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Removal of scattered surface waves using multicomponent seismic data

机译:使用多分量地震数据去除散射的表面波

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摘要

We have discussed previously a method for removing scattered surface waves from single-component seismic data based on the estimation of a near-surface scattering model, and we have applied it to both simulated and field data. In the present paper, we extend this method to the multicomponent case. From tests on simulated data, we have found that the multi-component method is more selective in differentiating between body waves and scattered surface waves since it exploits the fact that surface waves and body waves have different states of polarization. The crossline component turns out to be particularly effective for removing the crossline-scattered noise from the vertical component. We have applied the method to a multicomponent field data set. For this case, we have estimated the source waveform and Green's function directly from the data itself. The method results in a good image of the scatterer but can probably be improved by using better estimates of the horizontal and vertical waveforms. There are many ways in which the method, both for single-component and multicomponent data, can be extended. One can think of extending it to laterally varying background models. The method can, in principle, be used to eliminate other near-surface scattering effects like scattered head waves and guided waves, provided that a high-frequency asymptotic expression for these waves is used, or that their propagation characteristics can be estimated from the data. Furthermore, it can be useful to extend the method such that it takes conversions into account, especially head waves converted into Rayleigh waves and vice versa. The method can possibly be used also for obtaining information about shallow heterogeneities for construction purposes and might also be applied to the nondestructive evaluation of materials.
机译:前面我们已经讨论了一种基于近地表散射模型的估计,从单分量地震数据中消除散射面波的方法,并将其应用于模拟和现场数据。在本文中,我们将此方法扩展到多组件情况。通过对模拟数据的测试,我们发现,多分量方法在区分体波和散射表面波方面更具选择性,因为它利用了表面波和体波具有不同极化状态的事实。事实证明,交叉线分量对于从垂直分量中消除交叉线散射的噪声特别有效。我们已经将该方法应用于多分量现场数据集。对于这种情况,我们直接从数据本身估算了源波形和格林函数。该方法可产生良好的散射体图像,但可以通过使用更好的水平和垂直波形估计来改进。对于单成分数据和多成分数据,该方法可以通过多种方式进行扩展。可以考虑将其扩展到横向变化的背景模型。该方法原则上可以用于消除其他近表面散射效应,例如散射头波和导波,只要使用这些波的高频渐近表达式,或者可以根据数据估算其传播特性即可。此外,扩展该方法以使其考虑转换是有用的,尤其是将顶波转换为瑞利波,反之亦然。该方法可能还可以用于出于构造目的获取有关浅层异质性的信息,也可以应用于材料的非破坏性评估。

著录项

  • 来源
    《Geophysics》 |1996年第5期|p.1483-1488|共6页
  • 作者单位

    Shell Research, Volmerlaan 8, 2288 GD Rijswijk, The Netherlands;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

  • 入库时间 2022-08-18 00:20:07

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