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Crystal-growth kinetics of magnetite (Fe3O4) nanoparticles with Ostwald Ripening Model approach

机译:磁铁矿(Fe3O4)纳米粒子的晶体生长动力学,具有Ostwald成熟模型方法

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Magnetite (Fe3O4) nanoparticles is a magnetic nanomaterial that have potential properties to be applied as drug delivery The purpose of this study was to determine the influence of time and temperature synthesis of magnetie characteristics and determine its crystal growth kinetics model with Ostwald ripening model approach. Magnetite nanoparticles synthesized from FeCh, citrate, urea and polyethylene glycol with hydrothermal method at 180, 200 and 220 °C for 1,3,5,7,9 and 12 hours. Characterization by X-ray Diffraction (XRD) indicated that magnetite formed at temperatures of 200 and 220 °C. Magnetite crystallite diameter obtained was 10-29 nm. Characterization by Transmission Electron Mycroscope (TEM) shows that magnetite nanoparticles have uniform size and non-agglomerated. Core-shell shaped particles formed at 200 °C and 220 °C for 3 hours. Irregular shape obtained at 220 °C for 12 hour synthesis with particle diameter about 120 nm. Characterization using Vibrating Sample Magnetometer (VSM) shown that magnetite has super paramagnetism behaviour with the highest saturation magnetization (Ms) was 70.27 emu/g. magnetite crystal growth data at temperature of 220 °C can be fitted by Ostwald ripening growth model with growth controlled by the dissolution of surface reaction (n≈4) with the percent error of 2.53%.
机译:磁铁矿(Fe3O4)纳米颗粒是一种磁性纳米材料,其具有潜在的特性,待应用于药物递送本研究的目的是确定磁性特性的时间和温度合成的影响,并确定其具有Ostwald成熟模型方法的晶体生长动力学模型。磁铁矿纳米颗粒由熔融,柠檬酸盐,尿素和聚乙二醇合成,具有180,200和220℃的水热法,用于1,3,5,7,9和12小时。 X射线衍射(XRD)的表征表明,在200和220℃的温度下形成的磁铁矿。获得的磁铁矿晶体直径为10-29nm。透射电子镜(TEM)的表征显示磁铁矿纳米颗粒具有均匀的尺寸和非聚集。核 - 壳形颗粒在200℃和220℃下形成3小时。在220℃下获得的不规则形状12小时合成,粒径为约120nm。使用振动样品磁力计(VSM)表征示出磁铁矿具有最高饱和磁化强度(MS)的超级顺法行为为70.27兆/克。磁铁矿晶体生长数据在220℃的温度下,通过骨果实成熟的生长模型,通过溶解表面反应(N≈4)的溶解,误差为2.53%的百分比。

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