用户名: 密码: 验证码:
基于Hilbert-Huang变换的大地电磁信号处理方法与应用研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
大地电磁测深(Magnetotelluric, MT)是一种以天然交变电磁场为场源的电磁勘探方法,电磁场信号弱、频带宽、极易受各种噪声的干扰,是典型的非线性、非平稳信号。处理MT信号最传统的方法是Fourier变换,而Fourier变换是以平稳信号为理论基础的,与MT信号的非平稳特性相矛盾,且传统方法对MT信号的处理提出了许多前提条件,因此用Fourier变换分析MT信号有着明显的缺陷。Hilbert-Huang变换(Hilbert-Huang transform, HHT)是最新发展起来的,在多个领域已被证明了的分析非平稳信号的强有力工具。本文在分析总结国内外研究成果的基础上,把HHT变换应用到大地电磁信号的处理中来,从基于HHT的大地电磁信号去噪、时频分析、功率谱估计和阻抗估算等几个方面研究其在MT信号处理中的应用方法和应用效果,试图寻找处理MT信号的新途径。
     本文从HHT变换的原理出发,研究了经验模态分解(Empirical Mode Decomposition, EMD)的方法及EMD分解的完备性与局部正交性,给出了EMD分解的流程图,并结合大地电磁信号分析的特点,就EMD分解中存在的端点效应等几个问题,给出了本研究中解决相关问题的方法。以仿真信号为例,给出了HHT方法处理信号的基本流程,分析了Hilbert-Huang变换处理大地电磁信号的优越性。
     Hilbert-Huang变换为信号的去噪提供了一条良好的途径。其EMD分解出来的模态函数(Intrinsic Mode Function, IMF)序列是多通带滤波的结果,且可以完全重构。据此,可以根据噪声的特征构造时空滤波器或采用硬(软)阈值的方法对大地电磁信号进行消噪处理。本文研究了大地电磁测深信号与噪声的特征,提出了基于EMD分解的大地电磁信号去噪原理、方法和步骤,对大地电磁信号中常见的脉冲干扰、矩形干扰、周期干扰和三角波干扰等几种噪声进行了消噪处理,并对实例进行了分析,结果表明本文提出的噪声抑制方法是正确的,有效的抑制了噪声,改善了受干扰数据的质量,获得了稳定的参数估计值。
     时频分析是分析处理非平稳信号的有力工具,它将信号表示为时间和频率的联合函数,揭示信号的时变特征。HHT时频谱克服了其它一些方法的缺陷,具有完全的局部时频特性,可准确描述大地电磁信号的时变特征。基于这些特点,本文在对比研究了短时傅立叶变换、Winger-ville分布、小波变换等几种常用时频分析方法处理大地电磁信号的基础上,给出了MT信号的Hilbert时频谱特征,并研究了Hilbert时频谱在MT信号的噪声识别,分段平稳和数据筛选中的应用方法和应用效果。
     在MT信号处理中最传统也是最主要的谱估计方法还是基于Fourier变换的经典周期图法。而Fourier变换与大地电磁信号非线性,非平稳性的本质相矛盾,这必然导致谱估计的误差。本文在给出Fourier谱估计存在不足的基础上,提出了用Hilbert边际谱来估计大地电磁功率谱的方法,讨论了边际谱的物理意义和分辨率,采用了整体平均和阈值收缩等几种提高谱估计精度的方法,并比较研究了仿真信号和实测大地电磁信号的Fourier谱和Hilbert边际谱,分析了用Hilbert边际谱来估计大地电磁功率谱方法的优越性。
     大地电磁法主要以视电阻率曲线和相位曲线的形态特征作为分析大地结构与电性分布的基本依据,因此阻抗估算是大地电磁法研究中最基本的内容之一。而由于MT信号表现出非平稳的特征,引起阻抗估算结果也具有时变特征,因此,从瞬时谱上统计估算参量比Fourier分析更有利于实现稳健估计。论文提出了从HHT瞬时谱上统计估算阻抗张量的瞬时谱方法,给出了基于HHT边际谱估算阻抗张量的数学模型及其流程图;用数值模拟验证了方法的正确性,并对实测MT数据进行了分析;建立了基于HHT的大地电磁资料处理流程,并对一测线进行了处理分析。结果表明由HHT瞬时谱统计估算的阻抗张量最小化了大地电磁信号非平稳性带来的估算偏差,估算参量具有更好的稳健性,曲线形态也更加合理,圆滑,且在低信噪比情况下本文方法较传统方法有更强的抗干扰能力。
     通过以上几个方面的研究表明Hilbert-Huang变换是一种有效的处理非平稳信号的方法,能成功的应用于大地电磁信号去噪、时频分析、功率谱估计和阻抗估算等几个方面,且具有一定的优越性,为大地电磁信号处理提供了一种新的途径。
Magnetotelluric(MT) sounding is a kind of electromagnetic exploration method which uses natural alternating electromagnetic field as a field source. While MT signal is a typical non-linear and non-stationary signal because it is weak, bandwidth and highly vulnerable to be disturbed. The traditional methods of analysis determine the spectra using variations of the Fourier Transform (FT) and must assume that the signals under analysis are stationary over the record length. Because the FT is based on the theory of stationary signal and is ambivalent to the characteristic of MT signal. Therefore, analysis method of MT signal using Fourier transform has obvious flaws. In recent years, the Hilbert-Huang Transform (HHT) has been regarded as a powerful tool for adaptive analysis of non-linear and non-stationary signals and has received much attention in the signal processing community. This paper proposes for the first time the adoption of a new method of analysis for MT data, and focuses on noise suppressing, time-frequency analysis, power spectrum estimation and impedance estimation that are facilitated by applying the HHT.
