The solubility of hydrogen chloride in volcanic rock melts was experimentally determined at temperatures of 1200°C and 1290°C with the variation in the partial pressure of hydrogen chloride mixed with nitrogen under one atmosphere. The solubility of hydrogen chloride decreases not only with a rise in the temperature, but also with an increase in the silica content of volcanic rock melts, while it increases with an increase in the partial pressure of hydrogen chloride. The equilibrated concentration of chlorine obtained by experiments was compared with those in natural basalts collected from Japan and Hawaii.
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Iwasaki et al. (1967) studied this question.
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