Thermal Science 2023 Volume 27, Issue 1 Part B, Pages: 615-622
https://doi.org/10.2298/TSCI2301615Y
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Geothermal characteristics of the Xianshuihe fault zone and their engineering influence on tunnel construction
Yuan Dong (State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu, China + MOE Key Laboratory of Deep Earth Science and Engineering, Sichuan University, Chengdu, China + China Railway Eryuan Engineering Group Company, Ltd, Chengdu, China), xiaokun@stu.scu.edu.cn
Xiao Kun (State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu, China + MOE Key Laboratory of Deep Earth Science and Engineering, Sichuan University, Chengdu, China)
Feng Tao (China Railway Eryuan Engineering Group Company, Ltd, Chengdu, China)
Zhang Guang-Ze (China Railway Eryuan Engineering Group Company, Ltd, Chengdu, China)
Xu Zheng-Xuan (China Railway Eryuan Engineering Group Company, Ltd, Chengdu, China)
Wang Zhe-Wei (China Railway Eryuan Engineering Group Company, Ltd, Chengdu, China)
Yi Xiao-Juan (China Railway Eryuan Engineering Group Company, Ltd, Chengdu, China)
Lin Zhi-Heng (China Railway Eryuan Engineering Group Company, Ltd, Chengdu, China)
Zhang Zhi-Long (State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu, China + MOE Key Laboratory of Deep Earth Science and Engineering, Sichuan University, Chengdu, China)
Zhang Ru (State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu, China + MOE Key Laboratory of Deep Earth Science and Engineering, Sichuan University, Chengdu, China)
Qi Ji-Hong (College of Environment and Civil Engineering, Chengdu University of Technology, Chengdu, China)
The Zheduo Mountain tunnel crosses the Xianshuihe fault zone in Kangding
city. The Xianshuihe fault zone is composed of many large-scale faults and
features a complex geological structure and strong geothermal activity.
Based on geothermal drilling data, hydrogeological tests and the geothermal
geological back-ground of the study area obtained via hydrogeological
surveys and hydrogeo-chemical methods in the process of tunnel surveying,
this paper explores the exposure characteristics and distribution of
geothermal water in the study area, analyses its hydrogeochemical and
isotopic characteristics, and thoroughly studies the hydrogeological
structure of the geothermal water to explore the genetic mechanism
responsible for the formation of the geothermal water. The influence of the
geothermal water and high ground temperatures on tunnel construction is
further predicted, and practical and effective engineering treatment
suggestions are proposed.
Keywords: Xianshuihe fault zone, geothermal water, hydrogeochemistry, geothermometry
Show references
Tang, X., et al., Distribution and Genesis of the Eastern Tibetan Plateau Geothermal Belt, Western China, Environmental Earth Sciences, 76 (2016), 1, pp. 1-15
Zhang, J., et al., Geothermal Data Analysis at the High-Temperature Hydrothermal Area in Western Sichuan, Science China Earth Sciences, 60 (2017), 8, pp. 1507-1521
Tian, J., et al., Fluid Geochemistry and Its Implications on the Role of Deep Faults in the Genesis of High Temperature Systems in The Eastern Edge of the Qinghai Tibet Plateau, Applied Geochemistry, 131 (2021), 8, ID 105036
Liu, Q., et al., Near-Surface Geothermal Gradient Observation and Geothermal Analyses in the Xianshuihe Fault Zone, Eastern Tibetan Plateau, ACTA Geologica Sinica-English Edition, 91 (2017), 2, pp. 414-428
Hu, Y., et al., A Study on the Thermo-Mechanical Properties of Shotcrete Structure in a Tunnel, Excavated in Granite at Nearly 90 °C Temperature, Tunnelling and Underground Space Technology, 110 (2021), 4, ID 103830
Rybach, L., et al., Temperature Predictions and Predictive Temperatures in Deep Tunnels, Rock Mechanics and Rock Engineering, 27 (1994), 2, pp. 77-88
Wang, M., et al., A Study on the Heat Transfer of Surrounding Rock-Supporting Structures in High-Geothermal Tunnels, Applied Sciences, 10 (2020), 7, ID 2307
Li, X., et al., Hydrogeochemical Characteristics and Conceptual Model of the Geothermal Waters in the Xianshuihe Fault Zone, Southwestern China, International Journal of Environmental Research and Public Health, 17 (2020), 2, pp. 1-15
Zhang, Y., et al., Hydrochemical Characteristics and Multivariate Statistical Analysis of Natural Water System: A Case Study in Kangding County, Southwestern China, Water, 10 (2018), 1, pp. 1-17
Li, J., et al., Major Hydrogeochemical Processes Controlling the Composition of Geothermal Waters in the Kangding Geothermal Field, Western Sichuan Province, Geothermics, 75 (2018), 9, pp. 154-163
Luo, J., et al., Geothermal Potential Evaluation and Development Prioritization Based on Geochemistry of Geothermal Waters from Kangding Area, Western Sichuan, China, Environmental Earth Sciences, 76 (2017), 9, pp. 1-24
Yan, J., et al., Cooling Technology and Effect Analysis for High Geothermal Tunnel on Sichuan-Tibet Railway (in Chinese), China Railw. Sci. (China), 40 (2019), 5, pp. 53-62
Jiang, G. Z., et al., Compilation of Heat Flow Data in the Continental Area of China (in Chinese), 4th ed., Chinese Journal of Geophysics-Chinese Edition, 59 (2016), 8, pp. 2892-2910
Craig, H., Isotopic Variations in Meteoric Waters, Science, 133 (1961), 346, pp. 1702-1703
Ai, T., et al., Changes in the Structure and Mechanical Properties of a Typical Coal Induced by Water Immersion, International Journal of Rock Mechanics and Mining Sciences, 138 (2021), 2, ID 104597