Layer charge and electrophoretic mobility of smectites

被引:116
作者
Thomas, F [1 ]
Michot, LJ [1 ]
Vantelon, D [1 ]
Montargès, E [1 ]
Prélot, B [1 ]
Cruchaudet, M [1 ]
Delon, JF [1 ]
机构
[1] Inst Natl Polytech Lorraine, CNRS, Lab Environm & Mineral, F-54501 Vandoeuvre Nancy, France
关键词
layer charge; smectites; electrophoretic mobility; Cu-montmorillonite; synthetic saponites;
D O I
10.1016/S0927-7757(99)00291-5
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The aim of this study is to determine the effect of the layer charge of smectites on their electrophoretic mobility (EM), using electrophoresis measurements. In order to cover the charge domain from 0 to 2 charges per unit structural cell, two clay series were used: thermally treated Cu-montmorillonite (0-0.7) and synthetic saponites (0.7-2). All the studied samples are negatively charged in a pH range from 2 to 12. Neither layer charge nor ionic strength influences the EM of smectites at neutral to alkaline pH. At acidic pH, the EM of smectites ranges from -3 to -0.4 10(-8) m(2) s(-1) V-1 when the layer charge ranges from 0.8 to 2. High charge and low charge smectites, which are not expandable, tend to aggregate in aqueous suspension, and the measured EM corresponds then to the amphoteric sites of the edge faces of the layer stacks. These sites are negatively charged at pH values above 3. (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:351 / 358
页数:8
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