Abstract
This paper describes experiments on the conditions of deliquescence of the crystalline salts found in dust records from the air, and has a bearing on the formation of haze, fog, and condensation from the air. The possibility of identifying the nature of such salts when in very minute particles, so small that micro-chemical and crystallographic methods cannot be used, is indicated, the method being based upon the vapour pressure of deliquescence.
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21 articles.
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