     In this paper, starting with the principle of the HHT transform, the empirical mode decomposition (EMD) and the completeness and local orthogonality of EMD are studied. The flow chart of EMD is given. And combined with the characteristic of MT signal, some noduses that exist on the EMD, such as fluctuations, end effects and sifting-stopping criteria, are studied and given the method to resolve the relevant problems. Taking a simulative signal as an example, the basic flow of signal processing based on HHT is given and the superiority of Hilbert-Huang transform to analyze the MT signals is verified.
     The innovation of the HHT method brings a new way to filter data and reduce noise. The EMD filters signal with different time scales and is adaptive to signal. The intrinsic mode function (IMF) is result of multi-band filtering and can be completely reconstructed. Using the structural characteristics of the IMF, some new space-time filters and a hard (soft) threshold method can be realized to de-noise. This paper studies the characteristics of MT signal and its noise. The principle and step of de-noising method based on EMD are given. Some noises, such as impulse jamming, rectangle disturbing and sine wave noise, are analyzed and processed for the actual MT data. The results show that the de-noising method is effective and the quality of MT data is improved greatly. The EMD method can achieves stationary and reliable parameter estimations.
     Time-frequency analysis is a powerful tool for non-stationary signal processing. It will express signal as a joint function of time and frequency and reveal the time-varying characteristics of the signal. HHT method has overcome the shortcomings of other ways, completes abolition of the role of the window function and is not restricted with nuclear function and Heisenberg principle. Hilbert-Huang spectrum can precisely describe the nonlinear and non-stationary characteristics of MT signals. This paper compares the different time-frequency spectrums that are from several commonly method such as short time Fourier transform, Wigner-Ville distribution and Wavelet transform. Based on these characteristics, the time-frequency characteristics of HHT spectrum of MT signal are studied. Then Hilbert time-frequency spectrum is used in the MT signal noise recognition, data filtering and sub-smooth. Its application methods and application results are studied in this thesis.
     Power spectrum estimation takes an important role in MT signal processing. The most traditional and the most important power spectrum estimation method is the classical periodogram method which bases on the Fourier transform. The Fourier transform contradicts the non-linear, non-stationary nature of MT signal, which will inevitably lead to spectral estimation error. A new spectrum estimation method based on Hilbert-Huang transform is proposed in this paper. Firstly the marginal spectrum method based on HHT is presented and the linear property of marginal spectrum is demonstrated. Then, compared with the FT method, the physical signification and the preponderance of marginal spectrum for MT signal are further discussed. And some methods to improve the precision of spectrum estimation are proposed in detail. Finally the simulative data and the practical MT data are analyzed. The simulation and results of real data indicate that the HHT method suits the nature of MT signal much more.
