摘要
累托石是二八面体云母层与蒙脱石层1:1规则间层矿物。本文阐明累托石矿物结晶构造与阳离子交换性能的关系。阳离子交换性能在累托石定量与定性、改型、合成交联累托石和有机累托石等方面的应用。并介绍氧化钛交联累托石和在机累托石的有关特性。
The rectorite is a regular interstratified mineral consisting of dioctahedron muscovite-like and montmorillonite-like layer in 1: 1 ratio. In this paper following questions are discussed the relation of structure of rectorite crystal and property of cation exchange,the application of property of cation exchange for quantitative or qualitative determination,and for structure exchange of rectorite and for syntheses of TiO_2-cross-linked or organophilic rectorites. The properties of TiO_2-cross-linked or organophilic rectorite are described.
出处
《矿物岩石》
CAS
CSCD
1992年第1期96-101,共6页
Mineralogy and Petrology
关键词
累托石
阳离子交换
性能
应用
rectorite
cation exchange capacity
structure change
TiO_2-cross-linked rectorite
organophilic rectorite
