論文

査読有り 筆頭著者 国際誌
2019年5月

The nature and source of the volcanic ash during the 2015 small phreatic eruption at Hakone volcano, central Japan

Geochemical Journal
  • Muga Yaguchi
  • ,
  • Takeshi Ohba
  • ,
  • Masakazu Sago

53
3
開始ページ
209
終了ページ
217
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.2343/geochemj.2.0560
出版者・発行元
GEOCHEMICAL SOC JAPAN

On June 29, 2015, a small phreatic eruption occurred in the Owakudani geothermal area on Hakone volcano, central Japan. Ashfall was observed on June 29 and 30. In this study, constituent minerals, whole-rock composition, and watersoluble components of the ash sampled at the Owakudani geothermal area on June 30 were analyzed to determine the source depth and hydrothermal condition of this ash.The ash sample included smectite, pyrite, tridymite cristobalite, gypsum, and anhydrite with plagioclase and quartz, indicating that the ash was discharged from a relatively low- temperature (lower than 100-150 degrees C) and a near-neutral part of a hydrothermal alteration zone of the Owakudani geothermal area. The whole-rock chemical composition was characterized by an elevated Al2O3 content, supporting the inference that the source of the ash was in a near-neutral hydrothermal condition. Comparison of the mineral assemblage of the ash with that of the drilling core of the steam well evidently showed that the source depth of this ash was shallower than 350 m, as smectite is a mineral predominantly found at depths shallower than 350 m. In the ash leachate, 12,200 mg/kg of Cl and 6,600 mg/kg of SO4 were detected and their origin was deduced to be thermal water adhesion rather than volcanic gas because of their large adhesion amount and high Cl/S molar ratio. This Cl/S ratio corresponds to that of thermal waters approximately 23-351 m deep. This depth range is consistent with the lower limit depth estimated from the mineral assemblage.

リンク情報
DOI
https://doi.org/10.2343/geochemj.2.0560
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000517762600004&DestApp=WOS_CPL
URL
https://www.terrapub.co.jp/journals/GJ/abstract/5303/53030209.html
ID情報
  • DOI : 10.2343/geochemj.2.0560
  • ISSN : 0016-7002
  • eISSN : 1880-5973
  • Web of Science ID : WOS:000517762600004

エクスポート
BibTeX RIS