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Detection of P-wave Onset in Seismic Signals using Wavelet Packet Transform

机译:小波包变换检测地震信号中的P波起跳

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Detecting the onset of P-waves in seismic signals is a crucial objective in the development of early warning systems for earthquake-prone regions. This work presents a novel time-frequency based method to efficiently detect and pick the onset of P-wave in seismic signals with low SNR (signal-to-noise ratio). The proposed technique rests on a combination of time-series modelling of seismic noise and wavelet packet transform (WPT), in which the core idea involves tracking the difference between energies of data and one-step ahead model predictions over a select set of wavelet packets (frequency bands). Auto-regressive integrated moving average (ARIMA) models are used for modelling seismic noise, while the packets are selected using the prevailing understanding of P-wave frequency content. The proposed method is superior to the existing methods in two respects, (i) accuracy of detection and picking since it zooms into the frequency bands of interest (corresponding to P-wave onset) and (ii) robustness in the sense of minimal false alarms due to outliers and other sources, especially from low SNR seismograms. The performance of proposed method is illustrated on a simplified simulated process and real-time seismic data sets acquired under low SNR conditions. A comparative study with a recently developed maximum normalized cross correlation method is also presented to demonstrate the superiority of the proposed method.
机译:在地震多发地区预警系统的开发中,检测地震信号中P波的出现是至关重要的目标。这项工作提出了一种新颖的基于时频的方法,可以有效地检测和拾取具有低SNR(信噪比)的地震信号中的P波。所提出的技术基于地震噪声的时间序列建模与小波包变换(WPT)的组合,其中的核心思想包括跟踪数据能量之间的差异以及对选定的小波包集进行一步一步模型预测(频段)。自回归综合移动平均(ARIMA)模型用于建模地震噪声,而使用对P波频率内容的普遍理解来选择数据包。所提出的方法在两个方面优于现有方法:(i)检测和拾取的准确性,因为它可以放大到感兴趣的频带(对应于P波开始),并且(ii)在最小化虚警率的意义上具有鲁棒性由于离群值和其他来源,特别是来自低SNR地震图的缘故。通过简化的仿真过程和在低SNR条件下获取的实时地震数据集,说明了所提出方法的性能。还提出了与最近开发的最大归一化互相关方法的比较研究,以证明所提出方法的优越性。

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