摘要
文中以大冶四棵高岭土为研究对象,采用多种分析技术探讨、评价该资源的存在形态和特征.研究表明:四棵高岭土属于高硅(石英)、铁质渗蚀型的砂质粘土,石英及其它杂矿(长石)以较大颗粒存在,高岭土存在颗粒较小.
The behaviour of shike kaolinite in the raw has been studied from the point of riew of chemistry by x-rays diffraction, thermal analysis and chemical analysis. The experiment shows the consituent and relationship with size distribution of shike kaolinite.
出处
《湖北师范学院学报（哲学社会科学版）》
1994年第6期83-85,101,共4页
Journal of Hubei Normal University（Philosophy and Social Science）
关键词
高岭土
原矿
特征
Kaolinite,raw mineral,behaviour
