Articles | Volume 15, issue 6
https://doi.org/10.5194/nhess-15-1149-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/nhess-15-1149-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Hydrochemical characteristics of hot spring waters in the Kangding district related to the Lushan MS = 7.0 earthquake in Sichuan, China
Z. Chen
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
X. Zhou
CORRESPONDING AUTHOR
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
J. Du
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
C. Xie
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
L. Liu
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
Y. Li
CORRESPONDING AUTHOR
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
L. Yi
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
H. Liu
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
Y. Cui
CEA Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
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30 citations as recorded by crossref.
- Anomalies of gas molecular and isotopic compositions of terrestrial mud volcanoes caused by post-genetic processes - A case from the mud volcanoes in the Junggar Basin, northwest China Y. Wang et al. 10.1016/j.petrol.2020.107698
- Temporal variations in stable isotopes and synchronous earthquake-related changes in hot springs L. Zhang et al. 10.1016/j.jhydrol.2021.126316
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- Hydrogeochemical Characteristics of Hot Springs and Their Short-Term Seismic Precursor Anomalies along the Xiaojiang Fault Zone, Southeast Tibet Plateau C. Li et al. 10.3390/w13192638
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- The Analysis of Lithosphere–Atmosphere–Ionosphere Coupling Associated with the 2022 Luding Ms6.8 Earthquake J. Liu et al. 10.3390/rs15164042
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- Hydrogeochemistry of Hot Springs and the 2018 Mojiang M 5.9 Earthquake-Related Chemical Changes in the Simao Basin, China Q. Li et al. 10.3389/feart.2021.717680
- Hydrogeochemical origin and circulation of spring waters along the Karakorum fault, Western Tibetan Plateau: Implications for interaction between hydrosphere and lithosphere J. Wang et al. 10.3389/feart.2022.1021550
- Carbon isotope variations in inorganic carbon materials: Implications for mud volcanic carbon cycling in the northern Tianshan fold zone, Xinjiang, China Z. Chen et al. 10.1016/j.apgeochem.2018.07.018
- Earthquake-related hydrochemical changes in thermal springs in the Xianshuihe Fault zone, Western China B. Li et al. 10.1016/j.jhydrol.2019.124175
- Hydrogeochemistry and Precursory Anomalies in Thermal Springs of Fujian (Southeastern China) Associated with Earthquakes in the Taiwan Strait B. Wang et al. 10.3390/w13243523
- Effect of Large-Scale Mining Drainage on Groundwater Hydrogeochemical Evolution in Semi-Arid and Arid Regions A. Luo et al. 10.3389/fenvs.2022.926866
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- Reactive Transport Process of Earthquake‐induced Hydrochemical Changes in Guanding Thermal Spring, Western Sichuan, China J. NA et al. 10.1111/1755-6724.15121
- Stable isotopes and hydrogeochemical evolutions of groundwater from a typical seismic fault zone in the Mt. Lushan region, Eastern China Z. Bao et al. 10.3389/feart.2023.1285136
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Saved (final revised paper)
Latest update: 23 Nov 2024
Short summary
After the Lushan earthquake, Ca2+, HCO3- and TDS of spring water increased significantly, which may be attributed to the enhanced interaction between water and carbonate rocks by the increment of dissolved CO2. Na+, Cl- and SO42- in water from Guanding, Zheduotang, Xinxing and Gonghe springs decreased, which may be related to the dilution of precipitation water. The increase in Na+ and SO42- in water from Erhaoying spring may result from a greater increase in sulfur-rich groundwater.
After the Lushan earthquake, Ca2+, HCO3- and TDS of spring water increased significantly, which...
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