摘要
本文针对地球天然脉冲电磁场(ENPEMF)信号的非平稳性特点,通过采用归一化STFT-WVD变换(NSTFT-WVD)提取芦山MS7.0地震前地表天然脉冲电磁场信号的时频特性,来研究大地震发生前地表天然脉冲磁场的时频特点。通过对线性调频信号分别进行Short-Time Fourier Transform(STFT)和WignerVille Distribution(WVD),对比分析两者时频聚集的优缺点,提出采用NSTFT-WVD变换方法,可得到时频聚集特性更优且可抑制交叉项的时频分析方法。结果表明,对于ENPEMF非平稳信号,NSTFT-WVD变换能较为真实地反映震前ENPEMF信号的时-频-能量谱的联合分布特性,即震前1~2天呈现较为明显的脉冲全频率段静默状态,通道2和通道3数据的震前时频表现基本一致,具有较好的临震前兆的特点。
The present paper aims at the non-stationary characteristics of Earth's natural pulse electromagnetic field(ENPEMF)signals by using the normalized STFT-WVD(NSTFT-WVD)transformation,and the main analysis focuses on time-frequency characteristics of the ENPEMF signal before Lushan MS7.0earthquake.By comparing short-time Fourier transform(STFT)and Wigner-Ville distribution(WVD)transformation with the linear frequency modulation signal,this paper analyzes their advantages and disadvantages of both time and frequency focusing performance.NSTFT-WVD transform method can give us the better time-frequency aggregation and inhibits the cross-terms.The results show that NSTFT-WVD transform can reflect the real ENPEMF signal time-frequency-energy spectrum distribution before and after the earthquake,which could render more obvious silent state in entire frequency and sustained 1-2days before the earthquake.The timefrequency representation of data channels 2and 3are basically consistent with this characteristic,which well represents the feature of impending earthquake precursors.
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2016年第1期276-286,共11页
Earth Science Frontiers
基金
国家自然科学基金项目(41502281)
中国博士后科学基金项目(2015M582293)
湖北省自然科学基金面上项目(2014075101)
中国地质大学(武汉)实验技术研究项目(SJ-201423)