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Liu Kai, Zhang Hui, Zhang Jun, Song Lei, Chen Yan’e, Xia Yan, Tian Zhaoyang, Hai Changhong. 2019: Comparative analysis on coseismic response of water level in Shandong Province to several major earthquakes. Acta Seismologica Sinica, 41(1): 69-79. DOI: 10.11939/jass.20170161
Citation: Liu Kai, Zhang Hui, Zhang Jun, Song Lei, Chen Yan’e, Xia Yan, Tian Zhaoyang, Hai Changhong. 2019: Comparative analysis on coseismic response of water level in Shandong Province to several major earthquakes. Acta Seismologica Sinica, 41(1): 69-79. DOI: 10.11939/jass.20170161
shu

Comparative analysis on coseismic response of water level in Shandong Province to several major earthquakes

  • 1.

    Dezhou Seismic Station of Shandong Earthquake Agency，Shandong Dezhou 253000，China

  • 2.

    Changyi Seismic Station of Shandong Earthquake Agency，Shandong Weifang 251300，China

  • 3.

    Earthquake Agency of Heze City，Shandong Heze 274026，China

  • 4.

    Earthquake Agency of Zaozhuang City，Shandong Zaozhuang 277800，China

More Information
  • Received Date: February 05, 2018
  • Revised Date: October 30, 2018
  • Available Online: January 05, 2019
  • Published Date: December 31, 2018
    Graphical Abstract
    • Abstract
  • In the form of multi-well to multi-earthquake, six wells with good coseismic responses in the underground fluid observation network of Shandong Province are selected to analyze the coseismic variations of water level caused by the Japan MW9.0 earthquake, the Sumatra MW8.6 earthquake and the Nepal MW7.8 earthquake. We analyze the characteristics in the aspects of type and amplitude, and discuss the response mechanism. The results show that the major type of coseismic variations is oscillation. With quantitative analysis, we find that the rise of Liaogu-1 water level is due to the increase of permeability coefficient of aquifer. The different types between Liaogu-1 well and Lu-27 well on the same fault zone are due to the different regional geological conditions and seismic activities. The water level coseismic variation type of Lu-07 well is affected by local tectonic stress. The amplitude of water level coseismic variation is related to the magnitude and the distance between well and epicenter, and also depends on the change of hydrogeological condition.
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    • References (39)
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