用热重分析法和控制速率热分析法研究高岭石的热脱羟基作用

J. Mbey, Cyrill Joël Ngally Sabouang, Thomas B. Makon, S. Coulibaly, Sakéo Kong
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引用次数: 3

摘要

这项工作的目的是确定影响高岭石向偏高岭石转化的参数。为此,采用控制率热分析(CRTA)和热重分析(TGA)对四种高岭石的脱羟基化进行了研究。采用x射线衍射(XRD)和傅里叶红外(FTIR)对样品的高岭石性质进行了表征。利用x射线衍射(XRD)的欣克利指数(Hinckley index)对其结晶度进行了评价,并用透射电子显微镜(TEM)对其进行了形态学观察。样品的热分析表明,对于所有的样品,低缺陷,揭示了低量的吸附水在粘土表面。两种方法的脱羟基温度均受样品结晶度和粒径的影响。从两种技术中观察到,结晶度的增加导致脱羟基温度的升高。此外,还提出了粘土薄片大小对脱羟基温度的影响。结果表明,结晶度和粒度是控制高岭石向偏高岭石转化温度的重要参数。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The thermal dehydroxylation of kaolinite using thermogravimetric analysis and Controlled rate thermal analysis
The aim of this work was to identify parameters that could influence the conversion of kaolinite into metakaolinite. To this end, the dehydroxylation of four kaolinites, using controlled rate thermal analysis (CRTA) and thermogravimetric analysis (TGA), was investigated. X-ray diffraction (XRD) and Fourier transform infra-red (FTIR) were used to confirm the kaolinitic nature of the samples. Their crystallinity was evaluated using the Hinckley index from the XRD patterns and transmission electron microscopy (TEM) was used for morphological observation of the clay platelets. The thermal analyses of the samples indicate, for all samples, low defects as revealed by the low amount of adsorbed water on the clay surface. The dehydroxylation temperature from both techniques was influenced by the sample crystallinity and particle size. It was observed from both techniques that increase crystallinity resulted in high dehydroxylation temperature. Also, the influence of the clay platelets size on the dehydroxylation temperature, is proposed. All the results indicate that crystallinity and particle size are parameters that could be used to control the temperature for the conversion of kaolinite to metakaolinite.
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