三阶累积量在可控震源勘探信号处理中的应用
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摘要
可控震源浅层地震勘探接收信号受环境噪声污染严重。为了提高压制噪声的能力,尝试用三阶累积量为数学工具,求出发射信号与接收信号的三阶互累积量,并把互累积量用发射信号自累积量进行线性分解。根据分解系数序列来检测接收信号中各反射信号分量的存在,并估计各反射信号分量的时间延迟。数值实验结果表明,该方法能从信噪比为0dB的接收信号中准确检测出反射信号分量并估计其时间延迟。鉴于高阶累积量具有屏蔽高斯噪声的优点,其用于可控震源地震勘探信号处理的效果比传统的相关方法要好。
Controlled vibrator shallowlayer seismic exploration data are mixed with strong environment noise. In order to raise the level of depressing noise, this paper tries using threeorder cumulant as mathematics tool of vibrator signal processing. First the threeorder crosscumulant of launched signal and received signal is calculated, then this threeorder crosscumulant is linearly decomposed based on the threeorder cumulant of launched signal. In according to the coefficient series of decomposition, we can detect the reflected signals comprised in the received signal and estimate their timedelays. The results of experiment show that method of threeorder cumulant can detect the reflected signals accurately from received signal whose SNR is 0 dB and estimate their timedelays precisely. Because highorder statistics has the virtue of depressing Gauss noise, as the experiment result shows, the method of threeorder cumulant can show a good effect in processing vibrator signal which is better than that of traditional method of correlation.
引文
[1]陆锦辉,谷亚林,王敏,等.利用高阶统计量方法进行自适应信号处理[J].南京理工大学学报,1999,23(2);43-44.
    [2]何樵登,熊维纲.应用地球物理教程———地震勘探[M].北京:地质出版社,1991.
    [3]陈祖彬.电磁式可控震源相位自适应控制及可控震源系统研究[D].吉林大学博士论文,2002(5):35-39.
    [4]张子三.可控震源地震勘探中基于高阶统计量的信号处理技术研究[D].吉林大学博士论文,2001(5):77-79.
    [5]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,1999.
    [6]CarterGC.TimeDelayEstimationforPassiveSonarSignalProcessing[J].IEEETrans.Acoustics,Speech,SignalProcessing,1981,29(1):463-470.
    [7]TugnaitJK.TimeDelayEstimationwithUnknownSpatiallyCorrelatedGaussianNoise[J].IEEETrans.SignalProcessing,1993,41(3):549-558.
    [8]CarterC.CoherenceandTimeDelayDstimation[J].Proc.IEEE,1987,l7(2):236-255.
    [9]ChenCK,GardnerWA.Signal SelectiveTime Difference of ArrivalEstimationforPassiveLocationofManmadeSignalSourceinHighlyCorruptiveEnvironments[J].IEEETrans.SignalProcessing,1992,40(5):1185-1197.
    [10]BarteltH,LohmannAM,WirnitzerB.PhaseandAmplitudeRecoveryfromBispectra[J].AppliedOptics,1984,26(2):47-49.
    [11]BrewerJW.KroneckerProductsandMatrixCalculusinSystemTheory[J].IEEETrans.onCircuitsandSyst.,1987,35(5):120-123.

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