A three-dimensional swelling deformation of bentonite-sand mixtures is investigated. It is confirmed that the magnitude of volumetric strain
εv due to wetting depends mainly on mean principal stress
p regardless of principal stress ratio
R while the magnitude of deviator strain (
εa-
εr) induced by wetting depends on principal stress ratio
R regardless of mean principal stress
p. A linear relation exists between montmorillonite void ratio
em (defined as a ratio of water volume to montmorillonite volume) and mean principal stress
p in their log scales. This relation between montmorillonite void ratio
em and mean principal stress
p is independent of initial dry density, mixing rate of bentonite and sand, and principal stress ratio
R. In addition, there is a linear relation exists between deviator strain log(
εa-
εr) and principal stress ratio
R.
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