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Annealing Temperature Effects in Co-Precipitated CoFe_2O_4 Nanoparticles Using Bengawan Solo River Fine Sediment

机译:使用BINGAWAN SOLO河细沉积物共沉淀的COFE_2O_4纳米粒子的退火温度效应

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In this study, the synthesis of CoFe_2O_4 by using the fine sediment of the Bengawan Solo River, Trucuk District, Bodjonegoro Regency as raw materials. Synthesis with the coprecipitation method has been successfully carried out. The fine sediment is used as a source of Fe cation in the synthesis of CoFe_2O_4 from the nature. The XRD confirmation results showed that CoFe_2O_4 is formed at an annealing temperature of 800° C with crystallite sizes ranging from 34.88 to 38.05 nm. Thus, the VSM characterization showed that the magnetic properties of the CoFe_2O_4 nanoparticles depend on the heat treatment of the fine sediments as ore materials. Finally, the obtained CoFe_2O_4 samples can be used as photocatalysts with a maximum reduction rate ratio of 83%.
机译:在本研究中,通过使用BINGAWAN SOLO RIVER,TRUCUK区,BODJONEGORO REGENCY作为原材料的精细沉积物来合成COFE_2O_4。 已成功进行与CopRecipition方法的合成。 精细沉积物被用作来自性质的Cofe_2O_4的合成中的Fe阳离子来源。 XRD确认结果表明,CoFe_2O_4在800℃的退火温度下形成,微晶尺寸范围为34.88至38.05nm。 因此,VSM表征显示COFE_2O_4纳米颗粒的磁性特性取决于精细沉积物作为矿石材料的热处理。 最后,获得的COFE_2O_4样品可用作最大降低率比为83%的光催化剂。

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