     The characteristics of apparent resistivity and phase curves are mainly basis for analyzing the structure of the earth and distribute of conduction in MT sounding. Therefore analyzing, calculating and processing of impedance are one of the most basis and importance works. The non-stationary characteristics of MT signal cause that impedance estimation results have time-varying characteristics. Therefore, using time-frequency analysis methold to estimate parameters from the instantaneous spectrum are more conducive to robust estimation comparing with Fourier methold. This paper proposes a kind of instantaneous spectrum method to estimate impedance tensor based on the HHT marginal spectrum. The flow chart and mathematics model are given. Some simulative signal and a place of measured MT signals is processed. The results shows that the impedance tensor obtained from the HHT transient spectrum minimizes the estimation warp brought about by the non-stationary characteristics of MT data, and the estimated parameter is more stable and reliable than that from conventional methods. The parameter curves are less bars and more smooth, reasonable. The interpretability of data has been significantly improved.
     Through the above studies, the results show that the Hilbert-Huang transform is an effective method to deal with the non-stationary signals and provides a new way to process MT signal. HHT method has a wide application on MT signal noise suppressing, time-frequency analysis, power spectrum estimation and impedance estimation.
引文
[1]Tikhonov A N. Determination of the electrical characteristics of the deep strata of the Earth's crust[J]. Dokl. Akad. Nauk SSR,1950,73:295-311
    [2]Tkhonov A N. On the transient electric current in a homogeneous conducting halfspace[J]. Geofiz,1946,10(3):386-397
    [3]Cagniard L. Basic theory of the magnetotelluric method of geophysical prospecting[J]. Geophysics,1953,18:605-636
    [4]刘国栋,邓前辉.电磁方法研究与勘探[M].北京:地震出版社,1993,32-45
    [5]魏文博.我国大地电磁测深新进展及瞻望[J].地球物理学展,2002,17(2):245-254
    [6]Kavfman A A and Keller G V. The magnetotelluric sounding method[J]. Elesvier, 1981,595-598
    [7]朴化荣.电磁测深法原理[M].北京:地质出版社,1990,12-16
    [8]严家斌,柳建新,何继善.基于相关归—ROBUST海底大地电磁数据处理[J].地球物理学报,2003,46(2):241-245
    [9]Chen L S, Booker J R, Jones A G, et al. Electrically conductive crust in southern Tibet from INDEPTH magneto-telluric surveying[J]. Science,1996,274 (5293): 1694-1696
    [10]Wei W B, Ulrich, Jones A, et al. Detection of Wide-spread fluids in the Tibetan Crust by magnetotelluric studies[J]. Science,2001,292:716-718
    [11]刘国栋.电磁法和电磁法仪器新进展[M].北京:北京欧华联科技有限责任公司,2007
    [12]王书明,王家映.大地电磁信号统计特征分析[J].地震学报,2004,26(6):669-674
    [13]王书明,王家映.关于大地电磁信号非最小相位性的讨论[J].地球物理学进展,2004,19(2):216-221
    [14]严家斌.大地电磁信号处理理论及方法研究[D],长沙,中南大学,2003
    [15]杨生.大地电磁测深法环境噪声抑制研究及应用[D],长沙,中南大学,2004
    [16]D.o.Trad and J.M.Travassos. Wavelet filtering of magnetotellurie data[J]. Geophysics,2000,65,482-491
    [17]米萨克 N.纳比吉安.勘查地球物理电磁法(第一卷理论)(赵经祥译)[M]. 北京:地质出版社,1992
    [18]A.A.Kaufman, G.V.Keller.频率域和时间域电磁测深[M].北京:地质出版社,1987
    [19]傅良魁.应用地球物理教程[M].北京:地质出版社,1991
    [20]刘国栋,陈乐寿.大地电磁测深法研究[M].北京:地震出版社1984
    [21]周熙襄,钟本善.电法勘探数值模拟技术[M].成都:四川科学技术出版社,1986
    [22]Kerry Key, C. W. Adaptive finite-element modeling using unstructured grids: The 2D magnetotelluric example[J]. Geophysics,2006,71(6):291-299
