Abstract

The present position of theoretical investigation of the water-content versus relative humidity isotherm is briefly indicated. Previous workers have anticipated an effect on equilibrium water-content arising from the mechanical properties of the keratin network. Such an effect is reported for supercontracted wool fibres and for reduced and S-methylated fibres, for which an increased saturation water-content is observed. In the case of S-methyl wool, saturation water-content shows little or no dependence on the number of disulphide cross-links, however it does depend on the number of S-methyl groups present. The results are considered in terms ofFlory-Huggins solution theory, and it is indicated that this theory can be usefully applied for relative humidities in excess of 85%. In normal wool “solution” absorption is permitted only in the noncrystalline component, but in supercontracted wool or S-methyl wool takes place in both components. Even when saturation water-content is greatly increased the isotherm is not appreciably changed below 85% R. H., indicating that no additional sites for strong binding of water become available; apparently all such sites are accessible in normal wool at approximately 85% relative humidity.

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