首页 | 本学科首页   官方微博 | 高级检索  
     检索      

基于地震信号波形形态差异的面波噪声稀疏优化分离方法
引用本文:陈文超,王伟,高静怀,姜呈馥,雷江莉.基于地震信号波形形态差异的面波噪声稀疏优化分离方法[J].地球物理学报,2013,56(8):2771-3782.
作者姓名:陈文超  王伟  高静怀  姜呈馥  雷江莉
作者单位:1. 西安交通大学电子与信息工程学院波动与信息研究所, 西安 710049; 2. 陕西延长石油集团有限责任公司研究院, 西安 710075
基金项目:国家自然科学基金,国家科技重大专项
摘    要:实际地震信号通常可表示为具有波形特征差异的多种基本波形信号的线性组合,如叠前道集中的工频干扰噪声与有效波信号、面波噪声与体波信号等.选择单一数学变换方法,往往不易实现地震信号的稀疏表示.近年来发展的形态成分分析理论,通过联合多种数学变换,可实现对复杂信号的稀疏表示.本文根据单道地震记录中面波与体波信号波形结构特征的差异性,提出一种基于形态成分分析的面波噪声衰减方法.针对面波的低频、窄带以及频散特性选择一维平稳小波变换作为其稀疏表示字典,而针对体波波形的局部相关特性选择局部离散余弦变换作为其稀疏表示字典,建立基于双波形字典的形态成分分析模型,通过求解该稀疏优化问题获得最终的信噪分离结果.理论模型和实际地震资料处理证实该方法不仅能够衰减单炮地震记录中的强面波干扰噪声,同时能够更好地保护有效信号的波形特征与频谱带宽,为地震资料的后续处理和分析提供良好的数据基础.

关 键 词:形态成分分析  稀疏表示  平稳小波变换  局部余弦变换  面波噪声  
收稿时间:2012-06-06

Sparsity optimized separation of Ground-roll noise based on morphological diversity of seismic waveform components
CHEN Wen-Chao , WANG Wei , GAO Jing-Huai , JIANG Cheng-Fu , LEI Jiang-Li.Sparsity optimized separation of Ground-roll noise based on morphological diversity of seismic waveform components[J].Chinese Journal of Geophysics,2013,56(8):2771-3782.
Authors:CHEN Wen-Chao  WANG Wei  GAO Jing-Huai  JIANG Cheng-Fu  LEI Jiang-Li
Institution:1. School of Electronic and Information Engineering, Xi'an Jiaotong University, Xi'an 710049, China; 2. Research Institute, Shaanxi Yanchang Petroleum(Group) Co., LTD, Xi'an 710075, China
Abstract:Real seismic signals can usually be represented as a linear combination of multiple basic waveforms of different morphological characteristics, such as powerline single frequency interference noise and effective seismic signal, ground roll and body wave signals. By selecting a single mathematical transformation method, it will hard to achieve sparse representations of seismic signals. Morphological component analysis (MCA) theory has been developed in recent years, which can sparsely decompose complex signals through the augmented dictionary of basic mathematical transformations. According to the waveform divergence of ground-roll and body wave signals, this paper proposes a ground-roll attenuation method based on the morphological component analysis theory. To match with the requirements of the MCA, the 1D stationary wavelet transform (SWT) is chosen as the sparse representation dictionary of ground-roll due to its low frequency and narrow spectral bandwidth nature. Meanwhile, the local discrete cosine transform (LDCT) is chosen as the sparse representation dictionary of body waves due to its local interdependency characteristics. The optimization model on basis of the MCA is then built on the two amalgamated dictionaries and properly solved to obtain the final signal-noise separation results. The theoretical and real data processing results confirm that the method can not only attenuate strong ground-roll noise in seismic records but also preserves the waveform characteristics and spectral bandwidth of effective signal well. The method can provide high quality data for subsequent processing and analysis.
Keywords:Morphological component analysis  Sparse representation  Stationary wavelet transform  Local discrete cosine transform  Ground-roll noise
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号