亲爱的研友该休息了!由于当前在线用户较少,发布求助请尽量完整地填写文献信息,科研通机器人24小时在线,伴您度过漫漫科研夜!身体可是革命的本钱,早点休息,好梦!

On the absorbing boundaries to replicate semi-infinite half-space in numerical seismic analyses using the finite element method

有限元法 边界(拓扑) 反射(计算机编程) 空格(标点符号) 领域(数学分析) 半空间 边值问题 数学分析 计算机科学 几何学 地质学 数学 结构工程 工程类 操作系统 程序设计语言
作者
Tyler R. Hebert,James Bryce,Arka P. Chattopadhyay
标识
DOI:10.1190/image2022-3751979.1
摘要

PreviousNext No AccessSecond International Meeting for Applied Geoscience & EnergyOn the absorbing boundaries to replicate semi-infinite half-space in numerical seismic analyses using the finite element methodAuthors: Tyler R. HebertJames M. BryceArka Prabha ChattopadhyayTyler R. HebertMarshall UniversitySearch for more papers by this author, James M. BryceMarshall UniversitySearch for more papers by this author, and Arka Prabha ChattopadhyayMarshall UniversitySearch for more papers by this authorhttps://doi.org/10.1190/image2022-3751979.1 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InRedditEmail AbstractComputational analysis allows for easy replication of seismic tomography using numerical solving techniques. The Finite Element Method (FEM) and the Finite Difference Method (FDM) are the two primary methods which are used for such computational models that have been presented in the literature. One challenge of such analyses is the creation of a semi-infinite half space. In a monolithic, elastic domain, seismic waves propagate without any interruptions in the absence of domain boundaries. However, in a computational study, the geometry is of a finite volume and it is not possible to create a semi-infinite half-space without additional adjustments. To address this, certain boundary conditions which simulate the finite domain to behave like a semi-infinite half space are used. These conditions are enforced on the essential boundaries, which otherwise reflect the transient wave propagation. We call these conditions as absorbing layers, which trap the outbound waves at these boundaries, thus preventing reflection of the waves back into the domain of analysis. In this study, the efficacy of using different absorbing layers is investigated in the framework of the FEM formulation of the transient wave propagation in monolithic and multi-material linear elastic domains. We test three different methods of implementing absorbing layers into a computational model: Perfectly Matched Layers (PML), Caughey Absorbing Layer Method or Caughey Damping (CD), and Infinite Elements (IE). The assessment of CD and IE were performed in the commercial FEM software ABAQUS and were compared with benchmark computational results of PML from the literature. The quality of absorption was quantified based on the residual strain energy and displacements present in the domain of interest post interaction of the propagating waves with the absorbing layer. It was determined that the Infinite Elements provides an absorbing layer of reasonable accuracy at relative ease of implementation in seismic tomography simulations.Keywords: numerical seismic, finite element method, absorbing boundariesPermalink: https://doi.org/10.1190/image2022-3751979.1FiguresReferencesRelatedDetails Second International Meeting for Applied Geoscience & EnergyISSN (print):1052-3812 ISSN (online):1949-4645Copyright: 2022 Pages: 3694 publication data© 2022 Published in electronic format with permission by the Society of Exploration Geophysicists and the American Association of Petroleum GeologistsPublisher:Society of Exploration Geophysicists HistoryPublished Online: 15 Aug 2022 CITATION INFORMATION Tyler R. Hebert, James M. Bryce, and Arka Prabha Chattopadhyay, (2022), "On the absorbing boundaries to replicate semi-infinite half-space in numerical seismic analyses using the finite element method," SEG Technical Program Expanded Abstracts : 2576-2580. https://doi.org/10.1190/image2022-3751979.1 Plain-Language Summary Keywordsnumerical seismicfinite element methodabsorbing boundariesPDF DownloadLoading ...

科研通智能强力驱动
Strongly Powered by AbleSci AI
更新
PDF的下载单位、IP信息已删除 (2025-6-4)

科研通是完全免费的文献互助平台,具备全网最快的应助速度,最高的求助完成率。 对每一个文献求助,科研通都将尽心尽力,给求助人一个满意的交代。
实时播报
8秒前
英姑应助科研通管家采纳,获得10
8秒前
sdjtxdy发布了新的文献求助10
13秒前
17秒前
sdjtxdy完成签到,获得积分10
21秒前
dao发布了新的文献求助10
40秒前
44秒前
50秒前
1分钟前
千里草完成签到,获得积分10
1分钟前
2分钟前
量子星尘发布了新的文献求助10
2分钟前
小奋青完成签到 ,获得积分10
2分钟前
忧伤的绍辉完成签到 ,获得积分10
3分钟前
kuoping完成签到,获得积分0
3分钟前
3分钟前
GPTea应助科研通管家采纳,获得10
4分钟前
馆长应助科研通管家采纳,获得10
4分钟前
Lucas应助科研通管家采纳,获得20
4分钟前
GPTea应助科研通管家采纳,获得10
4分钟前
cc完成签到,获得积分10
4分钟前
科研通AI5应助dao采纳,获得10
5分钟前
5分钟前
dao发布了新的文献求助10
5分钟前
zhaimen完成签到 ,获得积分10
5分钟前
馆长应助科研通管家采纳,获得50
6分钟前
GPTea应助科研通管家采纳,获得20
6分钟前
希望天下0贩的0应助lll采纳,获得10
6分钟前
sky11完成签到 ,获得积分10
7分钟前
7分钟前
lll发布了新的文献求助10
7分钟前
lll完成签到,获得积分10
7分钟前
GPTea应助科研通管家采纳,获得10
8分钟前
SciGPT应助科研通管家采纳,获得10
8分钟前
英俊的铭应助科研通管家采纳,获得50
8分钟前
韶绍完成签到 ,获得积分10
9分钟前
量子星尘发布了新的文献求助10
9分钟前
GPTea应助科研通管家采纳,获得10
10分钟前
GPTea应助科研通管家采纳,获得10
10分钟前
月军完成签到,获得积分10
10分钟前
高分求助中
(应助此贴封号)【重要!!请各用户(尤其是新用户)详细阅读】【科研通的精品贴汇总】 10000
Zeolites: From Fundamentals to Emerging Applications 1500
Architectural Corrosion and Critical Infrastructure 1000
Early Devonian echinoderms from Victoria (Rhombifera, Blastoidea and Ophiocistioidea) 1000
Hidden Generalizations Phonological Opacity in Optimality Theory 1000
2026国自然单细胞多组学大红书申报宝典 800
Real Analysis Theory of Measure and Integration 3rd Edition 500
热门求助领域 (近24小时)
化学 医学 生物 材料科学 工程类 有机化学 内科学 生物化学 物理 计算机科学 纳米技术 遗传学 基因 复合材料 化学工程 物理化学 病理 催化作用 免疫学 量子力学
热门帖子
关注 科研通微信公众号,转发送积分 4910211
求助须知:如何正确求助?哪些是违规求助? 4186186
关于积分的说明 12999166
捐赠科研通 3953517
什么是DOI,文献DOI怎么找? 2167972
邀请新用户注册赠送积分活动 1186428
关于科研通互助平台的介绍 1093500