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Impact of freeze-thaw on liquefaction potential and dynamic properties of Mabel Creek silt.

机译:冻融对Mabel Creek淤泥液化潜力和动力特性的影响。

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摘要

In the early winter of 2002 (November), the Alaska Denali earthquake (Mw=-7.9) caused significant damage in partially frozen fine-grained soil and extensive liquefaction was observed in glacial fine-grained saturated soil surface deposits near Tok, Alaska. It illustrated that there was a need to evaluate the seismic response and liquefaction potential of fine-grain soil in cold regions however, until now most of the research on the liquefaction phenomenon and seismic response were mainly about soil in non-cold regions. The seismic response and liquefaction potential of soils in cold regions, especially those of fine-grained nature, has not been studied thoroughly and therefore is not well-understood.Based on this limited laboratory effort, results show that in most cases, temperature rise and freeze-thaw cycles can impact: (a) liquefaction potential, (b) dynamic properties and (c) post-cyclic-loading settlement of fine-grained soils. However, there was one case exception and this is decribed in the following sentence. When a fine-grained soil was conditioned in a partially frozen state, the possibility and threat of liquefaction significantly increased.This document presents a laboratory study on liquefaction potential and cyclic response of fine-grained soil in cold regions. As the main features of the soil in the ground of cold regions, temperature change at below freezing temperatures or near-freezing temperatures, and the seasonal climate change were evaluated on liquefaction potential, dynamic properties, and post-cyclic-loading settlement of fine-grained soils. Increasing temperatures from near freezing to the completely thawed temperature (i.e., 24°C, 5°C, 1°C, and 0.5°C) were used to thaw the frozen Mabel Creek silt to simulate temperature change on it, or the Mabel Creek silt experienced several freezing and thawing alternating processes (i.e., 1, 2, and 4 freeze-thaw cycles) to simulate seasonal climate change. Triaxial strain-controlled cyclic tests were conducted to evaluate liquefaction potential, dynamic properties, and post-cyclic-loading settlement.
机译:在2002年初冬(11月),阿拉斯加Denali地震(Mw = -7.9)在部分冻结的细粒土壤中造成了严重破坏,在阿拉斯加Tok附近的冰川细粒饱和土壤表面沉积物中观察到了广泛的液化。这说明有必要评估寒冷地区细粒土壤的地震响应和液化潜力,但是到目前为止,关于液化现象和地震响应的研究主要集中在非寒冷地区的土壤上。在寒冷地区,特别是细粒土壤中,土壤的地震响应和液化潜能尚未得到透彻研究,因此人们对其了解不多。基于有限的实验室工作,结果表明在大多数情况下,温度升高和冻融循环会影响:(a)液化潜力,(b)动力学特性,以及(c)细粒土的循环加载后沉降。但是,有一个案例例外,下面的句子中对此进行了描述。当将细粒土壤置于部分冻结状态时,液化的可能性和威胁显着增加。本文介绍了在寒冷地区细化土壤液化潜力和循环响应的实验室研究。作为低温地区土壤的主要特征,对低于冰点温度或接近冰点温度的温度变化以及季节性气候变化进行了评估,包括细化层的液化潜力,动力特性和循环荷载后沉降。粒状土壤。从接近冻结的温度升高到完全解冻的温度(即24°C,5°C,1°C和0.5°C)用于解冻冰冻的Mabel Creek淤泥以模拟其温度变化,或者Mabel Creek淤泥经历了几次冰冻和融化交替模拟季节性气候变化的过程(即1、2和4个冻融循环)。进行了三轴应变控制的循环试验,以评估液化潜力,动力特性和循环荷载后沉降。

著录项

  • 作者

    Zhang, Yu.;

  • 作者单位

    University of Alaska Fairbanks.;

  • 授予单位 University of Alaska Fairbanks.;
  • 学科 Engineering Civil.
  • 学位 Ph.D.
  • 年度 2009
  • 页码 191 p.
  • 总页数 191
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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