日本地球惑星科学連合2025年大会

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セッション記号 A (大気水圏科学) » A-HW 水文・陸水・地下水学・水環境

[A-HW30] 同位体水文学2025

2025年5月30日(金) 10:45 〜 12:15 展示場特設会場 (2) (幕張メッセ国際展示場 7・8ホール)

コンビーナ:安原 正也(立正大学地球環境科学部)、中村 高志(山梨大学大学院・国際流域環境研究センター)、柏谷 公希(京都大学大学院工学研究科)、浅井 和由(株式会社 地球科学研究所)、座長:柏谷 公希(京都大学大学院工学研究科)、浅井 和由(株式会社 地球科学研究所)、森川 徳敏(産業技術総合研究所 活断層・火山研究部門)

11:10 〜 11:25

[AHW30-06] Developing a Hydrothermal Index based on geochemical properties of groundwater to Reveal Hidden Geothermal Signatures

*Mochamad Iqbal1,2Koki Kashiwaya1Katsuaki Koike1 (1.Kyoto University、2.Institut Teknologi Sumatera)

キーワード:hidden geothermal system, geochemistry, hydrothermal index, trace element

Hidden geothermal systems, which lack surface manifestations such as hot springs or fumaroles, remain difficult to detect yet hold considerable potential for low–carbon energy development. This study proposes a geochemical approach to identifying these concealed resources through a trace element analysis of groundwater, with developing a Hydrothermal Index (HI) that integrates normalized concentrations of elements commonly enriched in geothermal fluids (e.g., Cl, Li, B, As, Cs, and Rb). Groundwater samples were collected from multiple locations in a region suspected of harboring a hidden geothermal system and analyzed by inductively coupled plasma mass spectrometry (ICP-MS). Our results reveal several sites with elevated HI values, i.e., significantly above the background, suggesting the ascent of deep geothermal fluids and mixing with shallow groundwater. Some of these elements (notably As) also indicate concerns about environmental quality, underscoring the dual importance of resource exploration and water quality monitoring. Spatial mapping of the HI highlights potential zones of the geothermal system and guides further investigation into reservoir properties and drilling targets. By demonstrating the effectiveness of trace element signatures and the HI, this work offers a practical method for uncovering hidden geothermal systems. Such identification is critical not only for expanding renewable energy portfolios but also for assessing possible environmental risks associated with fluid mixing in shallow aquifers. Ultimately, the approach outlined here can support sustainable geothermal development and contribute to global efforts to reduce carbon emissions.
This study was supported by JSPS KAKENHI (Grant Nos. 23K26602 and 21KK0090) and Joint Research Grant for the Environmental Isotope Study of Research Institute for Humanity and Nature.