Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (6): 1815-1822.doi: 10.13278/j.cnki.jjuese.201606205

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Comparison Analysis of Co-Seismic Response Characteristics of Groundwater Level at Two Sides of Fault: A Case Study of Dahuichang Observation Wells in the Middle of Babaoshan Fault in Beijing

Song Yang1,2, Gu Hongbiao1, Li Haijun1,2, Chi Baoming1,2   

  1. 1. Department of Earthquake Science, Institute of Disaster Prevention, Sanhe 065201, Hebei, China;
    2. Institute of Engineering Mechanics of China Earthquake Administration, Harbin 150080, China
  • Received:2016-03-02 Online:2016-11-26 Published:2016-11-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41302198), Science Research Project of Hebei Provincial Department of Education(QN20132004) and Earthquake and Technology Spark Program of China Earthquake Administration(XH16059)

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Abstract: Earthquake often causes different co-seismic response of groundwater level in observation wells at two sides of the fault. The research on the difference of co-seismic response ability, groundwater level variation at different sides of the fault and its governing factors is helpful to reveal evolution process of fault zone permeability, to deepen understanding the response mechanism of groundwater level to earthquake, and to guide the layout of earthquake observation networks. This paper has made a try to analyze the times, form, amplitude and shock ability of co-seismic response of groundwater level to earthquake in the observation wells in upper and lower side of the middle section of Babaoshan fault zone in Beijing. The borehole pressure coefficient has been calculated with digital filter by trend removing and the tidal parameters have been calculated using Baytap-G program. The volumetric strain of the two aquifers where the observation well is located has also been inverted for the last 7 earthquakes and the permeability variation before and after the earthquake can thereby be discriminated. The results show that the co-seismic response of groundwater level to earthquake in these two observation wells is different and the co-seismic response times of groundwater level in upper side of the fault zone in Beijing has more times and stronger ability than that in lower side, which is in relation to fault belt shielding effect and the different variation of aquifer permeability where the observation well is located.

Key words: Babaoshan fault, well water level, cross-fault, co-seismic response

CLC Number: 

  • P641.7
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