Abstract
A simple technique is developed which, for the first time, has enabled the experimental determination of the amount and composition of substances adsorbed from solution by microporous solids. The experimental results determined for the system [ethanol(1)-water(2)]/silicalite show considerable discrepancies with the predictions based on the available theories of adsorption from solution. These discrepancies are traced to the a priori assumption of no volume (or area) change of mixing inherent in the proposed theories. The experimental determination of the (individual) adsorption isotherms enables, for the first time, the calculation of the activity coefficients and the molar excess Gibbs free energy of the adsorbed phase independent of any a priori assumption other than the existence of a distinct adsorbed phase. For the system [ethanol(1)-ater(2)]/silicalite, the activity coefficients show considerable negative deviations from ideality and the molar excess Gibbs free energy is a strong function of spreading pressure as well as composition of the asorbed phase.
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