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Response of Liquefiable Sites in the Central Business District of Christchurch, New Zealand.

机译:新西兰基督城中央商务区的液化场所响应。

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The strong shaking of the 2010--2011 Canterbury earthquake sequence caused widespread liquefaction in much of the city of Christchurch, NZ, including large parts of the central business district (CBD). Understanding the effects of liquefaction on soil and building response is an area of earthquake engineering that continues to challenge practitioners and researchers. This challenging topic makes the study of case histories, such as those provided by the Canterbury earthquakes, an essential component to characterizing and understanding the effects of soil liquefaction on building performance. This thesis focuses on providing insights regarding the seismic response of liquefiable soils through the use of information and data collected in Christchurch, NZ following the Canterbury earthquake sequence.;Nonlinear effective stress site response analyses are often used by engineers to model the dynamic response of potentially liquefiable soils during strong shaking. For the presented research, a widely used one-dimensional nonlinear effective stress site response analysis program is used to perform this modeling. Ground motions recorded during six events of the 2010--11 Canterbury earthquake sequence are used in conjunction with the extensive site investigation data that has been obtained in Christchurch to complete site response analyses at several strong motion station sites in the greater Christchurch area. Deconvolved Riccarton Gravel input motions were generated, because representative, recorded rock or firm layer base-motions were not available in the Christchurch area. Nonlinear effective stress seismic site response analyses are shown to capture key aspects of the observed soil response through the comparison of acceleration response spectra of calculated surface motions to those of recorded surface motions; however, equivalent-linear and total stress nonlinear analyses are shown to capture these aspects as well. Biases in the computed motions compared to recorded motions were realized for some cases, but they can be attributed primarily to the uncertainty in the development of the input motions used in the analyses.;The study of the consequences of liquefaction on building performance is a complex soil-structure interaction problem that requires the use of well-documented case histories for validation purposes. An extensive site investigation and advanced laboratory testing program was carried out in Christchurch, NZ from April to October of 2014. The aim of this work was to provide characterization of the liquefaction resistance of foundation soils from building sites affected by liquefaction during the Canterbury earthquakes. In-situ penetration tests, such as CPT, are valuable methods for gaining an initial understanding of a site's characteristics and the expected performance of critical soil layers. However, to understand fully the complex response of soil at the element level, laboratory testing of relatively undisturbed soil specimens provide unique insights. To accomplish these goals, "undisturbed" sampling and triaxial testing (monotonic and cyclic) were performed on soils from key building sites in Christchurch's CBD. High quality sampling and testing could be achieved for most of the predominantly silty and sandy soils in the CBD. Test results indicate, though, that loose clean sand specimens were densified significantly during the sampling with the Dames & Moore