2016年10月30日意大利MW6.6地震破裂方向性效应对地震动参数的影响

Rupture directivity effect on the seismic ground motion parameter during Italy MW6.6 earthquake on October 30,2016

  • 摘要: 2016年10月30日意大利中部发生了MW6.6地震,这是继8月24日MW6.2地震后的又一次浅源破坏性地震,意大利国家强震台网在此次地震中获得了丰富的强震动三分向加速度记录。本文从工程强震动数据中心下载了三分向加速度记录,经基线校正和滤波等常规数据处理后发现,强震动体现出明显的方向性效应。根据震源机制解将强震动台站分为破裂前方区域的NW组和破裂后方区域的SE组,采用最小二乘法回归了不同分组的地震动峰值加速度、反应谱和持时的衰减规律,得出断层破裂方向性对地震动参数的幅值影响较大,在断层距相同的情况下,破裂前方区域的加速度和加速度反应谱幅值均高于破裂后方区域,而破裂前方区域的地震动持时远小于破裂后方区域,破裂方向性显著。

     

    Abstract: On October 30, 2016, another shallow-source MW6.6 earthquake occurred in cen-tral Italy after August 24 MW6.2 earthquake. A large number of three-component acceleration recordings of strong ground motion were collected by Italian strong-motion network and were downloaded from Engineering Strong Motion database (ESM) and analyzed by the base-line correction, filtering and other conventional data processing. Strong motion observation stations were divided into two groups as front rupture area NW and rear rupture area SE according to the focal mechanism solutions. Attenuation relationships of ground motion parameters, including amplitude, response spectrum and durations, were regressed by using the least squares method in the different two groups and we found that acceleration amplitude was affected by rupture directivity remarkably, and the amplitude and response spectrum of acceleration in the NW group were greater than those in the SE group in the case of the same Joyner-Boore distance RJB, while the duration in NW group was more less than that in SE group. In conclusion, near-source ground motion recordings were much rich and the characteristics of strong ground motion were greatly influenced by rupture directivity.

     

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