    [23]Martyn J, U, Bryan J, Alan D. Chave. Electromagnetic induction by a finite electric dipole source over a 2-D earth[J]. Geophysics,1993,58(2):198-214
    [25]罗延钟,张桂青.频率域激电法原理[M].北京:地质出版社,1988
    [26]罗延钟,张桂青.电子计算机在电法勘探中的应用[M].武汉:武汉地质学院出版社,1987
    [27]Mitsuhata, Y.2-D electromagnetic modeling by finite-element method with a dipole source and topography [J]. Geophysics,2000,65(2):465-475
    [28]杨长福,徐世浙.国外大地电磁研究现状[J].物探与化探,2005,29(3):244-247
    [29]Huang, N.E, Long, S.R, Shen, Z. Frequency downshift in nonlinear water wave evolution[J]. Adv Appl Mech,1996,32:59-117
    [30]Huang, N.E, Shen, Z, Long, S.R, Wu, et al. The empirical mode decomposition and the Hilbert spectrum for nonlinear and non-stationarity time series analysis[J]. Proc R Soc London, Ser A,1998,454:903-995
    [31]Huang, N.E, Wu, M.C, Long, S.R, et al. A confidence limit for the empirical mode decomposition and the Hilbert spectral analysis[J]. Proc R Soc London, Ser A,2003,459:2317-2345
    [32]Huang, N.E. The Hilbert-Huang transform in engineering[M]. Boca Raton: CRC Press,2005
    [33]张义平,李夕兵.Hilbert-Huang变换在爆破震动信号分析中的应用[J].中南大学学报(自然科学版).2005,36(5):882-827
    [34]Rato, R. T, Ortigueira, M.D, Batista, A.G. On the HHT, its problems and some-solutions[J]. Mechanical Systems and Signal Processing,2008, 22:1374-1394
    [35]Rong, J, Hong, Y. Studies of spectral properties of short genes using the wavelet subspace Hilbert-Huang transform (WSHHT) [J]. Physics A,2008, 387:4223-4247
    [36]林君,项葵葵,朱宝龙等.MT信号现场处理的实现技术研究.数据采集与处理[J].1997,12(1):52-55
    [37]李夕兵,张义平,左宇军等.岩石爆破振动信号的EMD滤波与消噪[J].中南大学学报(自然科学版).2006,37(1):150-154
    [38]Peng Z K, Tse P W, Chu F L. An improved Hilbert-Huang transform and its application in vibration signal analysis[J], Journal of Sound and Vibration, 2005,268:187-205
    [39]孙洁,晋文光,白登海等,大地电磁测深资料中的噪声干扰[J],物探与化探,2000,24(2):119-127
    [40]汤井田,何继善.可控源音频大地电磁法及其应用[M].长沙:中南大学出版社,2005
    [41]化希瑞,高频大地电磁系统数据处理方法研究[D],长沙,中南大学,2007
    [42]VozoffK. The magnetotelluric method in the exploration of sedimentary basins[J]. Geophysics,1972,37:98-141
    [43]Hermance J F. Processing of magetotelluric data[J]. Phys. Earth Planel Interiors.1973,7:349-364
    [44]陈乐寿,刘任,王天生.大地电磁测深资料处理与解释[M].北京:石油工业出版社,1989
    [45]Bahr K. Interpretation of the magnetotelluric impedance tensor, regional in duction and local telluric distortion[J]. Geophysics,1989,62:119-129
    [46]Szarka, Geophysical aspects of man-made electromagnic noise in the Earth a review Surv[J]. Geophysics,1988,9:287-318
    [47]Wight D E, H W Bostick. Real time fourier transformation of magnetotelluric Data. Electrical Geophysical Research Laboration the University of Tex as Austin,1977
    [48]Junge, Characterization of and correction for cultural noise. Surv[J]. Geophysics,1996,17:361-391
    [49]Kao, D. W. and Rankin, D. Enhancement of signal-to-noise ratio in magnetotelluric data[J], Geophysics,1977,142:103-110
    [50]T. M. Gamble, W. M. Goubau, J. Clarke, Magnetotelluric Data analysis: removal of Bias[J], Geophysics,1978,43:1157-1169
    [51]T. M. Gamble, W. M. Goubau, J. Clarke. Error analysis for remote reference Magnetotelluric[J], Geophysics,1979,44:959-968
    [52]T. M. Gamble, W. M. Goubau, J. Clarke,Magnetotelluric with a remote magnetic reference [J], Geophysics,1979,44:53-68
    [53]黄哲.大地电磁测深法远参考原理及效果分析.地震地质[J],2001,23(2):212-216
    [54]陈高,金祖发,马永生等.大地电磁测深远参考技术及应用效果[J].石油物探,2001,40(3):112-117
    [55]严良俊,胡文宝,陈清礼等.远参考MT方法及在南方强干扰地区的应用[J].江汉石油学院学报,1998,20(4):34-38
