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基追踪在面波分离与压制中的应用
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摘要
随着地震勘探技术的深入和发展,要求勘探目标越来越精细,面波是一种对地震记录信噪比影响较大的相干干扰,如果不很好地压制,会严重影响地震资料的后续处理及解释工作,传统的压制面波的方法都只是侧重考虑某一方面的单一特性或者仅依据某种条件假设等,尽管能有效地压制面波,但是在压制面波的同时有效波也会受到不同程度的损失。近几年来发展起来的基追踪(Basis Pursuit, BP)算法是信号稀疏。表示领域的一种新方法。它寻求从完备的(过完备)函数(基)集合中得到信号最稀疏的表示,即用尽可能少的基精确地表示原信号,从而获得信号的内在本质特性。根据地震信号的特性将此方法应用到地震资料处理中,为获得高分辨率的地震资料提供了新的研究方向。
     本文首先对面波分离与压制的发展及研究现状做了分析,然后介绍了目前常用去除面波的方法及信号稀疏分解基础知识,实现了基于BP的频率估计方法,实验结果证明了利用BP分解信号能够准确地估计出信号的频率,为BP分离地震信号提供了一定的方法基础。在第三章中,实现了基于BP的合成一维地震信号的时频分离,实验证明BP能够有效地分离出组成地震信号的各个子波,在BP分离地震信号的基础上提出了一种基于BP的面波分离与压制方法,该方法是基于稀疏分解的原理,以面波的频率特性和能量特性为依据,根据二维地震信号的实际频率范围及地震信号的结构特征建立白适应原子库,并从中筛选出能近似重建地震信号的重要原子,然后根据筛选出的重要原子分解系数以及参数来设置能量阈值和主频阈值范围,从每道地震信号分解结果中找出组成面波的原子重建该道的面波成分,用该道地震信号减去面波成分并得到该道压制面波后的地震信号,以达到分离与压制面波的效果。在第四章中,利用提出的BP分离与压制面波的方法对合成的二维地震记录进行了面波的分离与压制,与传统的一维傅里叶滤波方法和一维小波处理方法做对比,分别从主观和客观评价该方法的处理效果,证明了该方法在处理效果上的优越性。在第五章中,利用提出的BP分离与压制面波的方法对实际的地震剖面进行了面波的分离与压制,与传统的一维傅里叶滤波和一维小波处理方法对比,通过实验证明该方法对实际地震剖面处理效果较传统的方法仍然具有优势。
With the development of seismic exploration technology, exploration targets required more and more sophisticated,surface wave is a coherent interference, which is a signal to noise ratio greater impact on the seismic records.The traditional method of surface wave suppression only focus on one aspect to consider a single feature, or assumptions based only on certain conditions, despite the effective suppression of surface wave, however, while the effective suppression of surface wave, effective wave will also be different degrees of loss. Developed in recent years, the Basis Pursuit algorithm is that the area of sparse signal a new approach,which sought the most sparse representation of signal from the complete (overcomplete) function (base) set, that is expressing the original signal exactly with base as little as possible, thereby obtain the intrinsic nature of the signal characteristics. According to the characteristics of seismic signals,this paper applied this method to the seismic data processing, which provides a new research direction in order to btain high-resolution seismic data.
     This paper first analyzes the development and current research situation of separation and suppression method of surface wave, then introduced the normal method of removal of surface wave and the basis knowledge of signal sparse decomposition, analysis of the frequency estimation method which is based on BP, experimental results show the using of BP decomposition the signal can accurately estimate the frequency of the signal,which provides the basis of a certain method for BP separating seismic signals. In the third chapter, the separation of time-frequency of the synthesized one-dimensional seismic signals based on BP was achieved, experimental proved BP can effectively isolate the various sub-wave which composed seismic signal, separation in BP based on the seismic signal, a separation and suppression method of surface wave based on BP is bring forward on the basis of BP separating seismic signals, this method is based on the sparse decomposition principle, according as the frequency characteristics and energy characteristics of surface wave, according to the actual frequency range of two-dimensional seismic signals and structural characteristics of the seismic signal establishes adaptive atom dictionary, and selected the importance atoms which can approximate reconstruct the seismic signal form the atom dictionary, then according to decomposition coefficients and parameters of the selected importance atoms set the energy threshold and the range of main_frequency threshold adaptively, identify the atoms which compose surface wave form the decomposition results of every seismic signal and reconstruct the surface wave component of this seismic signal, using of this seismic signal subtract the surface wave component and get the seismic signal which its surface wave component is suppressed, to achieve and the effect of separating and suppressing surface wave. In the fourth chapter, using of the proposed method of BP to separation and suppression of surface wave separate and suppress the surface wave of synthetic two-dimensional seismic record, comparing with the traditional one-dimensional Fourier filtering and one-dimensional wavelet processing method, respectively subjective and objective evaluate the treatment effect of the method, results show that the method's superiority in the treatment effect. In the fifth chapter, using of the proposed method of BP to separation and suppression of surface wave separate and suppress the surface wave of the actual seismic profile, comparing with the traditional one-dimensional Fourier filtering and one-dimensional wavelet processing method, experimental results show this method still reflects its advantages in actual seismic data processing than the traditional methods.
