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Ding Fenghe, Liu Yaowei, Han Xiaolei, Wei Jianmin, Zha Si. 2017: Water level anomaly analysis in Jiangsu and Anhui Provinces based on the well tide and barometric pressure effect. Acta Seismologica Sinica, 39(2): 248-256. DOI: 10.11939/jass.2017.02.008
Citation: Ding Fenghe, Liu Yaowei, Han Xiaolei, Wei Jianmin, Zha Si. 2017: Water level anomaly analysis in Jiangsu and Anhui Provinces based on the well tide and barometric pressure effect. Acta Seismologica Sinica, 39(2): 248-256. DOI: 10.11939/jass.2017.02.008
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Water level anomaly analysis in Jiangsu and Anhui Provinces based on the well tide and barometric pressure effect

  • 1.

    Earthquake Administration of Inner Mongolia Autonomous Region, Hohhot 010010, China

  • 2.

    Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China

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  • Received Date: June 27, 2016
  • Revised Date: October 07, 2016
  • Published Date: February 28, 2017
    Graphical Abstract
    • Abstract
  • Based on the theories of fluid and rock mechanics, we have studied the variation of porosity and permeability coefficients of the wells Su02, Su03, Su06, Su18 and Dingyuan04 with barometric pressure and tidal effect in aquifer medium under undrained condition. Using the micro dynamic models of well-aquifer system under the conditions of force and water balance, we also analyzed the mechanism of simultaneous rise in water level since the second half of 2014. The results show that: ① There is a linear relationship between the barometric coefficient and the tidal factor of M2 wave for the five wells, that is, the lager the barometric coefficient, the larger the tide factor; ② A set of synchronous enlargement phenomenon occurred in porosity and permeability coefficient of each well, which is mainly because that the recharge is greater than the discharge.
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    • References (36)
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