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  4. Characterization of neutral fluids in the volcanic geothermal system under the Tatun Volcano Group, Taiwan
 
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Characterization of neutral fluids in the volcanic geothermal system under the Tatun Volcano Group, Taiwan

Journal
Journal of Geochemical Exploration
Journal Volume
278
Start Page
107814
ISSN
0375-6742
Date Issued
2025-11
Author(s)
Lu, Yi-Chia
Wang, Chyi
SHENG-RONG SONG  
PEI-LING WANG  
Song, Ting-Jui
Taguchi, Sachihiro
Peng, Tsung-Ren
LI-HUNG LIN  
Lee, Jian-Cheng
Li, Hong-Chun
DOI
10.1016/j.gexplo.2025.107814
URI
https://www.scopus.com/pages/publications/105010861689
https://scholars.lib.ntu.edu.tw/handle/123456789/731835
Abstract
The Tatun Volcano Group (TVG), located near the populated Taipei metropolitan area, is a promising geothermal energy source because of its active hydrothermal system. However, severe corrosion from acidic fluids hindered exploration in the 1970s. Given renewed global interest in renewable energy, this study examines the evolution and assesses the reservoir temperatures of neutral thermal fluids to mitigate corrosion-related challenges and facilitate geothermal exploration in the TVG. Water and carbonate samples were collected from hot springs, cores, cuttings, and outcrops along the TVG SW–NE corridor for geochemical analysis. A clumped isotope thermometer was used to calculate carbonate precipitation temperatures, combining stable water isotope analysis (18O and 2H), this approach provides carbonate clumped isotope composition-based reservoir temperatures of 181–276 °C in three areas. Distinct fluid origins and multiple chemical reactions across the depth (temperature) zones were identified. A geothermal model was generated to demonstrate the life cycle of non-strongly acidic fluids, from their deep origins to their upward migration and chemical interactions. Based on water and carbonate analyses, non-strongly acidic zones suitable for geothermal drilling have been identified in the active volcanic region of the TVG. Preliminary drilling data indicate that the vapor-dominated reservoirs in the TVG have significant potential for geothermal exploration and near-term development in conventional geothermal systems. This study further suggests that high-temperature, non-artesian well locations with carbonate deposits, which reflect a history of non-acidic environments, are excellent candidates for future enhanced geothermal systems, advanced geothermal systems, and superhot geothermal resource development.
Subjects
Clumped isotope thermometry
Geothermal system
Neutral hot fluid
Tatun
SDGs

[SDGs]SDG7

[SDGs]SDG13

[SDGs]SDG14

Publisher
Elsevier BV
Type
journal article

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