ION EXCHANGE CHARACTERISTICS OP A NEW MANGANESE OXIDE : SELF-DIFFUSION AND TRACE COMPONENT DIFFUSION

The kinetics of self-diffusion and trace component diffusion of Na+ and Cs+ in a new manganese oxide, having the chemical formula Na₄Mn₁₇O₂₇.13 H₂O, was studied. A uniform diffusion process was observed in all cases. The diffusion coefficients increase with particle size at the relatively large sizes, which is attributed to the conglomeration of small particles. The self-diffusion coefficient of Na+ is lower than that of Cs+ whereas the trace diffusion coefficients follow a reverse trend. Besides, the self-diffusion coefficients are not equal to the trace diffusion ones and opposite differences are observed for Na+ and Cs+. These results were tentatively explained in terms of the oxide water content and ion hydration.