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Deep Meteoric Water Circulation and Magmatic Fluid Discharge at an Active Volcano

Research Project

Project/Area Number 07640572
Research Category

Grant-in-Aid for Scientific Research (C)

Allocation TypeSingle-year Grants
Section一般
Research Field Meteorology/Physical oceanography/Hydrology
Research InstitutionKYOTO UNIVERSITY

Principal Investigator

KITAOKA Koichi  Kyoto University Faculty of Science Assoc.Prof., 理学部, 助教授 (30093230)

Co-Investigator(Kenkyū-buntansha) OHSAWA Shinji  Kyoto University Faculty of Science Res.Assoc., 理学部, 助手 (00201608)
YUSA Yuki  Kyoto University Faculty of Science Prof., 理学部, 教授 (90025403)
大沢 信二  京都大学, 理学部, 助手 (30243009)
Project Period (FY) 1995 – 1996
Project Status Completed (Fiscal Year 1996)
Budget Amount *help
¥2,300,000 (Direct Cost: ¥2,300,000)
Fiscal Year 1996: ¥700,000 (Direct Cost: ¥700,000)
Fiscal Year 1995: ¥1,600,000 (Direct Cost: ¥1,600,000)
KeywordsActive volcano / Fumarole / Magmatic steam / Stable isotope / Tritium / Geothermal water / Subsurface boiling / Deep water circulation / 火山性流体 / 相変化 / 温泉 / マグマ水 / 蒸気分離 / 臨界点 / 九重硫黄山
Research Abstract

Significant subsurface boiling of the deep circulating geothermal waters in Kuju-Iwoyama Volcano, Kyushu, Japan, was demonstrated by the hydrogen and oxygen isotopic study of hot spring waters and fumarolic steam condensates.
(1) Single-stage and continuous steam separations result in greatly different chloride and isotope contents of remaining liquid. Because of phase separation at high temperatures, deuterium contents of hot spring arehigher than those recharge waters, and part of the observed oxygen isotope shift may be due to boiling as well as water-rock reactions. The highest contents of chloride, oxygen-18 and deuterium observed in hot spring waters are considered to have resulted from boiling at shallow levels under single-stage steam separation of deep thermal water at its critical point. The lower contents of chloride, oxygen-18 and deuterium may have resulted from boiling under multi-stage steam separation of thermal waters, coupled with dilution with meteoric waters.
(2) Thus … More , we proposed that part of meteoric water is heated to the critical point of water during a hydrologic cycle through the volcano, forming a single-phase seam. The linear deltaD-delta^<18>O,deltaD-Cl, and delta^<18>O-Cl relationships for fumarolic condensates appear to have resulted from mixing at depths of the volcano between a magmatic steam and the super-critical steam of meteoric water origin.
(3) The tritium contents in fumarolic condensates suggest a short residence time (within about 6 years) of meteoric water circulating in the steam region, while those in hot spring waters are corresponded to a very long residence time over 100 years for the liquid region. The fumarolic discarge, therefore, is considered to be from the main water circulation system containing a vapor-dominated zone in the volcano and the hot spring discharge must be from the subsystem of liquid water circulation surrounding the vapor-dominated system.
(4) A sulfur hydrolysis in high temperature solution may occur as a possible mechanism of the formation of strongly sulfuric acid in the hot spring water. The new geothermometer for strongly acidic hot spring water by using its main chemical composition was developed by hydrothermal experiments of anhydrite-water system. Less

Report

(3 results)
  • 1996 Annual Research Report   Final Research Report Summary
  • 1995 Annual Research Report
  • Research Products

    (11 results)

All Other

All Publications (11 results)

  • [Publications] 北岡豪一 ほか: "九重硫黄山における噴気と温泉水のトリチウム濃度" 大分県温泉調査研究会報告. 47号. 21-28 (1996)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1996 Final Research Report Summary
  • [Publications] 北岡豪一 ほか: "九重硫黄山における深部循環熱水の沸騰による化学及び同位体組成の変化" 温泉科学. 46・4. 156-175 (1996)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1996 Final Research Report Summary
  • [Publications] 大上和敏 ほか: "強酸性熱水用地化学温度計の開発" 温泉科学. 46・2. 87-98 (1996)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1996 Final Research Report Summary
  • [Publications] K.Kitaoka, S.Ohsawa, Y.Yusa and M.Kusakabe: "Changes in chemical and isotopic compositions of deep geothermal waters through subsurface boiling at Kuju-Iwoyama Volcano, Central Kyushu, Japan." Journal of the Balneological Society of Japan. 46-4. 156-175 (1996)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1996 Final Research Report Summary
  • [Publications] K.Kitaoka, S.Ohsawa and K.Oue: "Deep meteoric water circulation at Kuju-Iwoyama Volcano from the viewpoint of tritium." Reports of Oita Prefecture Hot Spring Research Society. 47. 21-28 (1996)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1996 Final Research Report Summary
  • [Publications] K.Oue, S.Ohsawa, Y.Yusa and T.Kawano: "A new chemical geothermometer for strongly acidic hydrothermal water." Journal of the Balneological Society of Japan. 46-2. 87-98 (1996)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1996 Final Research Report Summary
  • [Publications] 由佐悠紀: "伽藍岳の地熱調査(2)" 大分県温泉調査研究会報告. 47. 7-12 (1996)

    • Related Report
      1996 Annual Research Report
  • [Publications] 北岡豪一: "九重硫黄山における噴気と温泉水のトリチウム濃度" 大分県温泉調査研究会報告. 47. 21-28 (1996)

    • Related Report
      1996 Annual Research Report
  • [Publications] 大上和敏: "強酸性熱水用地化学温度計の開発" 温泉科学. 46-2. 87-98 (1996)

    • Related Report
      1996 Annual Research Report
  • [Publications] 北岡豪一: "九重硫黄山における深部循環熱水の沸騰による化学及び同位体組成の変化" 温泉科学. 46-4. 156-175 (1996)

    • Related Report
      1996 Annual Research Report
  • [Publications] 大沢信二: "霧島火山群の噴気不活性ガス組成" 温泉科学. 45. 290-294 (1995)

    • Related Report
      1995 Annual Research Report

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Published: 1995-04-01   Modified: 2016-04-21  

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