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首页> 外文期刊>Journal of Applied Geophysics >Enhancing low-wavenumber components of full-waveform inversion using an improved wavefield decomposition method in the time-space domain
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Enhancing low-wavenumber components of full-waveform inversion using an improved wavefield decomposition method in the time-space domain

机译:在时空域中使用改进的波场分解方法增强全波形反演的低波纹组件

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摘要

Full-waveform inversion (FWI) is a successful technique that attempts to build high-resolution velocity models by minimizing the residuals between observed and calculated data after a series of iterations. However, its successful application still relies on the quality of the estimated initial velocity model, as well as on the design of a suitable hierarchical workflow. If the initial model is far away from the true model, the widely used gradient based FWI will inevitably get trapped into meaningless local minima. Given that the properties of the low-wave number components can help construct the initial model and overcome cycle skipping, we propose a low-wave number update FWI method based on the Hilbert transform called the hybrid method. This method provides a new form of FWI in the time-space domain that appears to be capable of enhancing the low-wavenumber updates. In this method, the updates of low wavenumbers and high wavenumbers are divided into two parts. In the first step, a gradient formula based on the Hilbert transform plays a key role in updating the low-wavenumber components. The gradient is formed by cross-correlation of upgoing and downgoing waves of source and residual wavefields. Instead of using the wavefield decomposition method in the frequency-wavenumber domain with high computational complexity, we apply a novel method to extract the upgoing and downgoing wavefields in the time-space domain. In addition to the acceptable computational burden, the memory is reduced greatly. The second step is the standard FWI, and its task is to update the high-wavenumber components. Numerical tests on an anomaly model and the Marmousi model demonstrate the effectiveness of the hybrid method for extracting low-wavenumber components even for noisy data or when low-frequency data are missing. (C) 2018 Elsevier B.V. All rights reserved.
机译:全波形反转(FWI)是一种成功的技术,它通过最小化在一系列迭代之后最小化观察和计算的数据之间的残差来建立高分辨率速度模型。然而,其成功的应用仍然依赖于估计的初始速度模型的质量,以及适当的分层工作流程的设计。如果初始模型远离真实模型,则广泛使用的基于梯度的FWI将不可避免地被困成无意义的局部最小值。考虑到低波数组件的特性可以帮助构造初始模型并克服周期跳跃,我们提出了一种基于称为混合方法的Hilbert变换的低波数更新FWI方法。该方法在似乎能够增强低波纹更新的时空域中提供了一种新的FWI形式。在该方法中,低波纹和高波纹的更新被分成两部分。在第一步中,基于Hilbert变换的梯度公式在更新低波数组件时起着关键作用。梯度是通过源极和残留波场的上行和衰减波的互相关而形成的梯度。不使用具有高计算复杂度的频率 - 波数域中的波场分解方法,而是应用一种新的方法来提取时间空间域中的上行和倒波。除了可接受的计算负担之外,内存还会大大减少。第二步是标准的FWI,其任务是更新高波纹组件。异常模型和Marmousi模型的数值测试证明了即使对于噪声数据或缺少低频数据,甚至缺少低波数部件的混合方法的有效性。 (c)2018 Elsevier B.v.保留所有权利。

著录项

  • 来源
    《Journal of Applied Geophysics 》 |2018年第2018期| 共13页
  • 作者单位

    China Univ Petr CNPC Key Lab Geophys Explorat State Key Lab Petr Resources &

    Prospecting Beijing 102249 Peoples R China;

    China Univ Petr CNPC Key Lab Geophys Explorat State Key Lab Petr Resources &

    Prospecting Beijing 102249 Peoples R China;

    China Univ Petr CNPC Key Lab Geophys Explorat State Key Lab Petr Resources &

    Prospecting Beijing 102249 Peoples R China;

    Beijing Foreign Studies Univ Beijing 100089 Peoples R China;

    China Univ Petr CNPC Key Lab Geophys Explorat State Key Lab Petr Resources &

    Prospecting Beijing 102249 Peoples R China;

    China Univ Petr CNPC Key Lab Geophys Explorat State Key Lab Petr Resources &

    Prospecting Beijing 102249 Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学 ;
  • 关键词

    Full-waveform inversion; Hilbert transform; Wavefield decomposition; Low-wavenumber updates;

    机译:全波形反转;希尔伯特变换;波场分解;低波浪更新;

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