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变高岭石的结构研究
引用本文:刘长龄,刘钦甫,陈济舟,张鹏飞,王俊桥,覃志安.变高岭石的结构研究[J].硅酸盐学报,2001,29(1):63-67.
作者姓名:刘长龄  刘钦甫  陈济舟  张鹏飞  王俊桥  覃志安
作者单位:1. 天津地质研究院,
2. 中国矿业大学北京校区,
3. 天津理工学院,
基金项目:国家自然科学基金资助项目!(4980 2 0 10 )
摘    要:变高岭石是高岭石的加热相变产物,用广角度X射线衍射散射(WAXS)和由它得到的径向分布函数(RDF)研究了变高岭石结构表明:它是一种含有少量结晶相或沿c轴失序的半晶物质,其结晶度随热处理温度而变化。构成变高岭石的结构单元是四面体MO4](M=Si,Al)和八面体Al2O6]。变高岭石结构中近邻四面体与四面体、四面体与八面体是共顶连接的。变高岭石的近程结构将不随结晶性或序性变化。它的微结构及其随热处理温度的变化主要决定于结构基元之间的关系和序性。

关 键 词:变高岭石  结构  径向分布函数  广角度X射线衍射散射
文章编号:0454-5648(2001)01-0063-05
修稿时间:2000年5月22日

STRUCTURE OF METAKAOLINITE
Liu Changling,Liu Qinfu,CHEN Jizhou,Zhang Pengfei,WANG Junqiao,Tan Zhian.STRUCTURE OF METAKAOLINITE[J].Journal of The Chinese Ceramic Society,2001,29(1):63-67.
Authors:Liu Changling  Liu Qinfu  CHEN Jizhou  Zhang Pengfei  WANG Junqiao  Tan Zhian
Abstract:Metakaolinite is a phase_changed substance obtained through heating kaolinite. The research on the structure of metakaolinite by using wide_angle X -ray diffraction_scattering technology(WAXS) and its radial distribution function(RDF) shows that metakaolinite is a hemicrystal which is disordered in c -axle and composed of non_crystalline phase and a little crystalline phase. The crystallinity is changed with heating temperature. The structure unites are tetrahedral MO 4](M=Si,Al) and octahedral AlO 6]. The adjacent tetrahedral-tetrahedral and tetrahedral-octahedral in metakaolinite are co_apical linkage, but the octahedral-octahedral are coplanar linkage. The short_range structure of metakaolinite is not changed with its crystallinity or ordered degree. The microstructure of metakaolinite and its changes with heating temperature are mainly depended on the relationship between the structure unites and ordered degree in metakaolinite.
Keywords:metakaolinite  structure  radial distribution function
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