This paper analyzes the possibilities of an original approach to constructing a distributed seismic monitoring system based on a stationary seismoacoustic propagation path of a sounding signal. Such a stationary path can be formed by a powerful source of low-frequency vibration oscillations located on the earth's surface, and a signal recording point located tens (or more) kilometers away from it. It is proposed to use hydroelectric power station units as a powerful vibration source, which have a typical mass of several hundred tons and create vibration signals in the environment of the earth's rocks with characteristic frequencies from a few to one to two tens of Hz (including harmonics), and as a registration point – deep well equipped with the necessary measuring instruments. To record low-frequency longitudinal waves in the thickness of the earth's rocks surrounding the well, a fairly simple and effective method is proposed, based on the use of an extended wellbore as a distributed seismic antenna and a microphone installed on the upper section of the well. The work shows that stresses in the field of a longitudinal seismic wave, acting on the wellbore, cause a change in its diameter, which in turn leads to the occurrence of oscillations of the column of liquid filling the wellbore at the frequencies of the seismic waves determined by the source. A specific scheme for implementing the discussed approach is considered using the example of the Nizhny Novgorod hydroelectric station and the Vorotilovskaya deep well located at a distance of about 40 km. Quantitative estimates and experimental data demonstrating the possibilities of using the corresponding stationary route are presented.
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