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How topography-dependent are topographic effects? Complementary numerical modeling of centrifuge experiments

机译:地形对地形的依赖性如何?离心实验的互补数值模拟

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Topographic effects, the modification of seismic shaking by irregular topographies compared to flat ground, have been extensively studied. Very few studies, however, have investigated the effects of the stratigraphy and nonlinear response of the underlying geology on topographic amplification. Furthermore, most experimental studies have been performed in the field, where it is often difficult to establish an ideal flat-ground reference station, as well as to characterize the soil properties and their spatial variability in sufficient detail. Dafni [1] recently tested the seismic response of step-like slopes in a series of centrifuge experiments, where the incident motion, reference station and material properties were characterized in detail. In this study, we investigated the influence of the container boundary on topographic effects observed in the centrifuge experiments by performing numerical simulations with and without the container boundary. Our analysis suggested that the rigid-body rocking motion of the centrifuge container likely increased the experimental topographic spectral ratios, contributing to the discrepancy between the simulated and observed spectral ratios. We also found that although the laminar box lateral boundaries caused spurious reflections, they didn't qualitatively affect the ground surface amplification pattern compared to numerical predictions of the same configuration without boundaries. At the same time, and most importantly, however, we found that the baseplate by trapping waves scattered and diffracted by the slope amplified the ground motion at the crest up to one order of magnitude compared to numerical predictions of the response in absence of the baseplate. Our results show that topographic effects can be significantly affected by the underlying soil stratigraphy, and allude to the potentially significant role of this phenomenon in elevating seismic risk in regions with strong topographic relief. The findings of this study also suggest that future studies will benefit from clear understanding and careful considerations of capabilities and limitations of different investigation methods and that the numerical modeling and the lab testing (or the field testing) methods should complement each other.
机译:与平坦地面相比,地形效应是不规则地形对地震震动的修正。但是,很少有研究研究地层的地层学和非线性响应对地形放大的影响。此外,大多数实验研究都是在野外进行的,在野外通常很难建立理想的平地参考站,而且很难足够详细地描述土壤特性及其空间变异性。 Dafni [1]最近在一系列离心实验中测试了阶梯状斜坡的地震响应,其中详细描述了入射运动,参考站和材料特性。在这项研究中,我们通过在有和没有容器边界的情况下进行数值模拟,研究了容器边界对离心机实验中观察到的地形影响的影响。我们的分析表明,离心容器的刚体摇摆运动可能会增加实验地形光谱比,从而导致模拟光谱比与观察光谱比之间的差异。我们还发现,尽管层状盒子的横向边界引起了虚假反射,但是与没有边界的相同配置的数值预测相比,它们没有定性地影响地面放大模式。同时,最重要的是,我们发现,与不存在底板时响应的数值预测相比,底板通过捕获由坡度散射和衍射的波将波峰处的地面运动放大了一个数量级。 。我们的结果表明,地形影响可能会受到潜在的土壤地层的显着影响,并且暗示了这种现象在增强具有强烈地形起伏地区的地震风险中的潜在重要作用。这项研究的结果还表明,未来的研究将受益于对不同调查方法的功能和局限性的清楚理解和仔细考虑,并且数值建模和实验室测试(或现场测试)方法应相互补充。

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