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Investigation of sintered iron ore fines as an oxygen carrier in chemical looping combustion

机译:烧结铁矿粉作为氧气在化学循环燃烧中的载体研究

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Sintered iron ore fines were selected as oxygen carriers in chemical looping combustion. The reactivity of the sintered iron ore was investigated in redox cycles using thermogravimetric methods under isothermal or non-isothermal conditions. The used sintered iron ore samples from the redox cycles in isothermal tests, which were chosen to evaluate their structural changes, were characterized using the N-2 adsorption-desorption, SEM-EDS, XRD and Raman spectroscopy. Results revealed that multiple redox cycle was an activation process of the selected sintered iron ore to promote its redox kinetics, as well as formations of the new crystalline phase. This was attributed to variations of the sintered iron ore in both their physical and chemical structural changes during redox cycles. The N-2 adsorption-desorption analysis indicated an increase of its surface areas of sintered iron ore during redox cycles. The SEM-EDS results revealed the appearance of tiny cracks on the tested ore sample surfaces. Both XRD and Raman results presented appearance of a new crystalline phase, such as the lepidocrocite (gamma-FeOOH), which was apparently generated in the reduction reaction of chemical looping cycles. The formation of the new lepidocrocite phase seemed correlated with the decrease of the oxygen transport capacity of the sintered iron ore. The sintered iron ore performed properly in the carbon-laden atmospheres, and there was no carbon deposition on its surface.
机译:在化学循环燃烧中选择烧结铁矿粉作为氧气载体。在等温或非等温条件下,使用热重法在氧化还原循环中研究了烧结铁矿石的反应性。使用N-2吸附-解吸,SEM-EDS,XRD和拉曼光谱对经过等温测试的氧化还原循环中使用过的烧结铁矿石样品进行评估,以评估其结构变化。结果表明,多个氧化还原循环是所选烧结铁矿石的活化过程,以促进其氧化还原动力学以及新结晶相的形成。这归因于在氧化还原循环中烧结铁矿石的物理和化学结构变化。 N-2吸附-解吸分析表明,在氧化还原循环中,烧结铁矿石的表面积增加。 SEM-EDS结果显示在测试的矿石样品表面上出现细小裂纹。 XRD和拉曼结果均显示出新的结晶相,如轻铁云母(γ-FeOOH),显然是在化学循环循环的还原反应中产生的。新的斜铁云母相的形成似乎与烧结铁矿石的氧气输送能力下降有关。烧结铁矿石在充满碳的气氛中表现良好,并且在其表面上没有碳沉积。

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