空气氧化法制备Fe3O4的反应机理

来源期刊:中南大学学报(自然科学版)2008年第3期

论文作者:杨喜云 龚竹青 彭长宏 陈白珍 徐徽 石西昌

文章页码:454 - 454

关键词:空气氧化法;Fe3O4;反应机理

Key words:air oxidation; Fe3O4; formation mechanism

摘    要:采用空气氧化法制备Fe3O4,分析反应过程中pH值随时间变化曲线和Fe的形态变化规律;用XRD和SEM检测反应各个阶段沉淀物的物相组成和形貌变化。研究结果表明:在中性和酸性介质中,Fe3O4的生成分3个阶段:Fe(OH)2悬浮液氧化为绿锈,绿锈转变为球形Fe3O4,Fe3O4氧化为针形FeOOH;氧化反应发生在液相,随着氧化的进行,pH值和液相Fe2+浓度发生改变,Fe3O4粒度不断增大;制备Fe3O4时,应控制pH值大于5.4,固相Fe(Ⅲ)与Fe(Ⅱ)的摩尔比小于1.8。

Abstract: Magnetite was prepared by air oxidation. Relationship between pH value and time was analyzed and the state change of iron was recorded during the formation process. Phase composition and morphology of the precipitates were detected with XRD and SEM at several stages of oxidation, respectively. The results show that three stages are observed during Fe3O4 formation in neutral and acidic media, the process is that Fe(OH)2 suspension is oxidized to green rust followed by converting to spherical magnetite particles, then some magnetite particles gradually oxidize to acicular FeOOH. The oxidation occurs in the aqueous solution. As oxidation continues, pH value and Fe(Ⅱ) concentration in supernatant liquid change with time, and Fe3O4 particle size increases. To get Fe3O4 with good quality, pH value should be greater than 5.4, and the molar ratio of Fe(Ⅲ) to Fe(Ⅱ) in the solid phase should be less than 1.8.

基金信息:湖南省自然科学基金资助项目
国家高技术发展计划资助项目

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