Expansion and contraction of clays in contact with solvents have been
often attributed to the influence exerted by the dielectric constant (
is-an-element-of) of the solvent on the equilibrium distance between c
lay plates. None of the models based on this assumption offers a unive
rsal treatment of the relationship between solvent properties and swel
ling. It is suggested that the swelling of clays may be described by a
n extension of the regular solution theory. Of 11 solvents tested, swe
lling of a mixed layer illite/smectite was greatest in N-methylformami
de but that of a Na-montmorillonite was greatest in water, contradicti
ng the assertion that swelling is correlated with solvent is-an-elemen
t-of. Permeability of beads of spray-dried Cu-montmorillonite (r = 3.5
mum) to hexane-2-propanol, 2-propanol-methanol, and methanol-water mi
xtures was measured by pumping the solvents at a rate of 1 mL/min thro
ugh an HPLC column. The highest intrinsic permeability (k) was observe
d in 2-propanol with lower k values in mixtures of both higher and low
er is-an-element-of.