摘要
120℃时膨润土、高岭土分别用水玻璃固化,固化物晶形仍以蒙脱石、高岭石结构为主,且蒙脱石可包含更多的水玻璃成分。其固化机理为水玻璃加强了这些硅酸盐的层间作用力,讨论了新型夹层物质形成的可能。
After bentonite and kaolin clay is hardened by water glass at 120℃ ,XRD measurement shows the crystal structure of hardened materials is similar to montmorillonite or halloysite.and montmorillonite can contain more water glass.It is suggested that a new interlayer material containing water glass have been prepared.
出处
《光谱实验室》
CAS
CSCD
1998年第4期8-11,共4页
Chinese Journal of Spectroscopy Laboratory