Seismo-Hydrogeodynamic Effects in Groundwater Pressure Changes: A Case Study of the YuZ-5 Well on the Kamchatka Peninsulaстатья
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Дата последнего поиска статьи во внешних источниках: 20 февраля 2024 г.
Аннотация:Seismo-hydrogeodynamic effects (SHGEs) in groundwater level (pressure) variations in
a range of periods from minutes to hours and days during local and teleseismic earthquakes were
considered based on the data of precision observations in a deep piezometric well located in a seismically
active region. With the use of the tidal analysis and frequency dependence of the barometric
response of the water level, a static confined response of groundwater pressure in a range of periods
from hours to the first tens of days was established. The annual water level trend was characterized
by the seasonal function of a hydrostatic head change in the well. In the groundwater pressure,
changes were detected due to several types of seismo-hydrogeodynamic effects: 1—the coseismic
fluctuations during the first tens of seconds and minutes after the arrival of seismic waves from
the earthquakes with magnitudes of 5.3–9.1 at epicentral distances of 80–700 km; 2—the supposed
hydrogeodynamic precursors of the two strongest events; 3—the four types of variations under
the vibration impact of seismic waves from Mw = 6.8–9.1 earthquakes at epicentral distances of
80–14,600 km. The dependence of the distinguished types of SHGEs on the earthquake parameters,
the intensity of the seismic impact in the well area and the amplitude-frequency composition of
seismic waves were considered.