    [57]陈清礼,胡文宝,苏朱刘等.长距离远参考大地电磁测深试验研究[J].石油地球物理勘探,2002,37(2):145-148
    [58]Oliver Ritter, A Junge and J K Dawes. New equipment and processing for magnetotelluric remote reference observations[J].Geophys,1998,132:535-548
    [59]J. C. Larsen, R. L. Mackie. Robust smooth magnetotelluric transfer Functions[J]. Geophysics.1996,124:801-819
    [60]D.Egbert and R. Booker, Robust estimation of geomagnetic transfer function[J]. Geophysics.1986,87:173-194
    [61]D.Sutarno and K.Vozoff. Phase-smoothed robust M-estimation of magnetotelluric impedance function[J]. Geophysics,1991,56:1999-2007
    [62]Chave Thomson and Ander, The estimation of power spectra, coherencies, and transfer functions[J]. Geophysics,1987,92:633-648
    [63]Egbert. Robust multiple-station magnetotelluric data processing[J]. Geophysics, 1997,130:475-496
    [64]Jones, Chave, Egbert, et al. A comparison of techniques for magnetotelluric response function estimation[J]. Geophysics,1994,116:14201-14213
    [65]Larsen. Transfer function:smooth robust estimates by least squares and remote reference methods[J]. Geophysics,1989,99:645-663
    [66]江钊.Robust估计及其在大地电磁资料处理中的初步应用.电磁方法研究与勘探[M].北京:地震出版社,1993
    [67]Sutarno D, Vozoff K. Robust M-estimation of magnetotelluric impedance tensors[J]. Expl. Geophysics,1989,20:383-398
    [68]林长佑,武玉霞,刘晓玲.大地电磁响应函数的除偏估算和误差的研究[J].西北地震学报,1988,10(3):25-38
    [69]严良俊.远参考MT方法及其在南方强干扰地区的应用[J].江汉石油学院学报,1998,20(4):68-74
    [70]刘国栋.我国大地电磁测深的发展.地球物理学报[J],1994,37(增刊)):301-310
    [71]李建平.小波分析与信号处理[M],重庆:重庆出版社,1997
    [72]Mallat S.H, Wang. Singularity detection and processing with wavelet[J], IEEE Trans on Information Theory,1992,38(2):617-643
    [73]G. Mallat. A theory for multi-resultion signal decomposition the Wavelet representation[J]. IEEE, Transactions on pattern analysis and machine intelligence,1989,7:674-693
    [74]邓贵忠,邸双亮.小波分析及其应用[M].西安:西安电子科技大学出版社,1992
    [75]王建忠.小波理论及其在物理与工程中的应用[J].数学进展,1992,21:289-316
    [76]宋守根,汤井田,何继善.小波分析与电磁测深中静态效应的识别、分离及压制[J],地球物理学报.1995,(38):120-128
    [77]徐义贤,王家映.有限长谐波信号的小波谱[J].中国学术期刊文摘,1999,5(2):192-193
    [78]徐义贤,王家映.小波谱及其对谐波信号的刻画能力[J].石油地球物理勘探,1999,34(1):22-28.
    [79]徐义贤,王家映.基于连续小波变化的大地电磁信号谱估计方法[J],地球物理学报,2000,43,676-683
    [80]师学明,王家映,张胜业等,多尺度逐次逼近遗传算法反演大地电磁资料[J].地球物理学报,2000,43:122-129
    [81]刘宏.小波分析在MT去噪处理中的适定性[J].石油地球物理勘探,2004,39(4):331-337
    [82]Rosenblatt M, Van Ness J W. Estimation of the bispectrum[J]. Ann. Math. Statzst.1965,36(1):1120-1136
    [83]Brillinger D R. An introduction to polyspectral[J]. Ann. Math. Statzst.1965, 36(1):1351-1374
    [84]Mendel J M, Tutorial on higher-order statistics in signal and system theory. theoretical results and some applications [J].IEEE,1991,79(3):278-305
    [85]Nikias C L, Raghuveer M R. Bispectrum estimation:a digital signal processing framework[J]. IEEE,1987,75(5):869-891
    [86]张贤达.时间序列分析—高阶统计量方法[M].北京:清华大学出版社,1996
    [87]李宏伟,程乾生.高阶统计量与随机信号分析[M].武汉,中国地质大学出版社,2002
    [88]杜宁平,史军,朱红涛等.高阶统计量分析在油气预测中的应用[J],海洋地质动态,2004,20,(8):27-29
    [89]王书明,王家映,利用高阶谱重构功率谱抑制高斯有色噪声[J].科学技术与工程,2004,4(2):69-73
    [90]王书明,王家映,高阶统计量对大地电磁测深资料处理方法的改进[J].石油地球物理勘探,2004,(增刊):1-4
    [91]王书明,李宏伟,王家映等.地球物理学中的高阶统计量方法[M].北京:科学出版社,2006
    [92]王书明,王家映.高阶统计量在大地电磁测深数据处理中的应用研究[J].地球物理学报,2004,47(5):928-933
    [93]王通.大地电磁测深信号的高阶谱估计及应用研究[D],2006,长沙,中南大学
    [94]Velis D R, Ultych T J. Simulated annealing wavelete stimation via fourth-order cumulant matching[J]. Geophysics,1996,61(6):1939-1948.
