Accuracy of the staggered-grid finite-difference method of the acoustic wave equation for marine seismic reflection modeling | |
Qian Jin1; Wu Shiguo1; Cui Ruofei2; Qian, J | |
2013 | |
发表期刊 | CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY |
ISSN | 0254-4059 |
卷号 | 31期号:1页码:169-177 |
文章类型 | Article |
摘要 | Seismic wave modeling is a cornerstone of geophysical data acquisition, processing, and interpretation, for which finite-difference methods are often applied. In this paper, we extend the velocity-pressure formulation of the acoustic wave equation to marine seismic modeling using the staggered-grid finite-difference method. The scheme is developed using a fourth-order spatial and a second-order temporal operator. Then, we define a stability coefficient (SC) and calculate its maximum value under the stability condition. Based on the dispersion relationship, we conduct a detailed dispersion analysis for submarine sediments in terms of the phase and group velocity over a range of angles, stability coefficients, and orders. We also compare the numerical solution with the exact solution for a P-wave line source in a homogeneous submarine model. Additionally, the numerical results determined by a Marmousi2 model with a rugged seafloor indicate that this method is sufficient for modeling complex submarine structures.; Seismic wave modeling is a cornerstone of geophysical data acquisition, processing, and interpretation, for which finite-difference methods are often applied. In this paper, we extend the velocity-pressure formulation of the acoustic wave equation to marine seismic modeling using the staggered-grid finite-difference method. The scheme is developed using a fourth-order spatial and a second-order temporal operator. Then, we define a stability coefficient (SC) and calculate its maximum value under the stability condition. Based on the dispersion relationship, we conduct a detailed dispersion analysis for submarine sediments in terms of the phase and group velocity over a range of angles, stability coefficients, and orders. We also compare the numerical solution with the exact solution for a P-wave line source in a homogeneous submarine model. Additionally, the numerical results determined by a Marmousi2 model with a rugged seafloor indicate that this method is sufficient for modeling complex submarine structures. |
关键词 | Marine Seismic Reflection Modeling Stability Condition Dispersion Relation Staggered Grid Finite-difference |
学科领域 | Marine & Freshwater Biology ; Oceanography |
DOI | 10.1007/s00343-013-2074-6 |
URL | 查看原文 |
收录类别 | SCI |
语种 | 英语 |
WOS研究方向 | Marine & Freshwater Biology ; Oceanography |
WOS类目 | Limnology ; Oceanography |
WOS记录号 | WOS:000313654000019 |
WOS关键词 | TRANSVERSELY ISOTROPIC MEDIA ; VELOCITY-STRESS ; HETEROGENEOUS MEDIA ; PROPAGATION ; SEISMOGRAMS |
WOS标题词 | Science & Technology ; Life Sciences & Biomedicine ; Physical Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/16283 |
专题 | 海洋地质与环境重点实验室 |
通讯作者 | Qian, J |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.China Univ Min & Technol, Sch Resource & Geosci, Xuzhou 221116, Peoples R China |
第一作者单位 | 中国科学院海洋研究所 |
推荐引用方式 GB/T 7714 | Qian Jin,Wu Shiguo,Cui Ruofei,et al. Accuracy of the staggered-grid finite-difference method of the acoustic wave equation for marine seismic reflection modeling[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2013,31(1):169-177. |
APA | Qian Jin,Wu Shiguo,Cui Ruofei,&Qian, J.(2013).Accuracy of the staggered-grid finite-difference method of the acoustic wave equation for marine seismic reflection modeling.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,31(1),169-177. |
MLA | Qian Jin,et al."Accuracy of the staggered-grid finite-difference method of the acoustic wave equation for marine seismic reflection modeling".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 31.1(2013):169-177. |
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