Mercury Concentrations in Fumarolic Gas Condensates and Mercury Chemical Forms in Fumarolic Gases : Case Study on Satsuma-Iwojima Volcano

  • SAKAMOTO Hayao
    Department of Earth and Environmental Sciences, Faculty of Science, Kagoshima University
  • FUJITA Shun-ichi
    Department of Earth and Environmental Sciences, Faculty of Science, Kagoshima University
  • TOMIYASU Takashi
    Department of Earth and Environmental Sciences, Faculty of Science, Kagoshima University
  • ANAZAWA Katsuro
    Department of Earth and Environmental Sciences, Faculty of Science, Kagoshima University

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  • 噴気孔ガス凝縮水中の水銀含有量と噴気孔ガス中の水銀の化学形 : 薩摩硫黄島火山をケーススタディとして

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Abstract

The mercury concentrations in fumarolic gas condensates collected from volcanic areas in Hokkaido, Miyazaki, and Kagoshima Prefectures, Japan, were investigated. Mercury concentrations ranged from 0.12 to 135 μgl-1 in 44 collected samples. It was found that there was a positive correlation between mercury and chloride concentrations in fumarolic gas condensates collected from Satsuma-Iwojima Volcano, Kagoshima Prefecture. It was considered that the mercury in fumarolic gas was discharged in the form of mercury (I or II) chloride. However, the results from mercury chemical equilibrium calculations for the vapor in fumarolic gases indicated that mercury was discharged mainly in the form of metallic mercury vapor.

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