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时频分析方法及在地震波谱研究中的应用
引用本文:张帆,钟羽云,朱新运,熊丹,周昕. 时频分析方法及在地震波谱研究中的应用[J]. 地震地磁观测与研究, 2006, 27(4): 17-22
作者姓名:张帆  钟羽云  朱新运  熊丹  周昕
作者单位:中国,合肥,230026,中国科学技术大学地球与空间科学学院;中国,杭州,310013,浙江省地震局;中国,杭州,310013,浙江省地震局
摘    要:地震波是一种非平稳信号,傅立叶分析已不适合。时频分析能对非平稳信号进行分析,并给出地震波信号能量的时间-频率分布。但是在时频分析时,存在交叉干扰项,会带来一些错误的信息。本文讨论了波恩-约旦(Born-Jordan)时频分布、乔伊-威廉斯(Choi-Williams)时频分布、赵-阿特拉斯-马克斯(Zhao-Atlas-Marks)时频分布3者之间抑制和消除交叉干扰项的特点,认为赵-阿特拉斯-马克斯(Zhao-Atlas-Marks)时频分布抑制交叉干扰项的效果和时频聚集性更好,更适合于分析地震波。

关 键 词:非平稳信号  时频分布  数字化地震波  交叉干扰项  时变频谱
文章编号:1003-3246(2006)04-0017-06
收稿时间:2006-02-27
修稿时间:2006-02-27

Application of time-frequency analysis to seismic wave spectrum research
Zhang Fan,Zhong Yuyun,Zhu Xinyun,Xiong Dan,Zhou Xin. Application of time-frequency analysis to seismic wave spectrum research[J]. Seismological and Geomagnetic Observation and Research, 2006, 27(4): 17-22
Authors:Zhang Fan  Zhong Yuyun  Zhu Xinyun  Xiong Dan  Zhou Xin
Affiliation:1 School of Earth and Space Science of University of Science and Technology of China, Hefei 230026, China 2
Abstract:Earthquake waveform signal is a kind of nonstationary signal, which can not be analyzed suitably by classical Fourier analysis. Time-frequency analysis can analyze nonstationary signal including earthquake signal. But the existence of cross distribution is inevitable. The characteristic of weakening the cross distribution of three kind of time-frequency presentation, which are Born-Jordan, Choi-Williams, Zhao-Atlas-Marks time-frequency presentation, is discussed in this article. In conclusion, Zhao-Atlas-Marks time-frequency presentation has weakest cross distribution, and is most suitable for analyzing earthquake waveform signal.
Keywords:nonstatonary signal   time-frequency presentation   digital earthquake wave   cross distribution
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