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Effects of Long-Duration Ground Motions on Liquefaction Hazards

机译:长时间地面运动对液化危害的影响

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摘要

Soil liquefaction during past earthquakes has caused extensive damage to buildings, bridges, dam, pipelines and other elements of infrastructure. Geotechnical engineers use empirical observations from earthquake case histories in conjunction with soil mechanics to predict the behavior of liquefiable soils. However, current empirical databases are insufficient to evaluate the behavior of soils subject to long-duration earthquakes, such as a possible Mw = 9.0 Cascadia Subduction Zone earthquake.;The objective of this research is to develop insight into the triggering and effects of liquefaction due to long-duration ground motions and to provide recommendations for analysis and design. Recorded ground motions from 21 case histories with surficial evidence of liquefaction showed marked differences in soil behavior before and after liquefaction was triggered. In some cases, strong shaking continued for several minutes after the soil liquefied, and a variety of behaviors were observed including dilation pulses, continued softening due to soil fabric degradation, and soil stiffening due to pore pressure dissipation and drainage. Supplemental field and laboratory investigations were performed at three sites that liquefied during the 2011 Mw = 9.0 Tohoku earthquake. The recorded ground motions and field investigation data were used in conjunction with laboratory observations, analytical models, and numerical models to evaluate the behavior of liquefiable soils subjected to long-duration ground motions.;Observations from the case histories inspired a framework to predict ground deformations based on the differences in soil behavior before and after liquefaction has triggered. This framework decouples the intensity of shaking necessary to trigger liquefaction from the intensity of shaking that drives deformation by identifying the time when liquefaction triggers. The timing-based framework promises to dramatically reduce the uncertainty in deformation estimates compared to conventional, empirically-based procedures.
机译:过去地震中的土壤液化对建筑物,桥梁,水坝,管道和其他基础设施要素造成了广泛破坏。岩土工程师将地震案例历史中的经验观察与土壤力学一起使用,以预测可液化土壤的行为。然而,当前的经验数据库不足以评估长期地震(例如Mw = 9.0卡斯卡迪亚俯冲带地震)的土壤行为。这项研究的目的是深入了解液化的触发作用和影响。进行长时间的地面运动,并为分析和设计提供建议。记录的来自21个案例历史的地面运动以及表面液化的证据表明,液化触发前后土壤行为存在明显差异。在某些情况下,土壤液化后持续强烈震荡几分钟,观察到多种行为,包括膨胀脉冲,由于土壤织物降解而导致的持续软化以及由于孔隙压力的耗散和排水而导致的土壤变硬。在2011年Mw = 9.0东北地震中被液化的三个地点进行了补充的现场和实验室调查。记录的地面运动和现场调查数据与实验室观察结果,分析模型和数值模型结合使用,以评估承受长期地面运动的可液化土壤的行为。;案例历史的观察启发了一个框架来预测地面变形基于液化触发前后土壤行为的差异。该框架通过识别液化触发的时间,将触发液化所需的摇动强度与驱动变形的摇动强度分离开。与基于经验的常规程序相比,基于时序的框架有望显着减少变形估计的不确定性。

著录项

  • 作者

    Greenfield, Michael W.;

  • 作者单位

    University of Washington.;

  • 授予单位 University of Washington.;
  • 学科 Civil engineering.;Geophysical engineering.;Engineering.
  • 学位 Ph.D.
  • 年度 2017
  • 页码 477 p.
  • 总页数 477
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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