首页> 外文会议>24th New Zealand Geothermal Workshop 2002 2002 Auckland >ENVIRONMENTAL EFFECTS OF VOLCANIC GASES ON REGIONAL RAINWATER CHEMISTRY AT KUJU, JAPAN
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ENVIRONMENTAL EFFECTS OF VOLCANIC GASES ON REGIONAL RAINWATER CHEMISTRY AT KUJU, JAPAN

机译:日本久久火山气体对区域雨水化学的环境影响

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Sampling and chemical analysis of rainwater at Kuju volcano were made for ten years from 1992 to examine the effects of volcanic gases on acidification of rainwater and the relationship with volcanic activity. Rainwaters in the near vicinity of the fumarolic area were acidified by HC1, H_2SO_4 and HF. Concentration of Cl~- quickly decreases with distance whereas that of SO_4~(2-) gradually decreases in spite of larger discharge rate of SO_2 relative to HC1 from the fumaroles. This implies that HCl preferentially dissolves into rainwater and deposits in the vicinity of the fumarole. Eruptive activity accompanying increase in discharge rates of acidic gases resulted in lowering pH of rainwater only in the near vicinity of fumarolic area. No appreciable effect was detected at distant places.
机译:从1992年开始,九州火山进行了十年的雨水采样和化学分析,以研究火山气体对雨水酸化的影响以及与火山活动的关系。富马酸区域附近的雨水被HCl,H_2SO_4和HF酸化。尽管SO_2相对于HC1从富马discharge的排放速率较大,但Cl〜-的浓度随距离而迅速降低,而SO_4〜(2-)的浓度却逐渐降低。这意味着HCl优先溶解在雨水中并沉积在喷气孔附近。伴随着酸性气体排放速率增加的爆发活动仅在富马酸地区附近导致雨水的pH值降低。在远处未检测到明显的影响。

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