Multi-step procedure for estimating nonlinear soil response in low seismicity areas – a case study of Lucerne, Switzerland

IF 2.8 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Paulina Janusz, Paolo Bergamo, Luis Fabian Bonilla, Francesco Panzera, Daniel Roten, Karina Loviknes, Donat Fäh
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Abstract

Summary The impact of nonlinear soil behaviour on seismic hazard in low-to-moderate seismicity areas is often neglected; however, it may become relevant for long return periods. In this study, we employed fully nonlinear 1D simulations to estimate the site-specific nonlinear soil response in the low seismicity area, using the city of Lucerne in Switzerland as an example. The constitutive model considers the development of pore pressure excess and requires calibration of complex soil models, including the soil dilatancy parameters. In the absence of laboratory measurements, we mainly used the cone penetration test (CPT) data to estimate the model variables and perform inversion for the dilatancy parameters. Our findings, using Swiss building code-compatible input ground motions, suggest a high probability of strong nonlinear behaviour and the possibility of liquefaction at high ground motion levels in the case study area. While the nonlinearity observations from strong-motion recordings are not available in Lucerne, the comparison with empirical data from other sites and other methods shows similarity with our predictions. Moreover, we show that the site response modelled is largely influenced by the strong pore pressure effects produced in thin sandy water-saturated layers. In addition, we demonstrate that the variability of the results due to the input motion and the soil parameters is significant, but within reasonable bounds.
估算低地震区非线性土壤响应的多步骤程序--瑞士卢塞恩案例研究
摘要 非线性土壤行为对中低震度地区地震危害的影响往往被忽视;然而,它可能与长重现期相关。在本研究中,我们以瑞士卢塞恩市为例,采用全非线性一维模拟估算了低地震区特定场地的非线性土壤响应。构成模型考虑了孔隙压力过剩的发展,需要校准复杂的土壤模型,包括土壤膨胀参数。在缺乏实验室测量的情况下,我们主要使用锥入度试验(CPT)数据来估算模型变量,并对膨胀性参数进行反演。我们使用与瑞士建筑规范兼容的输入地面运动进行了研究,结果表明,在案例研究区域,强非线性行为的概率很高,在高地面运动水平下有可能发生液化。虽然卢塞恩没有强地震动记录的非线性观测数据,但与其他地点的经验数据和其他方法进行比较后发现,我们的预测结果与之相似。此外,我们还表明,所模拟的场地响应在很大程度上受到了水饱和薄砂层中产生的强大孔隙压力效应的影响。此外,我们还证明,输入运动和土壤参数对结果的影响很大,但都在合理范围内。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geophysical Journal International
Geophysical Journal International 地学-地球化学与地球物理
CiteScore
5.40
自引率
10.70%
发文量
436
审稿时长
3.3 months
期刊介绍: Geophysical Journal International publishes top quality research papers, express letters, invited review papers and book reviews on all aspects of theoretical, computational, applied and observational geophysics.
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