    [95]白大为,底青云,王光杰等.Hilbert-Huang变换与ELF信号处理[J],地球物理学进展,2009.3:1032-1038
    [96]Tournerie B, Chouteau M. Estimation and removal of the MT static shift effect using geostatistical methods[J].17th IAGAWG 1-2 Workshop on EM Induction in the Earth, Hyderabad, India,2004,18-2
    [97]张翔,张世忠.小波变换在大地电磁测深静校正中的应用[J].江汉石油学院学报,2002,24(2):40-41.
    [98]Jones Alan G. Static shift of magnetotelluric data and its removal in a se dimentary basic envlronment[J]. Geophysics,1988,49(7):967-978
    [99]Groom R W, Bailay R C. Analytical investigations of the effects of near-surface three-dimensional galvanic scatters on MT tensor decompositions [J].1991, Geophysics,56:496-518.
    [100]Sternberg, B.k, Washburne, J.C. Correction for the static shift in Magnetotellutic using transient electromagnetic soundings[J]. Geophysics, 1988,53:987-998
    [101]罗延钟.可控源音频大地电磁法的静态效应校正[J].物探与化探,1991,(5):196-202
    [102]J.Maenae, L.Lay, et al. Measurement of static shift in MT and CSAMT surveys[J]. Exploration Geophysics,1998, (129):494-498
    [103]H.F.Morrison, E.A.Nichols, et al. Continuous MT profiling for Petroleum and mineral Prospecting[J]. Electromagnetic Instruments Ine. Inc,1994
    [104]汤井田,何继善.静效应校正的波数域滤波方法[J].物探与化探.1993,17:209-216
    [105]C.Torres-Verdin, F.X.Bostick, Prineiples of spatial surfaee Eleetric field filtering in magnetotelluric:Electromagnetic array profiling(EMAP) [J]. Geophysics,1992,57 (4).603-622
    [106]李韦文.浅层电性不均匀体对大地电磁测深的影响及其校正[J].电磁方法研究与进展,1993,(3):125-133
    [107]罗延钟,万乐.可控源音频大地电磁法[J].电法勘探新进展,1996,(5):28-48
    [108]付海燕.基于分形插值的大地电磁静校正方法[J],石油天然气学报(江汉石油学院学报),2006,28(6):77-83
    [109]Come J. P. Proceedings of the effects of Earthquake Frequency Non-stationarity on Inelastic Structural Response[J]. Proceeding of the 10th world Conference on Earthquake Engineering,1992, A.A. Balkema:Rotterdam, The Netherlands
    [110]Harm S. J. Hilbert Transforms in Signal Processing[M]. Artech House: Boston.1996
    [111]Cohen, L. Time-Frequency Analysis:Theory and Applications[M]. Prentice-Hall, Inc, Englewood Cliffs, N.J,1995
    [112]S.Q.Rice, Mathematical Analysis of random Noise. Ⅲ. Statistical Properties of Random Noise Currents[J], J.Bell Sys.Tech,1945,24:46-108
    [113]S.Q.Rice, Mathematical Analysis of Random Noise Ⅳ. Noise through Nonlinear Devices[J], J.Bell Sys. Tech,1945,24:109-156
    [114]M.S.Longuet-Higgins. The Instabilities of Gravity Waves of Niter Amplitude in Deep Water.II. Subharmonics[J], Proc.R.Soc.London.A,1978,360:489-505.
