用尼日利亚河州科诺布埃和乔科乔当地高岭土合成X型沸石

Victor Peter Maciver, K. Dagde, J. Konne
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引用次数: 6

摘要

这项工作描述了从尼日利亚河流州科诺布埃和乔科乔开采的高岭土中生产沸石X的工艺开发。该工艺包括原料高岭土的选矿和850°C的煅烧,将高岭土转化为活性更强的偏高岭土。然后,用硫酸清洗极具活性的偏高岭土,以获得合成沸石X所需的硅铝比。然后进行碱性熔融阶段,将偏高岭土与NaOH水溶液混合形成凝胶,将偏高岭土转化为沸石,然后在室温下放置7天。然后将样品装入丙烯容器中,在100℃的烤箱中进行反应6小时。通过x射线衍射(XRD)鉴定晶体相,x射线荧光(XRF)/能量色散光谱(EDS)分析化学/元素组成,扫描电子显微镜(SEM)分析表面形貌,傅里叶变换红外分光光度法(FT-IR)分析单元的分子振动。结果表明,由Chokocho高岭土(CK)合成的沸石比由Kono-Boue合成的沸石晶体更大,XRD和FTIR峰更清晰。在SEM上,CK比KK稍微粗糙的表面形貌也支持了这一点。KK和CK的XRF Si:Al比值分别为10.73和14.36。EDS结果支持XRF比值。在3488 cm-1和3755 cm-1处,CK比KK记录到更明显的沸石特征O-H拉伸带。结果表明,Kono-Boue和Chokocho两种高岭土均可制备X型沸石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Synthesis of Zeolite X from Locally Sourced Kaolin Clay from Kono-Boue and Chokocho, Rivers State, Nigeria
This work describes the development of a process to produce zeolite X from mined kaolin clay from Kono-Boue and Chokocho, Rivers State, Nigeria. The procedures involved the beneficiation of the raw kaolin and calcinations at 850°C, to transform the kaolin to a more reactive metakaolin. Afterwards, the extremely reactive metakaolin was purge with sulphuric acid to obtain the much needed silica-alumina ratio for zeolite X synthesis. An alkaline fusion stage was then carried out to transform the metakaolin into zeolite by mixing with aqueous NaOH to form gel then allowed to stay for a duration of seven days at room temperature. The samples were then charged into a propylene container and placed in an oven at a temperature of 100°C for the reaction to take place for 6 h. Identification of the crystalline phases by X-ray Diffraction (XRD), chemical/elemental compositions by X-ray Fluorescence (XRF)/Energy Dispersive Spectroscopic analyses (EDS), surface morphology by Scanning Electron Microscopy (SEM) and molecular vibration of units by Fourier Transform Infrared Spectrophotometry (FT-IR) were done. The results showed that the zeolite synthesized from Chokocho kaolin (CK) was more crystalline/larger with sharper peaks on both XRD and FTIR than that from Kono-Boue. This was also supported by slightly rougher surface morphology of CK over KK on SEM. XRF Si:Al ratios of 10.73 and 14.36 were obtained for KK and CK respectively. EDS results supported the XRF ratios. Sharper zeolitic characteristic O-H stretching bands at 3488 and 3755 cm-1 were recorded for CK than KK. However, both results showed that zeolite X have been produced from both Kono-Boue and Chokocho kaolin clays respectively.
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