The roles of molecular structure and charge are examined in the transp
ort of cations within montmorillonite clay films. The series of Ru(NH3
)(6)(3+), Co(NH3)(3+), Co(sep)(3)(3+), Co(Sep)(3+) and Co(bpy)(3)(3+)
are examined in detail via electrochemical and spectrochemical methods
. The electrochemical signal is enhanced both in minimizing the time r
equired to develop the signal and in the magnitude of the signal for R
u(NH3)(6)(3+). In addition, the potential for the observed reduction p
eak is shifted negative and the current peak associated with reduction
disappears with rinsing of the clay film. These observations are char
acteristic of a compound that is held by simple electrostatic charge c
haracteristics. In contrast, the compounds Co(NH3)(3+), Co(en)(3)(3+)
and Co(sep)(3+), while showing rapid and enhanced signal development,
eventually evolve a signal that is diminished with respect to the bare
electrode, consistent with a hydrophobic mode of retention. The signa
l for Co(bpy)(3)(3+) is slow to be observed, is diminished with respec
t to the bare electrode: and is shifted positive in potential, all hal
lmarks of a strong, non-electrostatic mode of binding within the clay.