The aim of this study is to determine the effect of the layer charge of sme
ctites on their electrophoretic mobility (EM), using electrophoresis measur
ements. In order to cover the charge domain from 0 to 2 charges per unit st
ructural cell, two clay series were used: thermally treated Cu-montmorillon
ite (0-0.7) and synthetic saponites (0.7-2). All the studied samples are ne
gatively 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 acid
ic pH, the EM of smectites ranges from -3 to -0.4 10(-8) m(2) s(-1) V-1 whe
n the layer charge ranges from 0.8 to 2. High charge and low charge smectit
es, 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
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