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Characteristics of Excess Pore Water Pressure of Nanjing Saturated Fine Sand Under the Interaction of Wave and Earthquake Loading

机译:波浪与地震相互作用作用下南京饱和细砂超孔隙水压力特征

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摘要

A stress path with continuous rotation of the principal stress direction and continuous alteration of amplitude of deviatoric stress difference under the interaction of wave and earthquake loading was proposed based on the characteristics of the stress path under wave and earthquake loading, respectively. Using a GDS dynamic hollow cylinder apparatus, a series of cyclic triaxial-torsional coupling shear tests were performed on Nanjing saturated fine sand via the stress path mentioned previously under different relative densities, effective initial confining pressures, plastic fines contents, and loading frequencies to study the development of excess pore water pressure (EPWP) of saturated sand under the interaction of wave and earthquake loading. It was found that the development of EPWP follows the trend of fast-steady-mutative-drastic, which is different from that under the cyclic triaxial test or wave loading. The number of cycles causing initial liquefaction (N_L) of saturated sand increases remarkably with relative densities. However, the relationships between N_L and effective initial confining pressures, plastic fines content, or loading frequencies are more complex.
机译:分别根据波浪和地震荷载作用下应力路径的特性,提出了在波浪和地震荷载作用下主应力方向连续旋转且偏应力差幅值连续变化的应力路径。使用GDS动态空心圆柱体装置,通过前面提到的应力路径,在不同的相对密度,有效初始围压,塑性粉含量和加载频率下,对南京饱和细砂进行了一系列循环三轴-扭转耦合剪切试验。波与地震荷载作用下饱和砂岩的超孔隙水压力(EPWP)的发展研究发现,EPWP的发展遵循快速-稳定-突变-急剧的趋势,这与循环三轴试验或波浪载荷下的趋势不同。引起饱和砂土初始液化(N_L)的循环次数随相对密度显着增加。但是,N_L与有效初始围压,塑料细粉含量或加载频率之间的关系更为复杂。

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