The pseudo-first-order rate constants For ion exchange of partially si
lver ion exchanged Y zeolites (AgnNa56-nY) with sodium ions are determ
ined from chronoamperometric studies of zeolite-modified electrodes in
aqueous solution. In the case of AgnNa56-nY when n less than or equal
to 5.9 the electrochemical reduction of intrazeolite Ag+ cations is c
ontrolled by an intracrystalline ion-exchange process rather than by c
ounterdiffusion of exchanging cations through the interconnected super
cage system of the zeolite. Herein the methodology for analysis of thi
s situation is developed where the rate of the electrochemical reactio
n is equated with the velocity of the rate-limiting ion-exchange react
ion. Good agreement between theory and experiment was observed. The ps
eudo-first-order rate constant for Ag+ exchange with Na+ is relatively
insensitive to the concentration of sodium in the electrolyte solutio
n, but decreases as the silver loading in the zeolite is increased up
to 5.9 silver ions per unit cell. The data are consistent with electro
n transfer to silver ions occurring subsequent to the ion-exchange ste
p, confirming once again that electron transfer occurs outside of the
zeolite framework.