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It is shown that the moisture desorption isotherm of wheat can be interpreted in harmony with Cassie's theoretical assumptions regarding adsorption on localized sites by the equation[Formula: see text]where N is the number of adsorbed molecules per gram of wheat and S is the number of localized sites. Kf/(1 + Kf) is a Langmuir-type factor for adsorption of the low energy fraction of molecules, and K′fn is a factor for adsorption of the normally condensed fraction of molecules. In agreement with theory K′,n,and S are independent of temperature. The dependence of K on temperature gives a value of −6.27 kcal/mole for the partial molal enthalpy of dilution of the low energy fraction of molecules, which is in the order of magnitude of a hydrogen bond. The analysis also illuminates the practice of the drying of wheat. An exact correspondence appears to exist between the calculated values of S and the apparent surface (or equilibrium) moistures observed in studying the diffusion of moisture out of wheat. The theoretical relation[Formula: see text]is therefore given for predicting apparent surface moisture contents in the vacuum drying of wheat, where[Formula: see text]
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H. A. Becker (1958) studied this question.
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