基于lt;igt;Llt;/igt;lt;subgt;1lt;/subgt;规范,使用具有优化常数系数的显式方案的空间导数简化隐式有限差分法

IF 3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Geophysics Pub Date : 2023-11-21 DOI:10.1190/geo2023-0246.1
Zhongzheng Miao, Jinhai Zhang
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引用次数: 0

摘要

显式有限差分(FD)方法被广泛应用于地震波传播的数值模拟中,用于近似空间导数。然而,传统的和优化的高阶显式有限差分方法都存在饱和效应,严重制约了数值精度的提高。相比之下,隐式 FD 方法以有理函数的形式近似空间导数,因此能以相对较低的阶数获得更高的数值精度,但由于需要对多对角矩阵进行反演,其计算成本较高。为了降低计算成本,我们推导了一种隐式 FD 方法的显式策略,利用离散傅立叶矩阵构建隐式 FD 方法;然后,将多对角矩阵的反演转化为显式矩阵乘法;接下来,我们构建了基于 L1 准则的目标函数,以降低隐式 FD 方法的近似误差。所提出的隐式 FD 方法的显式策略可以避免对多对角矩阵进行反演,从而提高计算效率。所提出的常数系数优化方法降低了中波范围内的近似误差,但在低波范围内却以可容忍的偏差(小于 0.0001)为代价。对于二维 Marmousi 模型,拟议方法得到的数值结果的均方根误差是同阶(即 5/3)传统隐式 FD 方法的五分之一,是更高阶(即 72)传统显式 FD 方法的三分之一。数值误差的显著减少使所提出的方法在大规模模型的数值模拟,特别是长时间模拟中大有可为。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Simplified implicit finite-difference method of spatial derivative using explicit schemes with optimized constant coefficients based on lt;igt; Llt;/igt;lt;subgt;1lt;/subgt; norm
The explicit finite-difference (FD) method is widely used in numerical simulation of seismic wave propagation to approximate spatial derivatives. However, both the traditional and optimized high-order explicit FD methods suffer from the saturation effect, which seriously restricts the improvement of numerical accuracy. In contrast, the implicit FD method approximates the spatial derivatives in the form of rational functions and thus can obtain much higher numerical accuracy with relatively low orders; however, its computational cost is expensive due to the need to invert a multi-diagonal matrix. We derive an explicit strategy for the implicit FD method to reduce the computational cost, constructing the implicit FD method with the discrete Fourier matrix; then, we transform the inversion of the multi-diagonal matrix into an explicit matrix multiplication; next, we construct an objective function based on the L1 norm to reduce approximation error of the implicit FD method. The proposed explicit strategy of the implicit FD method can avoid inverting the multi-diagonal matrix, thus improving the computational efficiency. The proposed constant coefficient optimization method reduces the approximation error in the medium-wavenumber range at the cost of tolerable deviation (smaller than 0.0001) in the low-wavenumber range. For the 2D Marmousi model, the root-mean-square error of the numerical results obtained by the proposed method is one-fifth that of the traditional implicit FD method with the same order (i.e., 5/3) and one-third that of the traditional explicit FD method with much higher orders (i.e., 72). The significant reduction of numerical error makes the proposed method promising for numerical simulation in large-scale models, especially for long-time simulations.
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来源期刊
Geophysics
Geophysics 地学-地球化学与地球物理
CiteScore
6.90
自引率
18.20%
发文量
354
审稿时长
3 months
期刊介绍: Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics. Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research. Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring. The PDF format of each Geophysics paper is the official version of record.
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