mechanism of iron oxides caused by alumina during reduction from magnetite has been studied. The experiments were carried out by reducing briquettes containing various mixtures of commercial magnetite fines and Al_2O_3 in a CO/CO_2 atmosphere at 950℃ in thermo-gravimetric equipment. Following reduction, samples were examined using optical microscopy, SEM-EDS and XRD. The diffusion of Al cations into the magnetite during reduction induces swelling and cracking of the briquettes. The composition of the magnetite phase approaches the composition of hercynite during reduction. Assuming the spinel structure is that of hercynite, reduction to non-stoichiometric wustite (Fe_(0.88)O) causes an expansion of over 16%. This transformation causes high tension forces in the magnetite/her-cynite phase in the vicinity of the interface with the wuestite which presumably account for the breakdown of the structure during the reduction.
机译:研究了由磁铁矿还原过程中氧化铝引起的氧化铁的降解机理。通过在热重设备中在950℃的CO / CO_2气氛中还原含有各种磁铁矿粉和Al_2O_3混合物的团块来进行实验。还原后,使用光学显微镜,SEM-EDS和XRD检查样品。在还原过程中,铝阳离子扩散到磁铁矿中会导致团块膨胀和开裂。在还原过程中,磁铁矿相的组成接近锂铁矿的组成。假设尖晶石结构是水英石,则还原为非化学计量的辉石(Fe_(0.88)O)会导致膨胀超过16%。这种转变在与钙铁矾的界面附近的磁铁矿/钙铁矿相中引起高张力,这可能是由于在还原过程中结构的破坏。

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