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The effect of calcination temperature on the synthesis of magnetic silica nanoparticles from geothermal sludge

机译:煅烧温度对地热污泥合成磁二氧化硅纳米粒子的影响

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Geothermal sludge is a waste from geothermal power plants (PLTP) with very high silica content. Geothermal sludge waste is potential as a basic material in the synthesis of silica nanoparticles. The research was conducted using FeCl_3 salt as Fe ions precursors forming the silica magnetic nanoparticles. This was obtained by reacting silica waste with NaOH 1,5 N at 90°C, added with 1,6 gr FeCl_3 and subsequently adding 2N HCl solution to form a gel at pH 5 and aging for 18 hours. The calcination temperature of the samples were varied at 400°C, 500°C, 600°C and 700°C. Characterization of magnetic silica nanoparticle included Brauner Emmet Teller (BET) to determine the surface area, X-Ray Diffraction (XRD) for phase identification and morphology of the nanoparticles was characterized Transmition Electron Mycroscope (TEM). The results showed that samples calcined at 400°C was in its amorphous phase and has the highest surface area of 658.11 m~2/g.
机译:地热污泥是来自地热发电厂(PLTP)的废物,具有非常高的二氧化硅含量。地热污泥废物是合成二氧化硅纳米颗粒的基本材料。使用FECL_3盐作为形成二氧化硅磁性纳米颗粒的Fe ICE前体进行该研究。这是通过在90℃下用NaOH 1,5 N反应二氧化硅废物而获得的,加入1,6 GR FECL_3并随后加入2N HCl溶液以在pH5处形成凝胶,老化18小时。样品的煅烧温度在400℃,500℃,600℃和700℃下变化。磁性二氧化硅纳米粒子的表征包括Brauner Emmet Teller(BET)以确定用于相位鉴定的表面积,X射线衍射(XRD)和纳米颗粒的形态被表征透射电子杂物镜(TEM)。结果表明,在400℃下煅烧的样品在其非晶相中,具有658.11m〜2 / g的最高表面积。

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