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A cyclic viscoelastic-viscoplastic constitutive model for clay and liquefaction analysis of multi-layered ground

机译:黏土的循环粘弹-粘塑性本构模型及多层地基的液化分析

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摘要

In order to estimate viscous effect of clay in the wide range of low to high level of strain, a cyclic viscoelastic-viscoplastic constitutive model for clay is proposed. First, we confirm the performance of the proposed model by simulating the cyclic undrained triaxial tests to determine the cyclic strength and deformation characteristics of a natural marine clay. Then, the proposed model is incorporated into an effective stress based liquefaction analysis method to estimate the effect of an intermediate clay layer on the behaviour of liquefiable sand layers. The seismic response against foreshocks, main shock as well as aftershocks of 1995 Hyogoken Nambu Earthquake is analysed in the present study. The difference of shear strength characteristics of the alluvial clay layer is one of the reasons why Port Island has a higher liquefaction potential than that of Rokko Island. The proposed model gives a good description of the damping characteristics of clay layer during large earthquakes. Acceleration responses in both clay layer and liquefiable sand layer just above it are damped due to viscous effect of clay. In the case of main shock and the following aftershocks that occurred within less than 9 days after main event, acceleration responses near ground surface are dc-amplified due to the developed excess pore water pressure, while responses near ground surface are amplified before and long after the main event. Using the viscoelastic viscoplastic model for clay layer, time history of acceleration response in upper liquefiable sand layer can be well calculated, in particular in the range of microtremor process after the main seismic motion.
机译:为了评估黏土在低应变至高应变范围内的粘滞效应,提出了黏土的循环粘弹-粘塑性本构模型。首先,我们通过模拟循环不排水三轴试验来确定天然海洋粘土的循环强度和变形特性,从而确定了所提出模型的性能。然后,将所提出的模型结合到基于应力的有效液化分析方法中,以估计中间粘土层对可液化砂层性能的影响。本文分析了1995年兵库县南部南部地震的前震,主震和余震的地震响应。冲积粘土层抗剪强度特性的差异是Port Island的液化潜力高于Rokko Island的原因之一。所提出的模型很好地描述了大地震作用下粘土层的阻尼特性。由于粘土的粘性作用,在粘土层和紧邻其上方的可液化砂层中的加速度响应都会减弱。在发生主震后不到9天发生主震和随后的余震的情况下,由于产生的过高孔隙水压力,地表附近的加速度响应会被直流放大,而地表附近的响应则在震后前后会被放大。主要事件。使用黏土的粘弹性粘塑性模型,可以很好地计算出上层可液化砂层的加速度响应的时程,特别是在主要地震运动后的微震过程范围内。

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