A reflection-based efficient wavefield inversion to retrieve a good initial background velocity

Chao Song, T. Alkhalifah
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引用次数: 1

Abstract

Full-waveform inversion (FWI) requires either a good initial velocity model or low-frequency data to mitigate the cycleskipping issue. Reflection-waveform inversion (RWI) uses a migration/demigration process to retrieve a background model that can be used as a good initial velocity in FWI. The drawback of the conventional RWI is that it requires the use of a least-squares migration, which is often computationally expensive. Efficient wavefield inversion (EWI) is a recently developed method from wavefield reconstruction inversion (WRI). EWI uses a modified source function to introduce the multiscattering components in the reconstructed wavefield. However, when the initial velocity is far from the true one, the wavefield can not be accurately reconstructed. We incorporate the RWI formulation into EWI by inverting for the Born scattered wavefield instead of the wavefield itself. In this case, we use the perturbation related to secondary sources as a modified source function. As the sources in the reflection-based EWI (REWI) are located in the subsurface, we are able to update the background model along the reflection wave path. We calculate the background model perturbation by a deconvolution process in each frequency like what is done in the original EWI. We demonstrate the validity of the proposed approach using synthetic data generated for the Marmousi model.
一种基于反射的有效波场反演,以检索良好的初始背景速度
全波形反演(FWI)需要良好的初速度模型或低频数据来减轻周期跳变问题。反射波形反演(RWI)使用偏移/反偏移过程来检索背景模型,该模型可作为FWI中良好的初始速度。传统RWI的缺点是它需要使用最小二乘迁移,这通常在计算上很昂贵。高效波场反演(EWI)是在波场重建反演(WRI)的基础上发展起来的一种新方法。EWI采用一种修正的源函数来引入重构波场中的多散射分量。然而,当初始速度与真实速度相差较大时,无法准确地重建波场。我们通过对玻恩散射波场而不是波场本身进行反演,将RWI公式纳入EWI。在这种情况下,我们使用与次级源有关的扰动作为修改的源函数。由于基于反射的EWI (REWI)中的震源位于地下,因此可以沿反射波路径更新背景模型。我们通过每个频率的反卷积过程计算背景模型扰动,就像在原始EWI中所做的那样。我们使用Marmousi模型生成的合成数据证明了所提出方法的有效性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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