Abstract
With a method previously described, the adsorption of air on glass is measured as a function of temperature. If the temperature be increased, it is found that the thickness of the adsorbed layer as measured by this method, decreases slowly. The rate of this decrease in thickness is not as great as was previously found when the adsorption of air on rock-salt crystal was measured under the same conditions by the same method. It was further found that there was an "ageing" effect of adsorption of air on glass.

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