Abstract

Abstract The effects of pH and clay film loading (thickness) on the electrochemistry of Fe(bpy)2+3, An− ion pairs (An− = CH3CO−2, CCl3CO−2, SO2−4) and Ru(NH3)3+6 exchange cations in montmorillonite- and laponite-modified graphite electrodes are investigated. Included in the study is the effect of pH on the activity of Fe(CN)3−6 anions in a clay film. We find that the number of surface-bound Fe(bpy)2+3, An− ion pairs capable of accessing the electrode surface decreases with increasing acidity, with the more basic CH3CO−2 counter-anions exhibiting the greater pH dependence. In contrast, the electroactivity of Ru(NH3)3+6 exchange ions intercalated in the gallery regions of the clay film is pH independent. Also, the fraction of electroactive Fe(bpy)2+3, An− ion pairs is essentially independent of clay film loading, indicating that the electroactive sites are confined to a narrow region of the film close to the electrode surface. However, the electroactivity of the more mobile Ru(NH3)3+6 exchange ions increases with film loading. Fe(CN)3−6 anions are easily displaced from a clay film by washing, but at pH 3.0–4.0 the complex anion decomposes to give a cyclic voltamogram indicative of Prussian blue (Fe3[Fe(CN)6]2) deposited on the clay surface. These differences in electrochemical behavior for Fe(bpy)2+3, An− ion pairs, Ru(NH3)3+6 exchange cations and Fe(CN)3−6 anions are inconsistent with the clay-layer protonation mechanism proposed previously to explain the decrease in electrochemical activity with decreasing pH for Ru(bpy)2+3, SO2−4 and K+,Fe(CN)3−6 salts at clay-modified electrodes. Instead, the pH dependence for M(bpy)2+3 species is most likely due to changes in the degree of ion-pair formation caused by the protonation of the An− counter-ions. These results, together with those of earlier studies, provide insights regarding the electrochemical accessibility of redox active species in clay-modified electrodes.

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