Institutional Repository of Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences
| Earthquake-induced impulsive release of water in the fractured aquifer system: Insights from the long-term hydrochemical monitoring of hot springs in the Southeast Tibetan Plateau | |
Tian, Jiao1; Zhou, Xiaocheng1; Yan, Yucong1; He, Miao1; Li, Jingchao1; Dong, Jinyuan1; Liu, Fengli1; Ouyang, Shupei1; Li, Ying1; Tian, Lei2; Wang, Yingchun3; Huang, Tianming4 ; Pang, Zhonghe4
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| 2023 | |
| Source Publication | APPLIED GEOCHEMISTRY
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| ISSN | 0883-2927 |
| Volume | 148Pages:16 |
| Abstract | The outpouring hot spring water is deep circulated groundwater and its chemical constituents act as information carriers of the hydrological setting, including the recharge source, circulation path, and reservoir properties. However, the temporal variation in hydrochemical components and their inducing mechanisms remain to be elucidated. In this study, hot springs along the Anninghe-Zemuhe Fault, a controlling fault on the eastern edge of the Tibetan Plateau, were investigated. According to the spatial chemical variations of the sixteen hot springs and the two-year hydrochemical monitoring results of four hot springs, the aquifers in such fault-controlled regions exhibit heterogeneous anisotropy and elastic properties. Earthquake activities were found to play a significant role in both spatial and temporal changes in chemical compositions. We found that the waters with the highest reservoir temperatures (-100 degrees C) and deepest circulation depth (-3 km) outcropped in the north of the fault, where earthquakes occur more intensively, deeply, and stronger than those in other parts of the fault. During the stress accumulating and releasing processes in the earthquake sequence, the fractured aquifer systems are elastic and subject to impulsive mixing with subordinate fracture waters which induced hydrochemical changes at different levels. The chemical constituents responded to seismic energy densities as low as 6.5 x 10-4 J/m3, showing superiority over the groundwater monitoring wells. However, earthquakes that occurred in a tectoni-cally independent area or with an inappropriate stress loading-unloading direction could fail to trigger a distinguishable mixing process with apparent chemical fluctuations. These findings provide insights into the hydrochemical response to earthquakes in orogenic areas and further draw attention to hydrochemical changes in hot spring waters in seismic studies. |
| Keyword | Hot springs Hydrochemical characteristics Earthquake-induced response Eastern edge of the Tibetan Plateau |
| DOI | 10.1016/j.apgeochem.2022.105553 |
| Funding Organization | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Project ; National Key Research and Development Project ; Central Public -interest Scientific Institution Basal Research Fund ; Central Public -interest Scientific Institution Basal Research Fund ; IGCP Project ; IGCP Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Project ; National Key Research and Development Project ; Central Public -interest Scientific Institution Basal Research Fund ; Central Public -interest Scientific Institution Basal Research Fund ; IGCP Project ; IGCP Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Project ; National Key Research and Development Project ; Central Public -interest Scientific Institution Basal Research Fund ; Central Public -interest Scientific Institution Basal Research Fund ; IGCP Project ; IGCP Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Project ; National Key Research and Development Project ; Central Public -interest Scientific Institution Basal Research Fund ; Central Public -interest Scientific Institution Basal Research Fund ; IGCP Project ; IGCP Project |
| WOS Keyword | GEOTHERMAL WATERS ; ANNINGHE FAULT ; HYDROTHERMAL SYSTEMS ; MINERAL EQUILIBRIA ; GROUNDWATER LEVEL ; CHEMICAL-CHANGES ; WESTERN SICHUAN ; EASTERN MARGIN ; HEAT-FLOW ; CHEMISTRY |
| Language | 英语 |
| Funding Project | National Natural Science Foundation of China[42130809] ; National Natural Science Foundation of China[41902252] ; National Natural Science Foundation of China[42073063] ; National Key Research and Development Project[2017YFC1500501] ; National Key Research and Development Project[2019YFC1509203] ; National Key Research and Development Project[2019YFC0604901] ; National Key Research and Development Project[2020IEF0703] ; National Key Research and Development Project[2021IEF0602] ; National Key Research and Development Project[2021IEF0101] ; Central Public -interest Scientific Institution Basal Research Fund[CEAIEF20220507] ; Central Public -interest Scientific Institution Basal Research Fund[CEAIEF20220213] ; Central Public -interest Scientific Institution Basal Research Fund[CEAIEF2022030205] ; IGCP Project[724] |
| Funding Organization | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Project ; National Key Research and Development Project ; Central Public -interest Scientific Institution Basal Research Fund ; Central Public -interest Scientific Institution Basal Research Fund ; IGCP Project ; IGCP Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Project ; National Key Research and Development Project ; Central Public -interest Scientific Institution Basal Research Fund ; Central Public -interest Scientific Institution Basal Research Fund ; IGCP Project ; IGCP Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Project ; National Key Research and Development Project ; Central Public -interest Scientific Institution Basal Research Fund ; Central Public -interest Scientific Institution Basal Research Fund ; IGCP Project ; IGCP Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Project ; National Key Research and Development Project ; Central Public -interest Scientific Institution Basal Research Fund ; Central Public -interest Scientific Institution Basal Research Fund ; IGCP Project ; IGCP Project |
| WOS Research Area | Geochemistry & Geophysics |
| WOS Subject | Geochemistry & Geophysics |
| WOS ID | WOS:000915267700001 |
| Publisher | PERGAMON-ELSEVIER SCIENCE LTD |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.iggcas.ac.cn/handle/132A11/106837 |
| Collection | 页岩气与地质工程院重点实验室 |
| Corresponding Author | Zhou, Xiaocheng |
| Affiliation | 1.China Earthquake Adm, Inst Earthquake Forecasting, Beijing 100036, Peoples R China 2.China Earthquake Networks Ctr, Beijing 100045, Peoples R China 3.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610059, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
| Recommended Citation GB/T 7714 | Tian, Jiao,Zhou, Xiaocheng,Yan, Yucong,et al. Earthquake-induced impulsive release of water in the fractured aquifer system: Insights from the long-term hydrochemical monitoring of hot springs in the Southeast Tibetan Plateau[J]. APPLIED GEOCHEMISTRY,2023,148:16. |
| APA | Tian, Jiao.,Zhou, Xiaocheng.,Yan, Yucong.,He, Miao.,Li, Jingchao.,...&Pang, Zhonghe.(2023).Earthquake-induced impulsive release of water in the fractured aquifer system: Insights from the long-term hydrochemical monitoring of hot springs in the Southeast Tibetan Plateau.APPLIED GEOCHEMISTRY,148,16. |
| MLA | Tian, Jiao,et al."Earthquake-induced impulsive release of water in the fractured aquifer system: Insights from the long-term hydrochemical monitoring of hot springs in the Southeast Tibetan Plateau".APPLIED GEOCHEMISTRY 148(2023):16. |
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