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累托石的阳离子交换性能及其应用研究
引用本文:陈济美. 累托石的阳离子交换性能及其应用研究[J]. 矿物岩石, 1992, 12(1): 96-101
作者姓名:陈济美
作者单位:湖北省地质实验研究所 武汉
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。

关 键 词:累托石 阳离子交换 性能 应用

STUDY ON PROPERTY OF CATION EXCHANGE OF RECTORITE AND ITS APPLICATION
Chen Jimei. STUDY ON PROPERTY OF CATION EXCHANGE OF RECTORITE AND ITS APPLICATION[J]. Journal of Mineralogy and Petrology, 1992, 12(1): 96-101
Authors:Chen Jimei
Abstract: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.
Keywords:rectorite  cation exchange capacity  structure change  TiO_2-cross-linked rectorite  organophilic rectorite  
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