Abstract
THE nature of the forces giving rise to the intra-crystalline swelling of montmorillonite has been several times discussed. The recent work of Bradley1 and of myself2,3,4 on the swelling caused by adsorption of organic liquids enables us to get a clearer view of the problem, because these liquids form well-defined complexes in which the influence of the exchangeable ions is less marked than with water.
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