The uniformity of clay films affects the transport of an anionic elect
roactive probe through the film. When cations other than Na+ are prese
nt in the initial swelling of the him (such as native K+ and Ca2+), or
when the native clay is highly charged, internal dislocations of the
film, caused by variable stacking domains, enhance the diffusive trans
port of Fe(CN)(6)(3-) across the film. This effect is investigated usi
ng clay-modified electrodes in which the clays are of variable exchang
e forms (Na+, Ca2+, or K+) and variable charge. The charge on the clay
is determined both by the native form of the clay and by reduction of
structural Fe3+. The results suggest that swelling of clays increases
in a linear fashion with CEC, at least for minimally charged clays.