    [115]钟佑明.希尔伯特—黄变换局瞬信号分析理论的研究[D],重庆,重庆大学,2002
    [116]谭善文.多分辨希尔伯特—黄变换方法的研究[D],重庆,重庆大学,2001
    [117]程军圣,于德介,杨宇.基于支持矢量回归机的Hilbert-Huang变换端点效应问题的处理方法[J].机械工程学.2006,42(4):23-31
    [118]邓拥军,王伟,钱成春等.EMD方法及Hilbert变换中边界问题的处理[J].科学通报.2001,46(3):257-263
    [119]张郁山,梁建文,胡幸贤.应用自回归模型处理EMD方法中的边界问题[J]自然科学进展.2003,13(10):1054-1059
    [120]盖强,马孝江,张海勇等.一种消除局域波法中边界效应的新方法[J].大连理工大学学报.2002.42(1):115-117
    [121]黄大吉,赵进平,苏纪兰.希尔伯特—黄变换的端点延拓[J].海洋学报.2003,25(1):1-11
    [122]刘慧婷,张昊,程家兴.基于多项式拟合算法的EMD端点问题的处理[J].计算机工程与应用.2004,(16):84-86
    [123]陈忠,郑时雄.EMD信号分析方法边缘效应的分析数据采集与处理[J].2003,18(1):114-118
    [124]盖强.局域波时频分析方法的理论研究与应用[D].大连,大连理工大学,2001·
    [125]毛炜,金荣洪,耿军平等,一种基于改进Hilbert-Huang时频分析法及其应用[J].上海交通大学学报,2006,40(5):721-726
    [126]曾治权.日地关系[M].北京:地质出版社,1989
    [127]陈乐寿,王光锷.大地电磁测深法[M].北京:地质出版社,1990
    [128]孙景群.大气电学基础[M].北京:气象出版社,1987
    [129]孙洁,晋光文,白登海等,大地电磁测深资料的噪声干扰[J].物探与化探,2000,24(2):119-128
    [130]Keller G V, Frischknecht. Electrical methods in geophysical prospecting[M]. Oxford, Pergamon Press,1966
    [131]Cantwell T. Detection and analysis of low-frequency magnetotelluric Signals: [D].MIT:1960
    [133]A.A考夫曼凯勒.大地电磁测深法[M].北京:地质出版社,1987
    [134]荒木忠次,高杉真司,筿原信男.MT法概论[J],1982,7(3):1-52
    [135]Morrison H F, Wombell E, Ward S H. Analyses of earth impedance using magnetotelluric field[J]. Geophysics,1968,73(8):2769-2778
    [136]Huang N E, Shen Zheng Long, Steven R. A new view of nonlinear water waves:the Hilbert spectrum[J]. Annual Review of Fluid Mechanics, 1999:417-457
    [137]Flandrin G, Rilling G, Goncalves P. Empirical mode decomposition as a filter
    bank[J]. IEEE Signal Processing,2004,11(2):112-114
    [138]汤井田,化希瑞,曹哲民,等.Hilbert-Huang变换与大地电磁噪声压制[J].地球物理学报,2008,51(2):603-610.
    [139]Donoho D L, JOHNSTONE I. Wavelet shrinkage asymptopia [J]. Journal of. Royal Statistical Society,1995,57 (2):301-369
    [140]Donoho D L. Denoising by soft-thresholding[J]. IEEE Trans on Information Theory,1995,41(3):613-627
    [141]陈清礼,胡文宝.利用地表电阻率校正大地电磁静态偏移[J].物探与化探,1999,23(4):289-295
    [142]严良俊,胡文宝.电磁勘探方法及其在南方碳酸盐岩地区的应用[J].北京:石油工业出版社,2001
    [143]杨生,鲍光淑.MT法中静态效应及阻抗张量静态校正法[J].中南工业大学学报,2002,33(1):8-13
    [144]Bailey R C. Decomposition of magneto-telluric impedance tensors in the presence of local three-dimensional galvanic distortion[J]. Journal of Geophysical Research,1989,94 (B2):1913-1925
    [145]Alan G Jones. Static shift of magnetotelluric data and its removal in a sedimentary basin environment [J]. Geophysics,1988,53 (7):967-978
    [146]科恩L.时-频分析:理论与应用[M].白居宪译.西安:西安交通大学出版社,1998.
    [147]邹红星,周小波,李衍达.时频分析:回溯与前瞻[J],电子学报,2000,9(28):78-83
    [148]张义平,李夕兵,赵国彦等.爆破震动信号的时频分析[J].岩土工程学报,2000,12(27):1472-1477
    [149]张贤达.现代信号处理(第二版)[M].北京:清华大学出版社,2002.
