MISC

2017年

北八甲田火山群,新湯断層周辺における地熱熱水の化学特性と 貯留層温度の評価

日本地熱学会誌
  • 松田 雅司
  • ,
  • 鈴木 陽大
  • ,
  • 井岡 聖一郎
  • ,
  • 村岡 洋文

39
2
開始ページ
73
終了ページ
79
記述言語
日本語
掲載種別
DOI
10.11367/grsj.39.73
出版者・発行元
日本地熱学会

<p>The southwestern foot of the Hakkoda–Odake volcano has many geothermal manifestations where geothermal development has been limited by the Natural Parks Law. The current target area, which is classified as Class II special zone has been deregulated for individual geothermal development. We conducted an investigation to determine the chemical and isotopic characteristics of the hot waters around the Shinyu Fault and to estimate the temperature of the geothermal reservoir. According to our δD–δ<sup>18</sup>O diagram, the hot waters in the study area are meteoric in origin. In addition, the triangle diagram for Cl<sup>–</sup>, SO<sub>4</sub><sup>2–</sup>, and HCO<sub>3</sub><sup>– </sup>concentrations indicates that these hot waters can be classified as steam-heated waters and volcanic waters. The B/Cl and Br/Cl ratios show that the volcanic waters are diluted with shallow groundwater as they flow through Jigokunuma downstream to Shinyu. We estimated the geothermal reservoir temperature to be between approximately 150 and 160 °C, based on anhydrite geothermometry and the chloride–enthalpy mixing diagram.</p>

リンク情報
DOI
https://doi.org/10.11367/grsj.39.73
CiNii Articles
http://ci.nii.ac.jp/naid/130006182220

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