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Sun F X，Cui Y J，Wang H Y，Li J，Du J G. 2020. Hydrochemical types and origins analysis of groundwater at the seismic monitoring stations in Liaoning Province. Acta Seismologica Sinica，42（1）：79−90. doi：10.11939/jass.20190091. DOI: 10.11939/jass.20190091
Citation: Sun F X，Cui Y J，Wang H Y，Li J，Du J G. 2020. Hydrochemical types and origins analysis of groundwater at the seismic monitoring stations in Liaoning Province. Acta Seismologica Sinica，42（1）：79−90. doi：10.11939/jass.20190091. DOI: 10.11939/jass.20190091
shu

Hydrochemical types and origins analysis of groundwater at the seismic monitoring stations in Liaoning Province

  • 1.

    Institute of Earthquake Forecasting，China Earthquake Administration，Beijing 100036，China

  • 2.

    Key Laboratory of Earthquake Prediction，China Earthquake Administration，Beijing 100036，China

  • 3.

    School of the Earth Science and Resources，China University of Geosciences （Beijing），Beijing 100083，China

  • 4.

    Liaoning Earthquake Agency，Shenyang 110000，China

  • 5.

    Institute of Disaster Prevention，Sanhe，Hebei 065201，China

More Information
  • Received Date: May 16, 2019
  • Revised Date: November 25, 2019
  • Available Online: March 25, 2020
    Graphical Abstract
    • Abstract

  • The hydrochemical types and origins of underground waters collected from 15 seismic monitoring stations in Liaoning Province are discussed based on the isotope ratios of hydrogen and oxygen as well as ion concentrations. δD and δ18O values of underground water ranged from −82.5‰ to −54.4‰ and from −11.4 ‰ to −7.3‰, respectively, which indicates that the waters had a meteoric origin. Granite is widely distributed in the studied area. The cold spring waters were the type of Ca-SO4·HCO3 and Ca-HCO3·SO4, while the hot spring waters from fractured granite were mainly type of Na-HCO3·SO4 due to the dissolution of silicate minerals. The water samples with moderate temperature in the western and middle parts of Liaoning Province were the type of Na·Ca-HCO3, resulting from dissolution of silicate minerals and carbonate. The concentration of F − is positively correlated with temperature, pH, concentrations of Na＋ and HCO3 −, indicating reaction between the granite and the fluids enriched in CO2 .

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