Efficient modeling of fractional Laplacian viscoacoustic wave equation with fractional finite-difference method

IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Computers & Geosciences Pub Date : 2024-06-27 DOI:10.1016/j.cageo.2024.105660
Bingluo Gu , Shanshan Zhang , Xingnong Liu , Jianguang Han
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Abstract

The fractional viscoacoustic/viscoelastic wave equation, which accurately quantifies the frequency-independent anelastic effects, has been the focus of seismic industry in recent years. The pseudo-spectral (PS) method stands as one of the most widely used numerical methods for solving the fractional wave equation. However, the PS method often suffers from low accuracy and efficiency, particularly when modeling wave propagation in heterogeneous media. To address these issues, we propose a novel and efficient fractional finite-difference (FD) method for solving the wave equation with fractional Laplacian operators. This method develops an arbitrary high-order FD operator via the generating function of our fractional FD (F-FD) scheme, enhancing accuracy with L2-optimal FD coefficients. Similar to classic FD methods, our F-FD method is characterized by straightforward programming and excellent 3D extensibility. It surpasses the PS method by eliminating the need for Fast Fourier Transform (FFT) and inverse-FFT (IFFT) operations at each time step, offering significant benefits for 3D applications. Consequently, the F-FD method proves more adept for wave-equation-based seismic data processes like imaging and inversion. Compared with existing F-FD methods, our approach uniquely approximates the entire fractional Laplacian operator and stands as a local numerical algorithm, with an adjustable F-FD operator order based on model parameters for enhanced practicality. Accuracy analyses confirm that our method matches the precision of the PS method with a correctly ordered F-FD operator. Numerical examples show that the proposed method has good applicability for complex models. Finally, we have carried out reverse time migration on the Marmousi-2 model, and the imaging profiles indicate that the proposed method can be effectively applied to seismic imaging, demonstrating good practicability.

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用分数有限差分法高效模拟分数拉普拉斯粘声波方程
精确量化与频率无关的无弹性效应的分数粘声/粘弹性波方程是近年来地震行业关注的焦点。伪谱(PS)方法是求解分数波方程最广泛使用的数值方法之一。然而,伪谱法往往存在精度和效率不高的问题,尤其是在异质介质中模拟波的传播时。为了解决这些问题,我们提出了一种新颖高效的分数有限差分(FD)方法,用于求解带有分数拉普拉斯算子的波方程。该方法通过我们的分数有限差分(F-FD)方案的生成函数开发出任意高阶有限差分算子,通过 L2- 最佳有限差分系数提高了精度。与经典的 FD 方法类似,我们的 F-FD 方法具有编程简单、三维扩展性强的特点。它无需在每个时间步进行快速傅立叶变换(FFT)和反傅立叶变换(IFFT)操作,从而超越了 PS 方法,为三维应用提供了显著优势。因此,F-FD 方法更适用于基于波方程的地震数据处理,如成像和反演。与现有的 F-FD 方法相比,我们的方法可以唯一逼近整个分数拉普拉斯算子,是一种局部数值算法,并可根据模型参数调整 F-FD 算子阶数,以提高实用性。精确度分析表明,我们的方法与采用正确阶次 F-FD 算子的 PS 方法的精确度相当。数值示例表明,所提出的方法对复杂模型具有良好的适用性。最后,我们对 Marmousi-2 模型进行了反向时间迁移,其成像剖面表明所提出的方法可以有效地应用于地震成像,证明了其良好的实用性。
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来源期刊
Computers & Geosciences
Computers & Geosciences 地学-地球科学综合
CiteScore
9.30
自引率
6.80%
发文量
164
审稿时长
3.4 months
期刊介绍: Computers & Geosciences publishes high impact, original research at the interface between Computer Sciences and Geosciences. Publications should apply modern computer science paradigms, whether computational or informatics-based, to address problems in the geosciences.
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