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首页> 外文期刊>Journal of thermal analysis and calorimetry >The oxidation kinetics study of ultrafine iron powders by thermogravimetric analysis
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The oxidation kinetics study of ultrafine iron powders by thermogravimetric analysis

机译:热重分析法研究超细铁粉的氧化动力学

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The oxidation kinetics of ultrafine metallic iron powder to hematite (α-Fe_2O_3) up to temperatures 800 °C were studied in air using non-isothermal and isothermal thermogravimetric (TG) analysis. The powders with average particles size of 90, 200, and 350 nm were made by the electric explosion of wire. It was observed that the reactivity of the iron powder is increased with the decreasing particle size of powder. The experimental TG curves clearly suggest a multi-step process for the oxidation, and therefore a model-fitting kinetic analysis based on multivariate non-linear regressions was conducted. The complex reaction can be best described with a three-step reaction scheme consisting of two concurrent and one parallel reaction step. In one reaction pathway Fe is oxidized to α-Fe_2O_3. The other pathway is described by the oxidation of Fe to magnetite (Fe_3O_4). At higher temperatures the formed Fe_3O_4 is further oxidized in a α-Fe_2O_3. It is established that the best fitting three-step mechanism employed a branching set of n-order equations for each step.
机译:利用非等温和等温热重分析(TG),研究了超细金属铁粉在高达800°C的温度下对赤铁矿(α-Fe_2O_3)的氧化动力学。通过电线的电爆炸制备平均粒径为90、200和350 nm的粉末。观察到,铁粉的反应性随粉末的粒径减小而增加。 TG实验曲线清楚地表明了氧化的多步骤过程,因此进行了基于多元非线性回归的模型拟合动力学分析。复杂的反应可以用三步反应方案来最好地描述,该方案由两个同时的反应步骤和一个平行的反应步骤组成。在一个反应​​途径中,Fe被氧化为α-Fe_2O_3。另一个途径是通过Fe氧化成磁铁矿(Fe_3O_4)来描述的。在较高温度下,形成的Fe_3O_4在α-Fe_2O_3中进一步被氧化。可以确定的是,最适合的三步机制为每个步骤采用了一个n阶方程的分支集。

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