波兰西南部Książ地下地球动力学实验室水管倾斜仪记录的10−3-10−4 Hz范围信号的研究

IF 0.7 Q4 ASTRONOMY & ASTROPHYSICS
M. Kaczorowski, D. Kasza, R. Zdunek, R. Wronowski
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引用次数: 0

摘要

Książ地球动力学实验室包括对各种地球动力学信号的研究。其中,我们记录了范围为10−3-10−4 Hz的谐波信号。这些信号是在长水管倾斜仪的测量系列中发现的。发现的信号由两类与各种现象相关的谐波组成。第一类信号属于地球固体的粘弹性振动,而第二类信号可能是由极长的大气次声波产生的。地球的振动信号已经被地球自由振动共振的特征频率很好地识别出来,这种共振主要发生在强烈地震之后。大气压微振动是逆气压效应对水动力系统水位的影响。我们观察到,来自两类的信号混合在相似频率的谐波中,并共同影响WTs的水动力系统。我们发现,第二类信号的振幅强烈依赖于地下水管仪表的位置,而所有仪表的一级信号的振幅是相似的。这些观测清楚地表明了第二类记录信号的大气来源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Investigation of Signals of the Range 10−3–10−4 Hz Registered by Water-Tube Tiltmeters in the Underground Geodynamic Laboratory in Książ (Sw Poland)
Abstract The Geodynamic Laboratory in Książ includes investigations of various kinds of geodynamic signals. Among others, we registered harmonic signals of the range 10−3–10−4 Hz. These signals had been found in the measurement series of the long water-tube (WT) tiltmeters. The discovered signals consist of two classes of harmonics associated with various kinds of phenomena. The first class of these signals belongs to viscoelastic vibrations of the Earth’s solid body, while the second class is produced possibly by the extremely long atmospheric infrasound waves. The signals of the vibrations of the Earth had been well recognized by the characteristic frequencies of the Earth’s free vibrations’ resonance, which occur mainly after strong earthquakes. The atmospheric pressure microvibrations affected the water level in the hydrodynamic systems of the WTs as a result of an inverse barometric effect. We observed that signals from both classes blend in the harmonics of similar frequencies and jointly affect the hydrodynamic systems of the WTs. We found that the amplitude of the second-class signals strongly depends on the location of water-tube gauges inside the underground, while the amplitudes of the first-class signals are similar for all the gauges. These observations clearly indicate the atmospheric origin of the second class of registered signals.
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CiteScore
1.00
自引率
11.10%
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