中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Finite-difference method for modeling the surface wave propagation with surface topography in anisotropic-viscoelastic media

文献类型:期刊论文

作者Zhou, Xuhui1,3,4; Huo, Shoudong1,3,4; Liang, Yao2; Dong, Shuli1,3,4
刊名JOURNAL OF APPLIED GEOPHYSICS
出版日期2023-10-01
卷号217页码:17
ISSN号0926-9851
关键词Anisotropic Viscoelastic Surface waves FD modeling Free -surface boundary condition
DOI10.1016/j.jappgeo.2023.105161
英文摘要The growth of urbanization makes it increasingly important to accurately investigate underground spaces. Surface-wave-based inversion methods are becoming popular due to their cost-effectiveness and efficiency in reconstructing underground space. However, these methods may produce inaccurate results in the presence of media anisotropy or/and viscoelasticity. To investigate the influence of media anisotropy or viscoelasticity on surface waves, it is crucial to develop an efficient and accurate forward modeling method in anisotropicviscoelastic (AV) media. The finite-difference (FD) method is a widely used forward modeling method in surface-wave-based inversion methods. However, implementing the free-surface boundary condition and representing non-flat topography can be challenging. Considering the challenges described above, this study proposes a simple and efficient FD method for modeling surface-wave propagation. The proposed method employs a parameter-modified strategy to implement the stress-free condition by modifying the model parameters near the (non-) flat free-surface boundary. A staircase discretization strategy is then used to represent the non-flat free surface. To suppress the staircase diffractions caused by the staircase discretization strategy, an independent wavefield superposition is adopted with modeling results of different parameter configurations. Compared with conventional FD methods, the proposed method can reduce computational costs while accurately simulating surface waves. Numerical experiments have demonstrated the accuracy and feasibility of the proposed method. The proposed method provides a theoretical basis for surface-wave-based inversion methods and contributes to the development of accurate underground space investigation.
WOS关键词SPECTRAL ELEMENT METHOD ; FORM INVERSION ; RAYLEIGH-WAVES ; SEISMIC DATA ; 2D ; DISPERSION ; SIMULATION ; ATTENUATION ; BOUNDARY ; VELOCITY
资助项目National Key Research and Develop- ment Program of China[2021YFA0716901] ; National Key Research and Develop- ment Program of China[2022YFB3904601] ; National Natural Science Foundation of China[42174160] ; National Natural Science Foundation of China[41904114]
WOS研究方向Geology ; Mining & Mineral Processing
语种英语
出版者ELSEVIER
WOS记录号WOS:001071758500001
资助机构National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Key Research and Develop- ment Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/110860]  
专题地质与地球物理研究所_中国科学院油气资源研究重点实验室
通讯作者Dong, Shuli
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Chinese Acad Geol Sci, Key Lab Deep Earth Dynam, Minist Nat Resources, Inst Geol, Beijing 100037, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China
4.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Zhou, Xuhui,Huo, Shoudong,Liang, Yao,et al. Finite-difference method for modeling the surface wave propagation with surface topography in anisotropic-viscoelastic media[J]. JOURNAL OF APPLIED GEOPHYSICS,2023,217:17.
APA Zhou, Xuhui,Huo, Shoudong,Liang, Yao,&Dong, Shuli.(2023).Finite-difference method for modeling the surface wave propagation with surface topography in anisotropic-viscoelastic media.JOURNAL OF APPLIED GEOPHYSICS,217,17.
MLA Zhou, Xuhui,et al."Finite-difference method for modeling the surface wave propagation with surface topography in anisotropic-viscoelastic media".JOURNAL OF APPLIED GEOPHYSICS 217(2023):17.

入库方式: OAI收割

来源:地质与地球物理研究所

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