The diffusion coefficients of potassium chloride and sodium chloride were measured in concentrated, saturated, and supersaturated solutions at 25°C employing Gouy interferometry. The results indicate a maximum in the diffusivity vs. concentration curve near saturation followed by a rapid decline in diffusivity toward zero with increasing concentration in the supersaturated region. This behavior supports the idea that the diffusion coefficient approaches zero at the spinodal concentration. The data were successfully correlated by modifying an empirical activity coefficient equation (Robinson and Stokes, 1955) to account for molecular cluster effects and employing the calculated activity coefficients along with a predictive equation for diffusivity in electrolytes (Robinson and Stokes, 1955
SCOPEThe study of diffusion coefficients in supersaturated solutions is of fundamental importance in understanding the mechanisms of diffusion and of crystal growth from solution. Virtually no data of this kind exist, however, resulting in the use of values obtained through the extrapolation of undersaturated diffusivity data into the supersaturated range. Sorell and Myerson (1982) demonstrated that diffusion coefficients obtained through extrapolation could be seriously in error. They measured the diffusivity of urea in supersaturated aqueous solutions and compared the results with those obtained through extrapolation of existing data. The experimental results showed a very rapid decline in the diffusion coefficient with increasing concentration in the supersaturated region. Differences of up to several hundred percent between the experimental and extrapolated data were reported. The purpose of this study is to: (1) experimentally measure diffusion coefficients in the electrolyte systems potassium chloride-water and sodium chloride-water at concentrations in the supersaturated region; (2) correlate the diffusion data through modification of existing relations for concentrationdependent diffusion in electrolytes; and (3) determine whether the rapid decline in diffusivity with increasing concentration in the supersaturated region observed in the urea-water system is observed in other systems.
CONCLUSIONS AND SIGNIFICANCEThe diffusion coefficients of potassium chloride in water at 25°C were measured at concentrations ranging from 0.7-4.23 M. Experimental results in the undersaturated region were consistent to within f 3 % of those of Costing (1950). Results show a maximum in the diffusivity vs. concentration curve near saturation (4.09 M) followed by a rapid decline in the diffusivity with increasing concentration in the supersaturated region,The diffusion coefficients of sodium chloride in water at 25°C were measured at concentrations ranging from 0.1-5.46 M. Experimental results in the supersaturated region were consistent to within f 3 % of those reported by Rand and Miller (1979). A maximum in diffusivity in the region of saturation followed by a rapid drop of diffusivity with increasing concentration was also observed.It is ...