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Effect of fines content on liquefaction potential of sands.

机译:细粉含量对砂土液化潜力的影响。

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摘要

One of the most dramatic causes of damage to infrastructure during earthquakes is liquefaction of saturated sandy soils. While liquefaction has been reported in numerous earthquakes (Seed, 1968), the phenomenon has been more dramatically illustrated in the Niigata, Japan Earthquake of 1964, the Alaska Earthquake the same year and recently in the Loma Prieta Earthquake of 1989. An understanding of this phenomenon is critical for mitigation against severe damages to buildings and various superstructures during earthquakes.; The purpose of this dissertation is to investigate the effect of fines on liquefaction behavior of sand by using stress and strain controlled consolidated undrained cyclic triaxial tests. It is also aimed to provide a framework for understanding the stress-strain behavior silty sands and offer guidelines for future research. The second purpose of the dissertation is to compare the laboratory test data with a theory based on the density of dissipated energy during cyclic loading. The theory originally is used for pure sand. Here, it is modified to give closer approximations for the experimental findings on silty sand. The model was successfully predicted the test results.; The resistance of soils with addition of 10% low plasticity and non-plastic fines compared to clean sand has small significance on the pore pressure generation of sand. Though adding 10% low plasticity fines slightly increases the resistance to liquefaction while addition of 10% non-plastic fines decrease the liquefaction potential. As non-plastic fines content increases up to a level of 30%, the liquefaction resistance decreases. There is a level of cyclic shear strain below which, there is little pore water pressure generation in saturated silty soils. This threshold strain level is similar to those observed in sands and is in the order of 0.01 percent.; It is anticipated that the outcome of this research will help engineers better understand the behavior of silty soils under seismic conditions and enable them to come up with a much comprehensive guideline or design against liquefaction of silty soils.
机译:地震期间破坏基础设施的最剧烈原因之一是饱和砂土的液化。尽管在许多地震中都报告了液化现象(Seed,1968年),但在1964年的日本新泻地震,同年的阿拉斯加地震以及最近的1989年的洛马普利塔地震中,这种现象得到了更为明显的体现。这种现象对于减轻地震期间建筑物和各种上部结构的严重损坏至关重要。本文的目的是通过应力和应变控制固结不排水循环三轴试验研究细粉对砂土液化行为的影响。它还旨在为理解应力-应变行为粉质砂提供框架,并为将来的研究提供指导。论文的第二个目的是将实验室测试数据与基于循环加载过程中耗散能量密度的理论进行比较。该理论最初用于纯砂。在这里,它被修改为粉砂的实验结果提供更接近的近似值。该模型已成功预测了测试结果。与干净的沙子相比,添加了10%的低塑性和非塑料细粉的土壤的抵抗力对沙子的孔隙压力产生意义不大。尽管添加10%的低塑性细粉会稍微提高抗液化性,而添加10%的非塑性细粉会降低液化潜力。当非塑料细粉含量增加到30%时,抗液化性降低。在一定程度的循环剪切应变之下,饱和粉质土壤几乎没有孔隙水压力产生。该阈值应变水平类似于在沙子中观察到的应变水平,约为0.01%。可以预期,这项研究的结果将有助于工程师更好地了解在地震条件下粉质土壤的行为,并使他们能够提出一个针对粉质土壤液化的非常全面的指南或设计。

著录项

  • 作者

    Erten, Duygu.;

  • 作者单位

    Rutgers The State University of New Jersey - New Brunswick.;

  • 授予单位 Rutgers The State University of New Jersey - New Brunswick.;
  • 学科 Engineering Civil.; Geophysics.
  • 学位 Ph.D.
  • 年度 1994
  • 页码 203 p.
  • 总页数 203
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 建筑科学;地球物理学;
  • 关键词

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