引文
[1]刘财,陈业全,刘洋,王典,苗广文.勘探地震资料处理新方法及新技术[M].科学技术出版社,2006.6.
    [2]刘洋,王典等.数学变换方法在地震勘探中的应用[J].吉林大学学报(地球科学版)Vol.35 2005
    [3]张军华,吕宁等.地震资料去噪方法技术综合评述[J].地球物理学进展.2006;26(2):546~563
    [4]俞寿朋.高分辨率地震勘探[M].北京:石油工业出版社,1993,1~34
    [5]赵馨.地震数据处理中叠前去噪应用研究[D].中国地质大学硕士论文,2008.5
    [6]夏洪瑞,周开明.地震资料处理中相干干扰消除方法分析[J].石油物探,2003,42(4):526-529.
    [7]李亚俊,地震勘探子波估计、面波消减新技术研究[D],吉林大学博士论文,2007.11
    [8]S.Chen, D.Donoho and M. Saunders, "Atomic decomposition by basis pursuit", to appear in SIAM J.Scientific Computing.
    [9]詹毅.地震资料叠前去噪方法研究[D],成都理工大学博士论文,2005,5
    [10]李文杰,魏修正等.基于频率衰减特性的面波压制方法[J].石油物探,2008,47(3):225~227.
    [11]王典,刘财等.反射法地震勘探噪声消除技术研究[J].地球物理学进展No.2.2006
    [12]梁志强.层状介质中多模式面波频散曲线研究[D].长安大学硕士学位论文.2006
    [13]康冶,于承业,等.f-x域去噪方法研究[J].工石油地球物理勘探,2003,38(2)136~138.
    [14]J.C.Tokeshi, M.B.Karkee. Reliability of Rayleigh wave dispersion curve obtained from f-k spectral analysis of microtremor array measuremen[J]. Soil Dynamics and Earthquake Engineering.2006,26:163~174
    [15]闫立志,景新义等.F-K滤波在噪音减去法中的作用[J].海洋地质动态,2006,22(10):28-32
    [16]李彩芹,张华.小波变换与F-K联合滤波在面波分离中的应用[J].中国煤田地质,2007,Vol.19 No.4
    [17]Brian Russell, Dan Hampson, Joong Chun. Noise elimination and the radon transform [J]. The Leading Edge,1990, Vol.9, No.11:18~23.
    [18]曾有良.Radon变换波场分离技术研究[D],中国石油大学硕士研究生学位论文.2007.4
    [19]罗国安,杜世通.小波变换及信号重建在压制面波中的应用[J].石油地球物理勘探,1996,31(3):337-349.
    [20]刘财,王典等.二维小波变换在地震勘探面波消除中的应用[J].地球物理学进展,2003,18(4):711-714.
    [21]Jones IF, Levy S.Signal-to-noise ratio enhancement in multi-channel seismic data via the Karhunen-Loeve transform[J]. Geophysical Prospecting,1987,35, 12~32.
    [22]杨文采.非线性K-L滤波及其在反射地震资料处理中的应用[J].石油物探,1996,35(2):17-26.
    [23]蔡仲华等.应用时空变KL滤波消除叠后地震记录相干噪声[J].石油地球物理勘探,1999,34(sup):53-58.
    [24]付燕,赵荣椿.消除叠后地震记录相干噪声的时-空变倾角KL变换[J].物探与化探,2002,26(2):143-147.
    [25]Mallat S, Zhang Z. Matching pursuits with time-frequency dictionaries[J]. IEEE Trans Signal Process.1993,41(12):3397-3415.
    [26]J. Fuchs. Recovery of exact sparse representations in the presence of bounded noise. Publication interne del'IRISA, (1618),2005.
    [27]汪雄良,王春玲.基于改进基追踪方法的信号去噪[J].计算机应用,2005,Vol 8.P19-21.
    [28]Elad, Michael; Matalon, Boaz; Zibulevsky, Michael. Image denoising with shrinkage and redundant representations.2006 IEEE Computer Society Conference on Computer Vision and Pattern Recognition, CVPR 2006,2006, p 1924-1931.
