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Comparative Study between Direct and Pseudomorphic Transformation of Rice Husk Ash into MFI-Type Zeolite

机译:稻壳灰直接和假性转变为MFI型沸石的比较研究

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Pre-shaped mesoporous amorphous rice husk ash (RHA) and MCM-41 derived from RHA as a silica source were transformed into MFI-type zeolites using two different structure-directing agents. Tetrapropylammonium hydroxide (TPAOH) was utilized as an alkali source for silica dissolution and structure control during the direct transformation of RHA into zeolite. A monopropylamine (PA)-containing alkaline solution (NaOH) was used for the pseudomorphic transformation of RHA or MCM-41 into zeolite. The hydrothermal conversion of RHA or MCM-41 into MFI-type zeolites was investigated as a function of reaction time at 175 °C. With PA as template, the crystallization took place inside and on the outer surface of RHA or MCM-41 without losing the original shape of the initial silica sources, while TPAOH led to the formation of conventional MFI-type zeolite crystals due to the complete dissolution of RHA. The final products were characterized by X-ray diffraction, nitrogen adsorption, scanning electron microscopy, and optical emission spectroscopy.
机译:使用两种不同的结构导向剂,将预成型的介孔无定形稻壳灰(RHA)和衍生自RHA的MCM-41作为二氧化硅来源转化为MFI型沸石。在RHA直接转化为沸石的过程中,氢氧化四丙基铵(TPAOH)被用作二氧化硅溶解和结构控制的碱源。含一元丙胺(PA)的碱性溶液(NaOH)用于RHA或MCM-41向沸石的假晶转变。研究了RHA或MCM-41到MFI型沸石的水热转化,它是在175°C下反应时间的函数。以PA为模板,结晶发生在RHA或MCM-41的内部和外部表面,而不会失去初始二氧化硅来源的原始形状,而TPAOH由于完全溶解而导致形成常规的MFI型沸石晶体RHA。最终产物通过X射线衍射,氮吸附,扫描电子显微镜和光发射光谱进行表征。

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