Three-dimensional frequency-domain full waveform inversion based on the nearly-analytic discrete method

IF 2.9 3区 地球科学 Earth and Planetary Physics Pub Date : 2021-04-13 DOI:10.26464/epp2021022
Zhang DeYao, Pan WenYong, Yang DingHui, Qiu LingYun, Dong XingPeng, Meng WeiJuan
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Abstract

The nearly analytic discrete (NAD) method is a kind of finite difference method with advantages of high accuracy and stability. Previous studies have investigated the NAD method for simulating wave propagation in the time-domain. This study applies the NAD method to solving three-dimensional (3D) acoustic wave equations in the frequency-domain. This forward modeling approach is then used as the “engine” for implementing 3D frequency-domain full waveform inversion (FWI). In the numerical modeling experiments, synthetic examples are first given to show the superiority of the NAD method in forward modeling compared with traditional finite difference methods. Synthetic 3D frequency-domain FWI experiments are then carried out to examine the effectiveness of the proposed methods. The inversion results show that the NAD method is more suitable than traditional methods, in terms of computational cost and stability, for 3D frequency-domain FWI, and represents an effective approach for inversion of subsurface model structures.

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基于近解析离散法的三维频域全波形反演
近解析离散法(NAD)是一种精度高、稳定性好的有限差分法。以往的研究已经对NAD方法在时域上模拟波的传播进行了研究。本研究应用NAD方法在频域求解三维声波方程。然后将这种正演建模方法用作实现3D频域全波形反演(FWI)的“引擎”。在数值模拟实验中,首先给出了综合算例,证明了NAD方法在正演模拟中相对于传统有限差分方法的优越性。然后进行了三维合成频域FWI实验,以检验所提出方法的有效性。反演结果表明,在计算成本和稳定性方面,NAD方法比传统方法更适合三维频域FWI,是一种有效的地下模型结构反演方法。
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来源期刊
Earth and Planetary Physics
Earth and Planetary Physics GEOSCIENCES, MULTIDISCIPLINARY-
自引率
17.20%
发文量
174
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