首页 | 本学科首页   官方微博 | 高级检索  
     检索      

强地震的前兆次声波研究
引用本文:邵长金,唐炼,李相方.强地震的前兆次声波研究[J].应用声学,2005,24(3):152-156.
作者姓名:邵长金  唐炼  李相方
作者单位:中国石油大学,北京,102200
摘    要:利用在北京昌平安装的次声三点阵,对强地震前兆次声波进行了5年的连续观测。统计分析结果表明:强震前约10天内常能测到振幅很强的前兆次声。其三维动态频谱的特点是,振幅由弱逐渐加强,达到极值后变弱;先为长周期波(10-20分),紧跟着短周期波(5-10分),然后又出现更长的周期波,最后长短周期波一起出现。提前时间与三点阵到震中距离之间没有明显的关系,与震级之间也没有明显的关系。

关 键 词:前兆次声波  次声三点阵  三维动态频谱  强震

Precursory infrasonic waves from strong earthquakes
SHAO Chang-Jin,TANG Lian and li Xiang-Fang.Precursory infrasonic waves from strong earthquakes[J].Applied Acoustics,2005,24(3):152-156.
Authors:SHAO Chang-Jin  TANG Lian and li Xiang-Fang
Institution:Department of Math & Physicss, University of Petroleum, Beijing 102200;Department of Math & Physicss, University of Petroleum, Beijing 102200;Department of Math & Physicss, University of Petroleum, Beijing 102200
Abstract:Our five-years measurement of the precursory infrasonic waves from strong earthquake using a tripartite array setup in Changping, Beijing shows that, 10 days or so before occurrence of a strong earthquake, a precursory infrasound with strong amplitude can often be observed. The spectrum characteristics are: (1) the amplitudes of precursory infrasound vary from weak (10~30Pa) to strong (50~80Pa) or even stronger (150-300 Pa); their periods are in at first (10~20min), then decreases to (5~10min), and finally become (5~40min). Their waveforms are distinctly different from that of meteor shower and strong wind. (2) The time of advancement has no obvious relation with the magnitude of earthquake or the distance or depth of epicenter.
Keywords:Precursory infrasonic waves  Infrasonic tripartite array  Three-dimensional dynamic frequency spectrum  Strong earthquake
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《应用声学》浏览原始摘要信息
点击此处可从《应用声学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号