Novel Optimal Staggered Grid Finite Difference Scheme Based on Gram–Schmidt Procedure for Acoustic Wave Modelling

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS pure and applied geophysics Pub Date : 2025-01-13 DOI:10.1007/s00024-024-03652-4
Min Zhang, Liming Zhou, Daiguang Fu, Shiqi Dong, Haibo Wu
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Abstract

The staggered grid finite difference method is used extensively in numerical simulations of acoustic equations; however, its application is accompanied by numerical dispersion. The most representative traditional method for suppressing the numerical dispersion is the Taylor expansion method, which primarily converts the acoustic equation into a polynomial equation of the trigonometric function and subsequently expands the trigonometric function into a power function polynomial through the Taylor expansion to finally obtain the difference coefficient. However, this traditional method is only applicable to the small wavenumber range. In this study, the Gram–Schmidt orthogonalization method, combined with the binomial theorem and Euler formula was used to reverse the polynomial of power function into a polynomial of trigonometric function and to obtain a new difference coefficient. To highlight the effectiveness of the proposed method, it was compared with the Taylor expansion method (TEM) and the least-squares method (LSM) by selecting a small wavenumber, middle wavenumber, and wide wavenumber ranges. Accuracy and dispersion analyses were conducted. The results showed that the new difference coefficient generated smaller errors and induced stronger suppression of the numerical dispersion. A comparative analysis of the uniform and complex models further validated the superiority of the proposed staggered grid difference coefficient.

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基于Gram-Schmidt过程的最优交错网格有限差分格式
交错网格有限差分法广泛应用于声学方程的数值模拟;然而,它的应用伴随着数值色散。压制数值色散最具代表性的传统方法是泰勒展开法,该方法首先将声学方程转化为三角函数的多项式方程,然后通过泰勒展开将三角函数展开为幂函数多项式,最后得到差分系数。然而,这种传统方法只适用于小波数范围。本研究采用Gram-Schmidt正交化方法,结合二项式定理和欧拉公式,将幂函数的多项式反化为三角函数的多项式,得到新的差分系数。为了突出该方法的有效性,通过选择小波数、中波数和宽波数范围,将该方法与泰勒展开法(TEM)和最小二乘法(LSM)进行了比较。进行了准确性和分散度分析。结果表明,新差分系数产生的误差较小,对数值色散的抑制作用较强。通过对均匀模型和复杂模型的对比分析,进一步验证了交错网格差系数的优越性。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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