    [150]S Qian, D Chen. Joint Time-Frequency Analysis[J], Prentice-Hall.1996, p: 109-132
    [151]陈君,闫述,李正斌.联合时频分析在电磁测深问题中的应用[J],电波科学学报,2003,8(4):393-400
    [152]陈明生,李正斌,闫述.瞬变电磁法资料的联合时-频分析初探[J].煤田地质与勘探.1993,27(3):55-57
    [153]J. Morlet, G. Arens, E. Fourgeau and D. Giard, Wave Propagation and Sampling Theory-Part:Sampling Theory and Complex Waves[J]. Geophysics, 1982, (2):222-236
    [154]张义平,李夕兵,赵国彦等.爆破震动信号的小波分析与HHT变换[J],爆炸与冲击,2005,11(6):528-536
    [155]孙晖,经验模态分解理论与应用研究[D],杭州,浙江大学,2005
    [156]李浩,谢桂海,杨磊等.Hilbert谱分析和平稳度[J].军械工程学院学报,2007,19(2):44-47
    [157]郑君里,应启布,杨为理.信号与系统[M].北京:高等教育出版社,2000
    [158]钟佑明,金涛,秦树人.希尔伯特—黄变换中的一种新包络线算法[J].数据采集与处理.2005,20(1):13-17
    [159]皇甫堪,陈建文,楼生强.现代数字信号处理[M].北京:电子工业出版社,2003.
    [160]Hayes M H. Statistical Digital Signal Processing and Modeling[M]. New York:John Wiley & Sons, Inc,1996
    [161]钟佑明,秦树人,汤宝平.希尔伯特-黄变换中边际谱的研究[J],系统工程与电子技术,2004,26(9):1323-1327
    [162]张海勇.一种新的非平稳信号分析方法-局域波分析[J].电子与信息学报.2003,25(10):1327-1334
    [163]盖强,张海勇,徐晓刚.Hilbert-Huang变换的自适应频率多分辨分析研究[J].电子学报,2005,33(3):563-566
    [164]Yue H Y, Guo H D. A SAR interferogram filter based on the empirical mode decomposition method[J]. Geosoience and Remote Sensing Symposium. IGARSS 01,2001:206-2063
    [165]丁宏,戴逸松,石要武.采用小波变换对短数据信号的谱估计方法[J],电子学报,1997,25(1):11-14
    [166]Torrence C and Compo G P. A practical guide to wavelet analysis.Bull[J]. Amer. Metero. Soc,1998,79(1):61-78.
    [167]Dowine T R, Silverman B W. The discrete multiple wavelet transform and threshold methods[J]. IEEE Transactions on Signal processing,1998, 46(9):2558-2561
    [168]黄永平.Hllbert-Huang变换及其若干改进研究[D],哈尔滨,哈尔滨工程大学,2007
    [169]Chant, I.J, Hastie, L.M. Time-frequency analysis of magnetotelluric data[J]. Geophysics,1992,111:399-413
    [170]Chant, I. J, Hastie, L.M. The Wigner-Ville analysis of magnetotelluric signals[J], Proceedings Geological Soc. of Australia,1990,25:89-90
    [171]Berdichevskii, M.P. Magnetotelluric sounding with applications to mathematical filters[J], Physics of the Earth,1973,3:68-76.
    [172]陈乐寿,白改先.处理大地电磁资料的瞬时谱方法[J].石油地球物理勘探,1984,12(6):562-574
    [173]A.G. Jones A.D.Chave, A comparison of Techniques for Magnetotellurie Response function estimation[J], Journal of geophysical research,1989,94: 14201-14213
    [174]王家映,地球物理反演理论[M],北京:中国地质大学出版社,1998
    [175]Yoonho Song, Hee Joon Kim, Ki Ha Lee. High-frequency electromagnetic impedance method for subsurface imaging[J]. Geophysics,2002,67 (2): 501-510
    [176]Basokur. A T. Definition of apparent resistivity for the presentation of magnetotelluric sounding data[J]. Geophysical Prospecting,1994,42:141-149
    [177]Sims.W.E, Bostick.F.X, Smith.H.W. The estimation of magnetotelluric impedance tensor element from measured data[J]. Geophysics,1971, 36:538-542
    [178]Bradley, M.B, Camelia, K. Application of the empirical mode decomposition and Hilbert-Huang transform to seismic reflection data[J]. Geophysics,2007, 72:29-37

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700