hydraulic fixed-piston sampler (an Osterberg-type thin-walled sampler). The cyclic resistances measured in the tests on "undisturbed" specimens were generally consistent with those estimated using empirical simplified liquefaction triggering procedures.;Important insights regarding the cyclic response of the shallow CBD soils were obtained through the laboratory testing carried out as a part of the research presented in this thesis. Triaxial testing of "undisturbed" soil specimens proved important in understanding not only the stress-strain response of the studied soils, but also allowed for further knowledge regarding the pore water pressure response of the tested soils during both cyclic and monotonic loading. Importantly, insights into how various soil types of the CBD responded to cyclic loading were gained through comparisons of cyclic triaxial (CTX) tests performed on a variety of sand and silty sand soils. It was seen through CTX results comparisons that silty sands (soils classified as SM) and clean sands (SP and SP-SM) responded similarly in cyclic loading, even when the fines content of the tested specimens differed. Monotonic triaxial testing was also performed on reconstituted specimens to characterize the steady state response of several soil units in the CBD. The extensive insight garnered from laboratory testing is critical for informing researchers and engineers studying the case histories provided by the Canterbury earthquakes of buildings founded on liquefiable soils, especially those using numerical-based soil-structure interaction analyses. The results of the monotonic and cyclic tests performed as part of this study provide useful data for calibrating advanced numerical models.;Appendices are included as a part of this dissertation to provide supporting information and data not included in the main body of the thesis. (Abstract shortened by UMI.).
机译:2010--2011年坎特伯雷地震序列的强烈震动在新西兰基督城的许多地方(包括中央商务区(CBD)的大部分地区)引起了广泛的液化。了解液化对土壤和建筑物响应的影响是地震工程领域,继续挑战着从业者和研究人员。这个具有挑战性的主题使案例历史研究(例如坎特伯雷地震提供的历史)成为表征和理解土壤液化对建筑性能影响的重要组成部分。本文的重点是通过使用在坎特伯雷地震序列后在新西兰基督城收集的信息和数据来提供有关可液化土壤地震响应的见解;工程师经常使用非线性有效应力场响应分析来模拟潜在的动力响应。剧烈摇动时会液化的土壤。对于本研究,使用了广泛使用的一维非线性有效应力部位响应分析程序来执行此建模。在2010--11年坎特伯雷地震序列的6次事件中记录的地面运动与在基督城获得的大量现场调查数据结合使用,以完成较大的基督城地区几个强运动站点的现场响应分析。去卷积的Riccarton Gravel输入运动是因为克赖斯特彻奇地区没有代表性的,记录下来的岩石或坚硬的层基础运动。非线性有效应力地震现场响应分析表明,通过比较计算出的表面运动的加速度响应谱与记录的表面运动的加速度响应谱,可以捕获观测到的土壤响应的关键方面。然而,等效线性和总应力非线性分析也显示了这些方面。在某些情况下,可以实现计算运动与记录运动相比的偏差,但这些偏差主要归因于分析中所用输入运动发展的不确定性。研究液化对建筑性能的影响是一个复杂的过程土壤-结构相互作用问题,需要使用记录良好的案例历史进行验证。 2014年4月至10月,在新西兰基督城进行了广泛的现场调查和先进的实验室测试程序。这项工作的目的是表征坎特伯雷地震中受液化影响的建筑工地的基础土壤的抗液化性。现场渗透测试(例如CPT)是有价值的方法,可以使您初步了解场地的特征以及关键土壤层的预期性能。但是,为了充分了解土壤在元素水平上的复杂响应,相对未受干扰的土壤样本的实验室测试提供了独特的见解。为了实现这些目标,对克赖斯特彻奇中央商务区主要建筑工地的土壤进行了“不受扰动”采样和三轴测试(单调和循环)。对于CBD中大多数主要为粉质和沙质的土壤,可以实现高质量的采样和测试。但是,测试结果表明,在使用Dames&Moore液压固定活塞采样器(Osterberg型薄壁采样器)采样期间,疏松干净的沙子样本得到了显着的致密化。测试中对“未受扰动”的样品测得的循环阻力通常与使用经验简化的液化触发程序估算的循环阻力一致。浅层CBD土循环响应的重要见解是通过实验室测试获得的,这是CBD的一部分。本文提出的研究。事实证明,“无扰动”土壤样品的三轴测试不仅对理解所研究土壤的应力应变响应非常重要,而且对于循环和单调加载过程中被测土壤的孔隙水压力响应也有进一步的了解。重要的是,通过比较在各种砂质和粉质砂土上进行的循环三轴(CTX)试验,获得了关于CBD的各种土壤如何对循环载荷作出响应的见解。通过CTX结果比较可以看出,即使测试样品的细度有所不同,粉砂(分类为SM的土壤)和干净的砂(SP和SP-SM)在循环载荷中的响应也相似。还对重构标本进行了单调三轴测试,以表征CBD中几个土壤单元的稳态响应。从实验室测试中获得的广泛见解对于通知研究人员和工程师研究在可液化土壤上建房的坎特伯雷地震提供的案例历史至关重要,尤其是那些使用基于数值的土壤-结构相互作用分析的方法。作为研究的一部分,单调和循环测试的结果为校准先进的数值模型提供了有用的数据。附录是本文的一部分,以提供本文中未包含的支持信息和数据。 (摘要由UMI缩短。)。

著录项

  • 作者单位

    University of California, Berkeley.;

  • 授予单位 University of California, Berkeley.;
  • 学科 Civil engineering.
  • 学位 Ph.D.
  • 年度 2015
  • 页码 577 p.
  • 总页数 577
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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