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Diffraction of SH-waves by surface or sub-surface topographies with application to soil-structure interaction on shallow foundations.

机译:地面或亚表面地形对SH波的衍射作用及其在浅层基础上的土-结构相互作用。

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摘要

Seismic response of local sites is a significant problem that has been broadly researched for decades. It is an essential step in evaluating maximum intensity of earthquake effects for a specified local site that might happen in the future considering the effects of local topography or various massive artificial structures nearby, so it is crucial to seismic hazard, risk analysis, and earthquake microzonation. Seismic waves can be categorized into body waves and surface waves. Among the three types of body waves: P-, SV-, and SH-waves, the response of SH-waves, is restrained to the out-of-plane unidirection, thus is the most fundamental one and studied in this dissertation.;The objectives of this dissertation are: first, to explore diffraction of incident plane or cylindrical SH-waves by various topographies or underground irregularities; secondly, to investigate the Soil-Structure Interaction (SSI) effects. Two-dimensional plane strain models studied are as diverse as ground surface irregularities (e.g., hills, canyons, canyons), geotechnical engineering (e.g., tunnels, underground cavities, excavations, foundations), and Soil-Structure Interaction models with non-, rigid, or flexible foundations. Although the geometries adopted in those models are relatively much simpler than the ones by numerical methods, the analytical solutions gained by these simple models are indispensable in verifying solutions by various numerical methods (e.g., Finite Element Method; Boundary Element Method). All the models attempted are sitting or encased in an elastic half-space. All the materials appeared are isotropic, homogeneous, and perfectly elastic.;Wave function expansion method is used for solving all the mathematical models in an analytical scheme. The model is computed by mathematically assembling different segments together on their interfaces adjacent to each other. Finally, the problem is reduced to solving a series of infinite linear equations. The governing finite linear equation systems after truncation via this way are always ill-conditioned that require carefully coped with to ensure the accuracy of solutions.;With the analytical solution attained, the response of displacement and stress along the free ground surface are discussed. Displacement and stress residues are calculated to verify the validity of those numerical results. Great effects on dynamic stress concentration and motion nearby due to the existence of those irregularities are observed, evaluated, and analyzed.
机译:本地站点的地震响应是一个重要的问题,数十年来已进行了广泛的研究。考虑到当地地形或附近各种大型人工结构的影响,这是评估将来可能发生的指定本地地点的地震影响的最大强度的重要步骤,因此对于地震危害,风险分析和地震微区划至关重要。地震波可分为体波和面波。在P波,SV波和SH波这三种体波中,SH波的响应受到平面外单向的约束,因此是最基本的一种,是本文研究的基础。本论文的目的是:首先,探讨各种地形或地下不平整对入射平面或圆柱SH波的衍射;其次,研究土壤-结构相互作用(SSI)的影响。研究的二维平面应变模型的种类繁多,包括地表不平整度(例如山丘,峡谷,峡谷),岩土工程(例如隧道,地下洞室,基坑,地基)以及具有非刚性结构的土-结构相互作用模型或灵活的基础。尽管这些模型中采用的几何形状比数值方法要简单得多,但是这些简单模型获得的解析解对于通过各种数值方法(例如,有限元法,边界元法)验证解是必不可少的。所有尝试的模型都坐在或包裹在一个弹性的半空间中。出现的所有材料都是各向同性的,均质的并且具有完美的弹性。波函数展开法用于解析方案中的所有数学模型的求解。该模型是通过在彼此相邻的界面上将不同的片段数学组合在一起来计算的。最后,将问题简化为求解一系列无限线性方程。截断后通过这种方式控制的有限线性方程组始终处于病态状态,需要仔细应对以确保解的准确性。通过获得解析解,讨论了沿自由地面的位移和应力响应。计算位移和残余应力以验证这些数值结果的有效性。观察,评估和分析了这些不规则性对动态应力集中和附近运动的巨大影响。

著录项

  • 作者

    Luo, Hao.;

  • 作者单位

    University of Southern California.;

  • 授予单位 University of Southern California.;
  • 学科 Engineering Civil.
  • 学位 Ph.D.
  • 年度 2008
  • 页码 266 p.
  • 总页数 266
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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