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Estimation of Nonlinear Time-dependent Soil Behavior in Strong Ground Motion Based on Vertical Array Data

机译:基于垂直阵列数据的强时震动中非线性时变土壤行为估计

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摘要

To improve our understanding of nonlinear elastic properties of soils, a method is proposed of estimation of stress-strain relations of soils in situ in strong ground motion based on vertical array data. Strong motion records provided by seismic vertical arrays allow estimation of nonlinear stress-strain relations in soils layers at different depths, from the surface down to the location of the deepest device. As an example, records obtained during the main shock of the 1995 Kobe earthquake at Port-Island, SGK, and TKS sites were used to estimate the stress-strain relations were selected, according to the profiling data. To account for temporal changes in the soil behavior, consecutive parts of records were examined, and for successive time intervals, the relations were found showing the best-fit approximation to the observed data. At Port Island and SGK sites, where the strongest accelerations were recorded, the obtained stress-strain relations showed systematic changes in the upper layer (0-14 m), such as, a progressive reduction of the slopes of the stress-strain curves due to liquefaction at Port Island and reduction and recovery of the slopes at SGK and TSK site. at the three site, the stress-strain relations remained stable in layers below 11-14 m. Thus, the proposed approach gives us a representation of the soil behavior in layers at different depths in strong ground motion; it allows calculation of the propagation of arbitrary seismic signals in the studied profiles and estimation of nonlinear components in the ground response by the nonlinear system identification technique. The method can also be applied to evaluate the ground response at sites where profiling data are available and an imposed motion can be estimated.
机译:为了增进我们对土壤非线性弹性特性的理解,提出了一种基于垂直阵列数据估算强地面运动中土体应力应变关系的方法。地震垂直阵列提供的强运动记录允许估算从表面到最深设备位置不同深度的土壤层中的非线性应力-应变关系。例如,根据分析数据,选择了1995年神户地震在Port-Island,SGK和TKS站点的主震中获得的记录,以估计应力-应变关系。为了说明土壤行为的时间变化,对记录的连续部分进行了检查,并针对连续的时间间隔,发现了显示与观测数据最接近的最佳关系。在记录到最强加速度的波特兰岛和SGK站点,所获得的应力-应变关系显示出上层(0-14 m)的系统变化,例如,由于应力-应变曲线的斜率逐渐减小港口岛的液化以及SGK和TSK站点的坡度减少和恢复。在这三个位置,应力-应变关系在11-14 m以下的层中保持稳定。因此,所提出的方法使我们能够表现出强地面运动中不同深度的土壤层的行为。它允许计算非线性地震信号在所研究剖面中的传播,并通过非线性系统识别技术估算地面响应中的非线性分量。该方法还可以用于评估可获得轮廓数据并可以估计施加的运动的站点的地面响应。

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