首页> 外文期刊>Journal of Seismic Exploration >THE EFFECT OF SIGNAL-TO-NOISE RATIO ON GROUND ROLL ATTENUATION USING ADAPTIVE SINGULAR VALUE DECOMPOSITION: A CASE STUDY FROM THE SOUTH WEST OF IRAN
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THE EFFECT OF SIGNAL-TO-NOISE RATIO ON GROUND ROLL ATTENUATION USING ADAPTIVE SINGULAR VALUE DECOMPOSITION: A CASE STUDY FROM THE SOUTH WEST OF IRAN

机译:自适应奇异值分解的信噪比对地面滚动衰减的影响:以伊朗西南部为例

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Ground roll as a type of coherent noise with high amplitude, low frequency and low velocity masks the reflections in seismic data. Ground roll suppression is one of the important topics in data processing. Adaptive Singular Value Decomposition (ASVD) is a coherency based filter which decomposes data into its eigenimages and can detect horizontal events in the first eigenimages. By using the adaptive method, the ground roll is converted to a horizontal event. By zeroing the first eigenvalues which present ground roll, it can be suppressed. By increasing the number of the eigenvalues to be zeroed, ground roll is better attenuated but more reflections are damaged as well. In this study, this filter is applied to synthetic data with various signal-to-noise ratios (SNR) and two real shot records from the South West of Iran as case studies. The first one was examined with high and low SNRs (with adding the noise). However, in the second one, extensive presence of ground roll and other noises led to an extreme decrease in SNR. Results of applying the filter to the synthetic and field data sets with various SNRs showed that the ASVD filter could attenuate the ground roll with minimum harm to signals and it was not sensitive to SNR, because the eigenvalues were sorted in a descending order in the eigenvalue spectrum. Therefore, after rotating the data, the ground roll as a horizontal and coherent event, was represented in the first eigenvalues. However, the random noise or reflections had lower energies and coherencies compared to the flattened ground roll and they were represented in the next eigenvalues. Due to this separation, the SNR has no impact on the ground roll attenuation via ASVD.
机译:地滚波是一种高振幅,低频和低速度的相干噪声,它掩盖了地震数据中的反射。抑制地滚是数据处理中的重要主题之一。自适应奇异值分解(ASVD)是基于一致性的过滤器,可将数据分解为其特征图像,并可以检测出第一特征图像中的水平事件。通过使用自适应方法,将地面滚动转换为水平事件。通过将出现地面滚动的第一特征值归零,可以将其抑制。通过增加要归零的特征值的数量,可以更好地衰减地滚,但同时也会损坏更多的反射。在本研究中,此过滤器应用于具有各种信噪比(SNR)和来自伊朗西南部的两个真实拍摄记录的合成数据作为案例研究。使用高和低SNR(加上噪声)检查了第一个。但是,在第二种方法中,广泛存在的接地噪声和其他噪声导致SNR极大降低。将滤波器应用于具有各种SNR的合成数据和现场数据集的结果表明,ASVD滤波器可以衰减地滚波,对信号的损害最小,并且对SNR不敏感,因为特征值按特征值降序排列光谱。因此,在旋转数据之后,地面滚动作为一个水平且连贯的事件在第一特征值中表示出来。但是,与平坦的地面波相比,随机噪声或反射具有较低的能量和相干性,它们在下一个特征值中表示。由于这种分离,SNR对通过ASVD的地滚衰减没有影响。

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