Blind deconvolution technique for de-noising of non-stationary seismic signals using DWT

M. Shahzad Younis, A. Hani
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Abstract

Discrete wavelet transform is an effective tool to disintegrate the time variant seismic data in time-frequency manner. This work incorporates the wavelet transform in the blind deconvolution technique to deal with the inherent non-stationarity present in seismic data and to improve the SNR of seismic data. Time varying nature of seismic data is the result of a depth varying character of seismic source wavelet (where high frequency components of the source wavelet get absorbs due to increasing heat gradient with depth) convolved with the non Gaussian distributed earth reflectivity in presence of additive Gaussian, color Gaussian noise. Seismic signal can thus be considered as a result of multiple subsystems with different constraints based on time-frequency localization convolved with input signal. Techniques based on stationarity assumptions are not effective in modeling the time variance character of source with depth. In this work we apply the discrete wavelet transform (DWT) to decompose the seismic data into different time-frequency signals. Denoising based on soft thresholding is applied to get the shrinkage effect of wavelet coefficients. Combination of blind deconvolution technique mixed with the discrete wavelet transform gives the best result in terms of reducing the noise and improving the resolution of seismic data with time. Denoising based on soft thresholding gives optimal minimum means square value, low convolutional noise and also low maximum distortion value than hard thresholding.
基于DWT的非平稳地震信号去噪盲反褶积技术
离散小波变换是对时变地震资料进行时频分解的有效工具。本文将小波变换引入到盲反褶积技术中,以处理地震资料固有的非平稳性,提高地震资料的信噪比。地震资料的时变性质是地震震源小波的深度变化特征(其中震源小波的高频分量由于热梯度随深度增加而被吸收)与存在加性高斯、彩色高斯噪声的非高斯分布地球反射率卷积的结果。基于时频局部化与输入信号的卷积,可以将地震信号视为具有不同约束条件的多个子系统的结果。基于平稳性假设的方法不能有效地模拟深度源的时变特征。本文采用离散小波变换(DWT)将地震数据分解为不同的时频信号。采用基于软阈值的去噪方法获得小波系数的收缩效果。将盲反褶积技术与离散小波变换相结合,在降低噪声和提高地震资料的时间分辨率方面效果最好。与硬阈值相比,基于软阈值的去噪具有最小均方值、较低的卷积噪声和较低的最大失真值。
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