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Shaking Table Test and Numerical Verification for Free Ground Seismic Response of Saturated Soft Soil

机译:饱和软土自由地面地震响应的振动台试验和数值验证

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This paper investigates shaking table test (1g) and numerical simulation (fully coupled) of vertically propagating shear waves for saturated soft free field. A large-scale shaking table model test was performed to study seismic response characteristics of saturated soft soil free field. According to test results of seismic response features of free field system in saturated soft soil, the free field nonlinearity fully coupled numerical model of dynamical effective stress of saturated soft soil was established using OpenSEES, based on the u-p formulations of dynamic consolidation equation as well as effective stress solution method for saturated two-phase media. The numerical simulation of the free field seismic response of saturated soft soil under various test conditions was performed and the calculated results were compared with the shaking table test results. The results show the following. With the increase of input ground motion intensity, the characteristic frequency of the saturated soft free ground decreases and the damping ratio increases gradually. The saturated soft soil ground has short period filtering and long period amplification effect on the horizontal input seismic loads. The failure foundation takes on the isolation and shock absorption under strong ground motions. The peak pore pressure ratio of the saturated soft soil ground is located in the shallow buried soil layer, and with the increase of the input ground motion intensity, the advantage of dynamic pore pressure ratio in this area is gradually weakened. The numerical simulation results are consistent with the results of the shaking table test. This fully coupled effective stress numerical method can reasonably simulate the seismic response characteristics of free field in saturated soft soil, which lay the foundation for other more complex parameter extrapolation models of saturated soft soil sites. This research can provide the necessary technical experience for experimental study on non-free field.
机译:本文研究了饱和软自由场的垂直传播剪切波的振动台试验(1g)和数值模拟(完全耦合)。进行了大型振动台模型试验,以研究饱和软土自由场的地震响应特征。根据饱和软土中自由场系统地震响应特征的测试结果,基于动力固结方程的上式和公式,利用OpenSEES建立了饱和软土动力有效应力的自由度非线性全耦合数值模型。饱和两相介质的有效应力求解方法。对饱和软土在各种试验条件下的自由场地震响应进行了数值模拟,并将计算结果与振动台试验结果进行了比较。结果显示如下。随着输入地震动强度的增加,饱和软自由地的特征频率减小,阻尼比逐渐增大。饱和软土地基对水平输入地震荷载具有短周期滤波和长周期放大作用。破坏的基础是在强地面运动下的隔离和减震。饱和软土的峰值孔隙压力比位于浅埋土层,随着输入地面运动强度的增加,该区域动态孔隙压力比的优势逐渐减弱。数值模拟结果与振动台试验的结果一致。这种完全耦合的有效应力数值方法可以合理地模拟饱和软土中自由场的地震响应特征,为饱和软土场地其他更复杂的参数外推模型奠定基础。该研究可以为非自由领域的实验研究提供必要的技术经验。

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