Sr Concentration and its Isotopic Ratio in the Sumikawa and Ohnoma Geothermal Fields

Junko Kamei, Hisao Kato, Akira Ueda, Osamu Okano, Masahiro Yamamoto

Research output: Contribution to journalArticle

2 Citations (Scopus)

Abstract

Concentrations and isotopic ratios of Sr were determined for waters and rocks in the Sumikawa and Ohnuma geothermal fields to provide constraints on modeling fluid movement and understanding water-rock interaction. The results are summarized as follows: 1) 87Sr/ 87Sr ratios of Quaternary volcanic rocks in the Sumikawa section (< 0.7041) are significantly lower than those of Tertiary marine sediments (≦ 0.7075). As a result, 87Sr/86Sr ratios of rocks increase northward where marine sediments distribute predominantly. 2) The Sr isotopic ratios of the geothermal fluids and hot spring waters are affected significantly by : their surrounding rocks, Particularly, geothermal fluids discharged from the Sumikawa wells have similar 87Sr/86Sr ratios to rocks around the feed zones, indicating an attainment of water-rock equilibrium in the vicinity of the wells. 3) A meaningful relationship between the concentration of Sr and Ca, and temperature in the reservoir fluid indicates that the fluid is saturated with respect to anhydrite : this conclusion is supported by a chemical equilibrium model. 4) 87Sr/86Sr ratios of geothermal fluids discharged from the Sumikawa production well, SC-1, have been changing temporally over the past four years. This may be due to a boiling of fluid in reservoir, return of reinjection water, and change of flow path of fluid discharging into reservoir.

Original languageEnglish
Pages (from-to)379-390
Number of pages12
JournalJournal of the Geothermal Research Society of Japan
Volume21
Issue number4
DOIs
Publication statusPublished - Jan 1999

ASJC Scopus subject areas

  • Geophysics

Fingerprint Dive into the research topics of 'Sr Concentration and its Isotopic Ratio in the Sumikawa and Ohnoma Geothermal Fields'. Together they form a unique fingerprint.

  • Cite this