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首页> 外文期刊>Bulletin of the Seismological Society of America >Effects of Moisture Content on the Dynamic Response and Failure Mode of Unsaturated Soil Slope Subjected to Seismic Load
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Effects of Moisture Content on the Dynamic Response and Failure Mode of Unsaturated Soil Slope Subjected to Seismic Load

机译:水分含量对抗震载荷的不饱和土坡动力响应和失效模式的影响

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摘要

Understanding the relationship between the moisture content of unsaturated soil and the instability and dynamic response of slope under the action of seismic load can bring convenience to the field of slope safety assessment. The effect of moisture content of the unsaturated soil on the failure mode and dynamic response of slope under seismic loading was investigated using shaking table tests. In this regard, three different moisture contents of 5%, 8.1%, and 12.5% were considered. The experimental results show that the amplification factor of acceleration (AFA) on the slope surface increases with the increase in both relative elevation and excitation amplitude of acceleration (EAA). As the moisture content of unsaturated soil increases, AFA tends to decrease. An empirical correlation describing the relationship among AFA, relative elevation, dimensionless EAA, and moisture content of unsaturated soil was proposed. The excitation frequency of acceleration (EFA) has a significant impact on the AFA at the middle and upper parts of the slope. The deformation of slope surface is able to reflect the failure mode of slope, which can be used in slope monitoring work. The slope with different moisture contents of unsaturated soil has different instability modes. With the increase in soil moisture content, the slope needs more energy to reach the unstable state under seismic loading. There are three typical regions of principal stress field in the slope exposed to seismic loading, which control the evolution of initial slip plane inside the slope.
机译:了解不饱和土壤的水分含量与坡度的不稳定性和动力响应之间的关系,可以为坡度安全评估领域带来便利。采用振动台试验研究了不饱和土壤水分含量对地震载荷下坡度的破坏模式和动力响应的影响。在这方面,考虑了三种不同的水分含量为5%,8.1%和12.5%。实验结果表明,随着加速度(EAA)的相对高度和激发幅度的增加,倾斜表面上的加速度(AFA)的放大因子增加。随着不饱和土壤的水分含量增加,AFA趋于降低。提出了描述了AFA,相对升高,无量纲EAA和不饱和土壤的关系的经验相关性。加速度(EFA)的激发频率对斜坡的中间部分和上部的AFA产生显着影响。倾斜表面的变形能够反射斜率的故障模式,其可用于坡度监测工作。具有不同水分含量的不饱和土壤的斜率具有不同的不稳定模式。随着土壤水分含量的增加,斜坡需要更多的能量以在地震载荷下达到不稳定状态。斜坡上有三个主应力场的典型区域,暴露在地震载荷中,控制斜率内的初始滑动平面的演变。

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    Southwest Jiaotong Univ Sch Civil Engn 111 First Sect North Second Ring Rd Chengdu 610031 Sichuan Peoples R China;

    Southwest Jiaotong Univ Sch Civil Engn 111 First Sect North Second Ring Rd Chengdu 610031 Sichuan Peoples R China;

    Griffith Univ Sch Engn &

    Built Environm Gold Coast Campus Southport Qld 4222 Australia;

    Southwest Jiaotong Univ Sch Civil Engn 111 First Sect North Second Ring Rd Chengdu 610031 Sichuan Peoples R China;

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  • 正文语种 eng
  • 中图分类 地震学 ;
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