The response of fluid-saturated reservoirs to lunisolar tides: Part 1. Background parameters of tidal components in ground displacements and groundwater level
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  • 作者:A. N. Besedina (1)
    E. A. Vinogradov (1)
    E. M. Gorbunova (1)
    N. V. Kabychenko (1)
    I. S. Svintsov (1)
    P. I. Pigulevskiy (2)
    V. K. Svistun (3)
    S. V. Shcherbina (2)

    1. Institute of Geosphere Dynamics
    ; Russian Academy of Sciences ; Leninskii pr. 38/1 ; Moscow ; 119334 ; Russia
    2. Institute of Geophysics (IGP)
    ; National Academy of Sciences ; Kiev ; Ukraine
    3. Dnepropetrovsk Geophysical Expedition 鈥淒neprogeofizika
    ; 鈥? Dnepropetrovsk ; Ukraine
  • 刊名:Izvestiya, Physics of the Solid Earth
  • 出版年:2015
  • 出版时间:January 2015
  • 年:2015
  • 卷:51
  • 期:1
  • 页码:70-79
  • 全文大小:1,802 KB
  • 参考文献:1. Adushkin, V.V., Spivak, A.A., and Kharlamov, V.A., Effects of lunar-solar tides in the variations of geophysical fields at the boundary between the Earth鈥檚 crust and the atmosphere, / Izv., Phys. Solid Earth, 2012, no. 2, pp. 104鈥?16.
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    3. Besedina, A.N., Kabychenko, N.V., Gorbunova, E.M., and Svintsov, I.G., Monitoring tidal variations in the seismic and hydrogeological data collected at the East European Platform, / Proc. 33rd General Assembly of the European Seismological Commission, Moscow, 2012a, pp. 242鈥?43.
    4. Besedina, A.N., Vinogradov, E.A., Gorbunova, E.M., and Svintsov, I.S., Investigation of tides in geophysical fields registered in the Mikhnevo geophysical observatory area, in: / Dinamicheskie protsessy v geosferakh (Dynamic Processes in Geospheres), Moscow: GEOS, 2012b, pp. 99鈥?07.
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  • 刊物主题:Geophysics/Geodesy;
  • 出版者:Springer US
  • ISSN:1555-6506
文摘
The first part of this work is dedicated to the response of different-age structures to lunisolar tides, which can be considered as a sounding signal for monitoring the state of fluid-saturated reservoirs. The complex approach to processing the data obtained at the testing sites of the Institute of Geosphere Dynamics of the Russian Academy of Sciences, Institute of Geophysics of the National Academy of Sciences of Ukraine, and KIEV station of the IRIS seismic network is applied for recognizing the tides against the hydrogeological, barometric, and seismic series. The comparative analysis of the experimental and theoretical values of the diurnal and semidiurnal tidal components in the time series of ground displacements is carried out. The tidal variations in the groundwater level are compared with the tidal components revealed in the ground displacement of the different-age structure of the Moscow Basin and Ukrainian Shield, which are parts of the East European artesian region. The differences in the tidal responses of the groundwater level and ground displacement probably suggest that the state of the massif is affected by certain additional factors associated, e.g., with the passage of earthquake-induced seismic waves and the changes in the hydrogeodynamic environment.

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