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

机译:使用小波包变换检测地震信号中的P波起义

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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:检测地震信号中的P波的发作是用于地震易发区域的预警系统的关键目标。该工作提出了一种新的时频基础方法,以有效地检测和选择具有低SNR(信噪比)的地震信号中的P波开始的启动。所提出的技术依赖于地震噪声和小波分组变换(WPT)的时间序列建模的组合,其中核心思想涉及跟踪数据的能量与一步的小波包中的一步模型预测的差异(频段)。自动回归集成移动平均(ARIMA)模型用于建模地震噪声,而使用对P波频率内容的普遍了解选择分组。所提出的方法在两个方面中优于现有方法,(i)检测和拣选的准确性,因为它放大到频段(对应于P波开始)和(ii)在最小误报的意义上的鲁棒性由于异常值和其他来源,尤其是低SNR地震图。所提出的方法的性能在简化的模拟过程和在低SNR条件下获取的实时地震数据集。还提出了具有最近开发的最大归一化交叉相关方法的对比研究以证明所提出的方法的优越性。

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