Non-stationary adaptive S-wave suppression of ocean bottom node data

IF 3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Geophysics Pub Date : 2024-07-26 DOI:10.1190/geo2023-0779.1
Zhihao Chen, Zhaolin Zhu, Bangyu Wu, Yangkang Chen
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Abstract

Ocean-bottom node (OBN) is widely used because of its wide azimuth, long offset, and low frequency advantages. However, in the vertical component of the OBN geophone, a significant amount of shear waves induced noise may be recorded. This significantly impacts the quality of the vertical component data and may affect the follow-up merging of dual-sensor data. Some commercially available methods apply normal-movement correction, which necessitates velocity data. We avoid this by adaptive matching method, which relies solely on seismic data. Therefore, we developed a novel adaptive subtraction method for S-wave leakage suppression using the horizontal component as the noise model. Our method effectively handles the non-stationarity of the input seismic data in all time and space directions, mitigating instability caused by manual selection of the smoothing radius. A method is introduced for estimating a global non-stationary smoothing radius using the noise model. Compared to the commercial and stationary smoothing methods, our method can better suppress shear wave noise while balancing residual noise and signal leakage more effectively. Both synthetic and field data examples demonstrate significant improvement of the proposed method.
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海底节点数据的非稳态自适应 S 波抑制
洋底节点(OBN)因其方位角宽、偏移长、频率低等优点而被广泛使用。然而,在 OBN 地震检波器的垂直分量中,可能会记录到大量剪切波引起的噪声。这会严重影响垂直分量数据的质量,并可能影响双传感器数据的后续合并。一些市场上销售的方法会应用法向移动校正,这就需要速度数据。我们采用自适应匹配方法避免了这一问题,该方法仅依赖于地震数据。因此,我们利用水平分量作为噪声模型,开发了一种新的自适应减法方法来抑制 S 波泄漏。我们的方法能有效处理输入地震数据在所有时间和空间方向上的非平稳性,减轻了人工选择平滑半径造成的不稳定性。介绍了一种利用噪声模型估算全局非稳态平滑半径的方法。与商业和固定平滑方法相比,我们的方法能更好地抑制剪切波噪声,同时更有效地平衡残余噪声和信号泄漏。合成数据和现场数据实例都证明了所提方法的显著改进。
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来源期刊
Geophysics
Geophysics 地学-地球化学与地球物理
CiteScore
6.90
自引率
18.20%
发文量
354
审稿时长
3 months
期刊介绍: Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics. Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research. Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring. The PDF format of each Geophysics paper is the official version of record.
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