稀土正铁氧体与赤铁矿纳米复合材料的特性

O. Lavrynenko, O. Pavlenko, O. Olifan
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摘要

基于稀土元素的正铁氧体光催化剂在可见光的作用下可以中和多种有害物质和有机染料,这使得它们有望引入资源节约型水净化技术。采用热重分析、x射线物相分析、扫描电镜、能谱分析等方法,对铁的无机盐与镧系元素(La、Er、Sm、Dy、Nd、Yb)和Y的水溶液在弱碱性环境下化学沉淀,并在800℃和1100℃下对沉积物进行热处理,得到稀土元素和赤铁矿的纳米级正铁氧体样品进行了研究。研究发现,在铁和稀土的氢氧化物相同时析出过程中,由于相变温度和前驱相析出氢指数的差异,它们在温度影响下的转变在空间上是分离的。结果表明,根据初始溶液的化学组成,针铁矿在190 ~ 250℃的温度范围内形成,赤铁矿在425 ~ 450℃形成。在300-330°С观察到氢氧化镧的脱羟基作用,在390 - 900°С范围内继续形成氧化镧。钙钛矿相在960℃时结晶。通过x射线物相分析,确定了800℃热处理后的沉积物中存在赤铁矿和稀土氧混合物相。在1100℃时,粉末的组成中有25 ~ 40 nm的钙钛矿和赤铁矿结构。测定了在650 ~ 770℃的温度下辅助物质的去除,1100℃烧制的粉末中没有K、Na、S、Cl、C等杂质。赤铁矿和钙钛矿颗粒结晶良好,形成脆弱的团聚体,样品的比表面积为几m2/h。
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Characteristics of nano-sized composites based on rare earth orthoferrites and hematite
Photocatalysts based on orthoferrites of rare earth elements are used to neutralize a number of harmful substances and organic dyes under the influence of visible light, which makes them to promise the introduction of resource-saving water purification technologies. The thermal-gravimetric analysis, X-ray phase analysis, scanning electron microscopy, and energy-dispersive spectroscopy was used to study nanoscale samples of orthoferrites of rare earth elements and hematite obtained by the chemical precipitation of aqueous solutions of inorganic salts of ferrum with lanthanides (La, Er, Sm, Dy, Nd, Yb ) and Y in a weakly alkaline environment and subsequent heat treatment of sediments at 800 and 1100 °C. It was found that during the simultaneous precipitation of hydroxide phases of ferrum and REE, their transformation under the influence of temperature is spatially separated due to the differences in the temperatures of phase transformations and the hydrogen index of the precipitation of precursor phases. It is shown that, depending on the chemical composition of the initial solutions, goethite is formed in the temperature range of 190-250 °C, and the formation of hematite takes place at 425-450 °C. Dehydroxylation of lanthanum hydroxide is observed at 300-330 °С, and the formation of lanthanum oxides continues in the range from 390 to 900 °С. The perovskite phase crystallizes at 960 °C. Using the X-ray phase analysis method, it was established that hematite and a mixture of REE oxygen phases are present in the sediments heat-treated at 800 °C. At 1100 °C, the structure of perovskite and hematite with particle sizes from 25 to 40 nm was identified in the composition of the powders. It was determined that the removal of auxiliary substances takes place at temperatures of 650-770 °C and no impurities of K, Na, S, Cl, or C in the powders fired at 1100 °C. Hematite and perovskite particles are well crystallized and form fragile aggregates, the specific surface area of the samples is several m2/h.
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