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EARTHQUAKE ›› 2008, Vol. 28 ›› Issue (2): 131-138.

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Discussion on variation mechanism of water chemistry observation items due to mining in Wang3 well in Tianjin

MA Jian-ying1, LIU Xue-ling2, SHAO Yong-xin1, LU Peng3   

  1. 1. Earthquake Administration Of Tianjin Municipality, Tianjin 300201;
    2. Baodi Seismostation, Earthquake Administration of Tianjin Municipality, Tianjin 300180;
    3. Institute of Disaster-Prevention Science and Technology, Yanjiao 065201, China
  • Received:2007-09-05 Revised:2007-10-31 Online:2008-04-30 Published:2021-10-29

Abstract: With the large-scale mining of geothermal water, it has made great influence on the chemical observation of underground water. This paper aims at preliminary discussion on the mechanism from two aspects, which may cause the influence: underground hydrodynamic condition and thermal-dynamical condition. On the initial period of mining, it was not obvious. The longer the mining continues, the more obvious the influence will cause. The underground water's pressure and temperature plays a dominant role on that variation process, so it is crucial to monitor well's situation on the water's chemical observation.

Key words: Water chemistry observation, Anomaly variation mechanism, Structure background, Wang3 well

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