Ground-Motion Modeling of the 2016 Mw 6.2 Amatrice, Italy, Earthquake, by a Broadband Hybrid Kinematic Approach, Including Empirical Site Effects

František Čejka, Ľubica Valentová Krišková, S. Sgobba, F. Pacor, F. Gallovič
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引用次数: 1

Abstract

The region of Central Italy is well known for its moderate to large earthquakes. Events such as the 2016 Mw 6.2 Amatrice earthquake generated in the shallow extensional tectonic regime motivate numerical simulations to gain insights into source-related ground-motion complexities in the near-source region. We utilize a hybrid integral-composite kinematic rupture model by Gallovič and Brokešová (2007) to simulate the Amatrice earthquake in a broadband frequency range (up to 10 Hz). In the first step, we optimize the input source parameters using a grid-search method by minimizing the spectral acceleration bias between synthetic and recorded strong-motion data at reference rock stations within 50 km of the source. To verify the robustness of the optimal model, we simulate the ground motions at 400 virtual stations and compare their spectral accelerations with the predictions of an empirical nonergodic ground-motion model (GMM) for rock sites in Central Italy (Sgobba et al., 2021). The synthetics show a good agreement with the empirical model regarding both median and variability. Finally, we account for local site effects at nonreference stations by combining the simulations on rock with empirical site terms derived by the nonergodic GMM. The site-corrected spectral responses generally improve the match with the observations, demonstrating a successful fusion of numerical simulations with empirical estimates toward reproducing near-source ground motions.
采用宽带混合运动学方法(包括经验场地效应)对 2016 年意大利阿马特里斯 6.2 级地震进行地动建模
意大利中部地区以发生中到大型地震而闻名。2016 年阿马特里斯 6.2 级地震(Mw 6.2 Amatrice)发生在浅伸展构造体系中,这促使我们通过数值模拟来深入了解近震源地区与震源相关的地动复杂性。我们利用 Gallovič 和 Brokešová(2007 年)的混合积分复合运动学破裂模型,在宽带频率范围(最高 10 Hz)内模拟了阿马特里斯地震。第一步,我们使用网格搜索法优化输入震源参数,最大限度地减小震源 50 公里范围内参考岩石站合成数据与记录强震数据之间的频谱加速度偏差。为了验证优化模型的稳健性,我们模拟了 400 个虚拟站点的地动,并将其频谱加速度与针对意大利中部岩石站点的经验非啮合地动模型(GMM)(Sgobba 等人,2021 年)的预测结果进行了比较。合成结果表明,在中位数和变异性方面,合成结果与经验模型都非常吻合。最后,我们通过将岩石模拟与非啮合 GMM 得出的经验站点项相结合,考虑了非参考站点的局部站点效应。经过场地校正的频谱响应总体上提高了与观测结果的匹配度,这表明数值模拟与经验估算的融合取得了成功,从而重现了近源地动。
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