The response of fluid-saturated reservoirs to lunisolar tides: Part 1. Background parameters of tidal components in ground displacements and groundwater level

被引：10

作者：

Besedina, A. N. ^{[1
]}

Vinogradov, E. A. ^{[1
]}

Gorbunova, E. M. ^{[1
]}

Kabychenko, N. V. ^{[1
]}

Svintsov, I. S. ^{[1
]}

Pigulevskiy, P. I. ^{[2
]}

Svistun, V. K. ^{[3
]}

Shcherbina, S. V. ^{[2
]}

机构：

[1] Russian Acad Sci, Inst Geosphere Dynam, Moscow 119334, Russia

[2] Natl Acad Sci, Inst Geophys IGP, Kiev, Ukraine

[3] Dnepropetrovsk Geophys Expedit Dneprogeofizika, Dnepropetrovsk, Ukraine

来源：

IZVESTIYA-PHYSICS OF THE SOLID EARTH | 2015年 / 51卷 / 01期

基金：

俄罗斯基础研究基金会;

关键词：

Groundwater Level; Solid Earth; East European Platform; Ground Displacement; Diurnal Tide;

D O I：

10.1134/S1069351315010036

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

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.

引用

页码：70 / 79

页数：10

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