摘要
对安装在泉州地震台的SLJ-100型加速度计强震仪和CTS-1型地震仪记录到的汶川Ms8.0地震波进行对比。结果显示:1)在频谱方面,两种仪记录在0.012~2 Hz内基本一致,在低频段由于仪器响应不同存在差异;2)波形和相对位移反应谱方面,经基线校正和带通滤波后的两种记录呈现相当高的一致性;300 s周期内的相对位移反应谱表明,基线校正并没有引入不可接受的长周期噪声干扰。
Seismic waves of the Ms8.0 Wenchuan earthquake were compared which were recorded the strong-motion seismograph (SLJ-100 accelerometer) and the seismograph (CTS-1 seismometer) in by Both of Quanzhou Seismostation seismostationrecorded relatively complete seismic waves of Wenchuan earthquake ( May 12, 2008). In order to carry out a comprehensive comparative analysis of two types of records, the author first does baseline correction and bandpass filtering in the 20 Hz ~ 120 s by using SLJ-100 accelerogram. The results show that: 1 ) Viewed from spectrum, strong-motion seismograph records and seismograph records are almost the same from the rangein of 0.012 Hz to 2 Hz. The differences lie in the low-frequency and the high-frequency due to different in- strument response and instrument noise respectively. 2)Viewed from wave form and relative displacement, the re- cords of SLJ-100 and CTS-1 show relatively high consistency after baseline correction and band pass filtering. These indicate that from high-accuracyaccelerogram integral to speed and displacement trough baseline correction is feasible. The 300 s cycle relative displacement response spectrum shows that baseline correction does not introduce unacceptable long period noise.
出处
《大地测量与地球动力学》
CSCD
北大核心
2013年第A01期172-175,共4页
Journal of Geodesy and Geodynamics
关键词
汶川地震
强震仪
地震仪
地震波
位移反应谱
Ms8.0 Wenchuan earthquake
strong-motion seismograph
seismograph
seismic wave
displacement response spectrum