钛铁矿非等温氢还原动力学的构造模型与实验验证:关于 Kahnuj 钛铁矿的案例研究

Leila Ghasemi, Seyed Hossein Seyedein, Mandana Adeli, Mohammad Reza Aboutalebi
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摘要

在这项研究中,研究了来自国内矿山(伊朗克尔曼卡努吉)的钛铁矿精矿在 500 °C 至 1100 °C 温度范围内的纯氢中的还原动力学。根据非等温还原结果,使用 Coats-Redfern 方法计算了原精矿和预氧化精矿的相应动力学参数。原钛铁矿和预氧化钛铁矿在 800 ℃ 下的还原过程都是通过产物层的扩散控制的。对在 1000 ℃ 下预氧化的钛铁矿进行的动力学分析表明,还原过程遵循化学反应以及成核和生长机制。与未加工的钛铁矿相比,在 800 ℃ 和 1000 ℃ 下预氧化的样品表现出更高的质量损失值和还原度。预氧化对钛铁矿还原的促进作用归因于预氧化钛铁矿的相变以及预氧化后还原过程中产生的多孔结构。X 射线衍射(XRD)图证实,在 800 ℃ 氧化后存在假金红石、金红石和赤铁矿,而在 1000 ℃ 氧化后,假沸石和金红石是稳定的相。
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Constitutive Model and Experimental Verification of Kinetics of Non-isothermal Hydrogen Reduction of Ilmenite: A Case Study on Kahnuj Ilmenite

In this study, the reduction kinetics of ilmenite concentrate from a domestic mine (Kahnuj, Kerman, Iran) in pure hydrogen in the temperature range of 500 °C to 1100 °C was investigated. From the non-isothermal reduction results corresponding kinetic parameters for the as-received and pre-oxidized concentrates were calculated using the Coats-Redfern method. The reduction process in both raw and pre-oxidized ilmenite, at 800 °C was controlled by diffusion through the product layer. The kinetic analysis for ilmenite pre-oxidized at 1000 °C indicated that the reduction process followed a chemical reaction and nucleation and growth mechanism. The samples pre-oxidized at 800 °C and 1000 °C exhibited higher mass loss values and reduction degrees compared to the raw ilmenite. The promoting effect of pre-oxidation on the reduction of ilmenite is attributed to the phase changes in pre-oxidized ilmenite and the porous structure created during the reduction process after the pre-oxidation process. X-ray diffraction (XRD) patterns confirmed the presence of pseudorutile, rutile, and hematite after oxidation at 800 °C, and pseudobrookite and rutile were stable phases after oxidation at 1000 °C.

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