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Simulation of soil-pile-superstructure interaction in the New Madrid Seismic Zone.

机译:新马德里地震带中土-桩-上部结构相互作用的模拟。

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摘要

Deep alluvial soil deposit of the Mississippi Embayment overlies the New Madrid Seismic Zone (NMSZ). The simulation of soil-pile-superstructure interaction (SPSI) at this area has to be divided into two steps. First, the motions at rock base were developed to the interested foundation level and then input for the SPSI analysis.; A new cyclic nonlinear soil model has been developed to take into account the influence of the effective confining pressure on the site response analysis in deep soil deposits. A pore pressure generation model is loosely coupled into the soil model to simulate the possible liquefaction near surface soil layers. The model is implemented into a two-dimensional finite element code in the time domain and calibrated with the recorded motions at typical sites in California. This model was applied into the site response analysis at a Missouri highway bridge site located on the New Madrid rift complex. The results indicate that the influence of the confining pressure is significant for the site response analysis of deep soil sediments and liquefaction could be trigged for M = 6.5 or larger earthquakes in the NMSZ. A coupled SPSI analysis method is then presented to study the seismic response of the highway bridges in the NMSZ. Pile-soil interaction is simulated by the dynamic nonlinear p-y method including the effect of gap and the excess pore water pressure buildup at the pile-soil interface. The presented SPSI approach provided reasonably good agreement with the results the dynamic centrifuge tests. Finally, this method is implemented into the same bridge site for future earthquake scenarios of Mw 7.0. Results indicate that the excess pore water pressure at pile-soil interface significantly influence foundation and superstructure responses.
机译:密西西比河湾的深层冲积土层覆盖了新马德里地震带(NMSZ)。该区域的土-桩-上部结构相互作用(SPSI)模拟必须分为两个步骤。首先,将岩石基础上的运动发展到感兴趣的基础层次,然后输入进行SPSI分析。考虑到有效围压对深层土壤沉积物场地响应分析的影响,开发了一种新的循环非线性土壤模型。孔隙压力产生模型被松散地耦合到土壤模型中,以模拟地表土壤层附近可能的液化。该模型在时域中实现为二维有限元代码,并使用加利福尼亚典型站点上记录的运动进行校准。该模型已应用于位于新马德里裂谷综合体的密苏里州公路桥梁工地的现场响应分析中。结果表明,围压的影响对于深层土壤沉积物的现场响应分析具有重要意义,在NMSZ的M = 6.5或更大地震中,可以触发液化。然后提出了一种耦合SPSI分析方法来研究NMSZ中公路桥梁的地震响应。通过动力非线性p-y方法模拟桩-土相互作用,包括间隙的影响和桩-土界面处多余的孔隙水压力的增加。提出的SPSI方法与动态离心测试的结果提供了相当好的一致性。最后,针对未来的7.0兆瓦地震场景,将该方法实施到同一桥梁站点中。结果表明,桩-土界面处的多余孔隙水压力显着影响地基和上部结构的响应。

著录项

  • 作者

    Zheng, Wei.;

  • 作者单位

    University of Missouri - Rolla.;

  • 授予单位 University of Missouri - Rolla.;
  • 学科 Engineering Civil.
  • 学位 Ph.D.
  • 年度 2004
  • 页码 194 p.
  • 总页数 194
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 建筑科学;
  • 关键词

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