JaLCDOI 10.18926/ESR/13908
フルテキストURL ESR_6_39.pdf
著者 Yamamoto Masahiro| Ichimoto Hideo| Komatsu Shinji| Yamashita Ruka|
抄録 Hydrogen and oxygen isotope rations of thermal waters from 46 spas in Okayama Prefecture range from -62.6 to -29.2% in δD and from -10.0 to -4.4% in δ18O, respectively. The isotope rations indicate that all but one of the thermal water in Okayama prefecture are meteoric in origin. The Ofuku thermal water is the only exception, which is probably a mixture of seawater and meteoric water with the ratio of about 1. Sulfur isotope rations of dissolvel sulfate in the thermal waters range from -6.2 ti 59.3% in δ34S. The high δ34S values observed in some thermal waters may be due to bacterial reduction of sulfate.
キーワード Hydrogen isotope ratio Oxygen isotope ratio Sulfur isotope ratio Thermal water Spa Okayama
出版物タイトル Okayama University Earth Science Report
発行日 1999-09-20
6巻
1号
開始ページ 39
終了ページ 44
ISSN 1340-7414
言語 English
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310408