{"title":"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","authors":"Zhongzheng Miao, Jinhai Zhang","doi":"10.1190/geo2023-0246.1","DOIUrl":null,"url":null,"abstract":"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.","PeriodicalId":55102,"journal":{"name":"Geophysics","volume":"4 1","pages":""},"PeriodicalIF":3.0000,"publicationDate":"2023-11-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"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\",\"authors\":\"Zhongzheng Miao, Jinhai Zhang\",\"doi\":\"10.1190/geo2023-0246.1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"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.\",\"PeriodicalId\":55102,\"journal\":{\"name\":\"Geophysics\",\"volume\":\"4 1\",\"pages\":\"\"},\"PeriodicalIF\":3.0000,\"publicationDate\":\"2023-11-21\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geophysics\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1190/geo2023-0246.1\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geophysics","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1190/geo2023-0246.1","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
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.
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.