Abstract:The wavelet packet transform gives information in both the time and frequency domains, and it is very useful for describing nonstationary signals like seismograms. Moreover, this structure is dependent on the signal under study; hence we can choose the time-frequency decomposition more appropriate for every signal. In this article, we propose a new method for filtering based on the wavelet packet transform. This approach uses different parameters for filtering, depending on the band of frequencies that we are … Show more
“…Its soft signal variations and shape allow for an easy fit to our type of data. Daubechies wavelets have been employed to analyse seismic signals (e.g., Galiana-Merino et al 2003, drilling-ability data (Frantziskonis and Denis 2003) 8 and precipitation series (Luan et al 2011). Morlet wavelets are used to find temporal periodicities.…”
“…Its soft signal variations and shape allow for an easy fit to our type of data. Daubechies wavelets have been employed to analyse seismic signals (e.g., Galiana-Merino et al 2003, drilling-ability data (Frantziskonis and Denis 2003) 8 and precipitation series (Luan et al 2011). Morlet wavelets are used to find temporal periodicities.…”
“…It is necessary to reduce the interference noise of the microseismic signals as much as possible. As any slight noise, distortion, or phase shift on the first arrival can result in an incorrect time picking (Galiana-Merino et al 2003), a denoising method based on ITD (Zhang et al 2012) is more suitable for detecting the seismic signal because the abrupt change of the amplitude at the beginning of the first pulse is preserved. We therefore apply the ITD method to the microseismic signals.…”
A b s t r a c t A method to identify the P-arrival of microseismic signals is proposed in this work, based on the algorithm of intrinsic timescale decomposition (ITD). Using the results of ITD decomposition of observed data, information of instantaneous amplitude and frequency can be determined. The improved ratio function of short-time average over long-time average and the information of instantaneous frequency are applied to the time-frequency-energy denoised signal for picking the P-arrival of the microseismic signal. We compared the proposed method with the wavelet transform method based on the denoised signal resulting from the best basis wavelet packet transform and the single-scale reconstruction of the wavelet transform. The comparison results showed that the new method is more effective and reliable for identifying P-arrivals of microseismic signals.
“…3b, we show the theoretical period ranges associated to the wavelet packet coefficients obtained for 2 levels of decomposition (scale 2). More details about the DWPT can also be found in Galiana-Merino et al [26].…”
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