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EARTHQUAKE ›› 2015, Vol. 35 ›› Issue (2): 133-138.

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Temporal Characteristics of the Tectonic Stress Field of Zhangbo Belt Area based on Digital Water Level

DING Feng-he1, HA Yuan-yuan2, WANG Yong1, WEI Jian-ming1, HAN Xiao-lei1, WANG Jian-ying1, MA Yi3, ZHOU Xiao-long4   

  1. 1. Earthquake Administration of Inner Mongolia Autonomous Region, Hohhot 010010, China;
    2. Transportation College of Inner Mongolia University, Hohhot 010020, China
  • Received:2014-09-25 Online:2015-04-30 Published:2020-06-24

Abstract: We selected digital water level and corresponding air pressure data of 6 wells in the Zhangbo Belt area, which are continuous, stable and with obvious solid tide since 2008. These wells are Changping station well, Shunyi Banqiao well, Baodi well, Xinzhuang well, Yutian(03) well, Dahuichang well etc. We obtained porosity and volume compression coefficient between solid skeleton and water under undrained condition by the barometric efficiency and M2 tidal factor smooth fitting. In horizontally layered one-dimensional aquifer mode, making use of partial aquifer parameters (porosity, water and solid skeleton volume compression coefficient), relationship between water level variation and aquifer vertical stress, we quantitatively analyzed the dynamic change process of tectonic stress field of the Zhangbo Belt area. The results show that Zhangbo Belt area has continued with stress enhancement activities in recent years.

Key words: Tectonic stress field, Digital water level, Temporal characteristics, The Zhangbo Belt area

CLC Number: