Using the seismic waveform data recorded by the second sampling water level instrument of Yong'an well and compared with the CMG-3ESPC-60 seismometer,the coseismic response characteristics,response capability and seismic wave loading response of the well water level are analyzed. The results show that: The second sampling water level meter can also record the seismic body wave(P wave,S wave)and surface wave R,and the dispersion phenomenon of surface wave is clear,which can better reflect the action process of seismic wave and the release of energy in the process of source rupture; well water level has different responses to near-field earthquakes and far-field earthquakes, and its coseismic response capability was not necessarily related to magnitude and epicentral distance; compared with the CMG-3ESPC-60 seismometer,both of them have obvious periodic signals,and the amplitude of the surface wave band changes the most, which is the main center frequency. The water level waveform is consistent with the velocity value integral amplitude spectrum of the CMG-3ESPC-60 seismometer, and also has a wider frequency band,but lower than that of the CMG-3ESPC-60 seismometer.
图2 永安井水位记录到青海玛多县7.4级地震的同震响应曲线Fig.2 The coseismic response curve of Maduo M7.4 earthquake in Qinghai Province recorded by Yong′an well water level
2.2同震响应能力
表1 永安井水位记录到不同震级和震中距地震的同震响应参数Table 1 Coseismic response parameters of earthquakes with different magnitudes and epicentral distances recorded by Yong′an well water level
图3 永安井水位记录到不同震级、震中距的同震波形响应信号Fig.3 Coseismic waveform response signals with different magnitudes and epicentral distances recorded by the Yong′an well water level
图4 永安井水位与CMG-3ESPC-60地震计波形及S变换时频特征对比Fig.4 Comparison of waveform and S-transform time-frequency characteristics between Yong′an well water level and CMG-3ESPC-60 seismometer
图5 永安井水位(a)与CMG-3ESPC-60地震计速度值积分(b)振幅谱对比Fig.5 Comparison of the water level of Yong′an well(a)and amplitude spectrum of CMG-3ESPC-60 seismometer velocity value integration(b)