Signal to Noise Ratio Enhancement Using Empirical Wavelet Transform

W. Y. Lee, R. Hamidi, D. Ghosh, Mohd Hafiz Musa
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Abstract

Noise is the unwanted energy in a seismic trace opposed to the signals corresponding to reflected energy from the subsurface features. Since it can overlap with the main signals’ energy and conceal the geological information, noise attenuation is one of the most important steps in seismic data processing. The most common method is frequency filtering. However, due to its limitations on separating the noise from signals, this method usually results in hurting the signal. Hence, it is important to develop an alternative method that can attenuate the noise without affecting the signal. Filters based on time-frequency analysis of the data can have a better separation of the noise from signal as they maintain the time localization of events while presenting their frequency content simultaneously. One of the recent approaches to time-frequency analysis of signals is the Empirical Wavelet Transform (EWT) which provides adaptive wavelet filter bank for signal analysis. In this paper, a filter is designed based on EWT for random noise attenuation and is applied on both synthetic and real data. To evaluate the proposed filter performance, its results are compared with the filters based on Short Time Fourier Transform and Wavelet transform. As the EWT filter separate different seismic features using the adaptive basis wavelets, it can attenuate the noise while preserving the signals with higher precision.
基于经验小波变换的信噪比增强
噪声是地震轨迹中与地下特征反射能量对应的信号相反的多余能量。由于噪声衰减会与主信号能量重叠,掩盖地质信息,因此噪声衰减是地震资料处理的重要步骤之一。最常用的方法是频率滤波。然而,由于其在分离信号噪声方面的局限性,这种方法通常会对信号造成损害。因此,开发一种可以在不影响信号的情况下衰减噪声的替代方法是很重要的。基于数据时频分析的滤波器,在保持事件的时间局部化的同时,同时呈现事件的频率内容,可以更好地将噪声从信号中分离出来。经验小波变换是信号时频分析的最新方法之一,它为信号分析提供了自适应小波滤波器组。本文设计了一种基于小波变换的随机噪声抑制滤波器,并将其应用于合成数据和实际数据。为了评估该滤波器的性能,将其结果与基于短时傅里叶变换和小波变换的滤波器进行了比较。小波变换滤波器利用自适应基小波分离不同的地震特征,可以在降低噪声的同时保持较高的信号精度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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