    [29]Zhengfei Tai and Samuel Cheng. Automatic Fluorescent Dot Counting In Interphase Cell Nuclei Using Basis Pursuit Image Analysis. Digital Object Identifier 10.1109/TPSD.2008
    [30]冯志鹏,朱萍.玉基追踪在齿轮损伤识别中的应用[J].北京科技大学学报,2008,Vol.30 No.1
    [31]Alonso Ramfrez-Manzanares, Mariano Rivera. Basis Pursuit Based Algorithm for Intra-Voxel Recovering Information in DW-MRI. Proceedings of the Sixth Mexican International
    [32]李媛媛.小波变换去除面波的方法研究[D],长安大学硕士论文,2004.6
    [33]Temlyakov V.Nonlinear Merhods of Approximation.IMI Research Reports, Dept. of Mathematics, University of South Carolina,2001,01:09
    [34]Shie Qian and Dapang Chen.Signal representation using adaptive normalized Gaussianfunctions[J].Signal Processing,1994,36:111
    [35]Chen, W.Luo. Orthogonal least methods and their applicationtonon-linear system identieation[J]. hit. Jour.Control,1989,50:1873-1896
    [36]P.Bloomfield and W.Steiger, Least Absolute Deviations:Theory Applications and Algorithms[J]. Birkhauser, Boston,1983
    [37]王建英,尹忠科,张春梅.信号与图像的稀疏分解及初步应用[M].2006,第1版,成都:西南交通大学出版社
    [38]陈磊.信号稀疏分解在空间谱估计中的应用.西南交通大学硕士论文[D].2004
    [39]应怀樵.波形和频谱分析与随机数据处理[M].中国铁道出版社,198:3330~331.
    [40]Chne.S, DonohoD.L. Application of pursuit in spectrum estimation[C]. ICASSP'98.Poceeedings of the 1998 IEEE International Conference on Aeoustics, Speech, and Signal Proeessing,1998. vol.3.1998:1865-1868.
    [41]http://jpk.dqpi.net/yydqwl/sxzds/wcscsx.doc
    [42]杨宝俊.勘探地震学导论[M].吉林:吉林科学技术出版社,1990
    [43]Sheriff R.E. Encyclopedic dictionary of exploration geophsics.Tulsa:Society of Exploration Geophysicists,1994
    [44]李庆忠.走向精确勘探的道路.多分辨地震勘探系统工程剖析[M].北京石油工业出版社,1994
    [45]邓小英.Ricker子波最小二乘支持向量回归机及其在地震勘探资料去噪中的应用[D].吉林大博士论文,2007
    [46]Philippe S, Guy D. Seismic sequence analysis and attribute extraction using quadratic time-frequency representations [J]. Geophysics 2001,66(6):1947~ 1959.
    [47]高静怀,满蔚仕等.广义S变换域有色噪音与信号识别方法[J].地球物理学报,2004,47(5):869~875.
    [48]金雷,李月,杨宝俊.用时频峰值滤波方法消减地震勘探资料中随机噪声的初步研究[J].地球物理学进展,2005,20(3):724~728.
    [49]高静怀,陈文超等.广义S变换与薄互层地震响应分析[J].地球物理学报,
    2003,46(4):526~532.
    [50]王西文,杨孔庆,周立宏等.基于小波变换的地震相干体算法研究[J].地球物理学报,2002,45(6):847~853.
    [51]刘喜武,张宁等.地震勘探信号时频分析方法对比与应用分析[J].地球物理学进展.2008,Vol.23 No.3
    [52]Gabor D. Theory of Communication[J]. Journal of the IEEE.1946,93:429~ 497.
    [53]卫俊平.时频分析技术及应用[D].西安:电子科技大学,2005.
    [54]Jeffrey C, William J. On the existence of discrete Wigner distribution[J]. IEEE Signal Processing Letters,1999,6(12):304~306.
    [55]赵淑红.时频分析方法及其在地震数据处理中的应用[D].长安大学,2006.
    [56]Cohen L. Generalized phase-space distribution functions[J]. Jour. Mat h. Phys, 1966,7:781~787.
    [57]Jeffrey C, William J. Shift covariant time-frequency distributions of discrete signals [J].1999,47(1):133~146.
    [58]Jeffrey C, William J. A function of time, frequency, lagand doppler[J].1999, 47(3):789~799.
    [59]Jeffrey C, Patrick F. Virtues and vices of quartic time-frequency distributions [J]. IEEE Transactions on Signal Processing,2000,48(9):2641~2650.
    [60]Rioul, M.Vetterlil. Wavelet and signal processing[J]. IEEE Signal Processing, 1991,8(4):14~381
    [61]Avijit Chakraborty, David Okaya. Frequency-time decomposition of seismic data using wavelet-based methods[J]. Geop hysics,1995,60(6):1906~1916.
    [62]马世伟.非平稳信号的参数自适应时频表示及其应用的研究[D].上海大学博士论文.2000
    [63]Sheriff R E, Geldart L P.勘探地震学[M].初英,等译.石油工业出版社,1999,第2版
    [64]万学娟.非理想条件下地震面波的性质及压制方法研究[D].中国石油大学硕士论文,2009.5
    [65]关伟.基于小波变换的地震信号去噪方法研究与模拟[D].中国地质大学硕士论文,2008.5

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