土耳其地震强震区近地表剪切波速对地震地面运动的影响及对中国设计谱特征参数修订的启示

    Influence of near-surface shear wave velocity on seismic ground motion of Turkey earthquake and implications for revision of characteristic parameters of seismic design response spectrum in China

    • 摘要: 2023年2月6日土耳其Mw7.8级强烈地震为典型的浅源走滑型地震,造成大规模地表破裂,近断层区域出现超预期的强烈地震动,导致大量房屋倒塌。基于土耳其地震断裂两侧60 km范围内的强震动记录,系统开展强震区地震动峰值、频谱、持时的空间分布特征研究,深入剖析场地表层30 m范围内平均剪切波速(VS30)对地震动特性的影响规律;并全面开展近断层实际地震反应谱与中国抗震设计反应谱的对比分析,重点探讨反应谱特征参数与中国规范设计取值的差异。结果表明:①土耳其地震断裂两侧60 km区域以Ⅰ1类和Ⅱ类场地为主,峰值加速度大于0.40g以及峰值加速度比值超过3的强烈地面运动主要分布在距离断裂30 km范围内,且普遍为速度脉冲型地震动;②峰值加速度比值随VS30衰减的拟合结果与经验关系非常接近,而能量持时随VS30的变化规律不明显;③反应谱特征周期及动力放大系数均随VS30的增大而减小,91.7%的反应谱特征周期及29.2%的动力放大系数均超过中国规范取值;④类似此次土耳其地震若发生在中国9度设防地区,Ⅰ1类场地-设计地震分组为第一组的设计谱在周期0.65~2.30 s、Ⅱ类场地-设计地震分组为第一组的设计谱在周期0.50~2.45 s,均未能满足抗震设防的需要。宜适当提高设计反应谱平台高度和增加平台段宽度以适应高烈度地震作用。

       

      Abstract: The powerful Mw7.8 earthquake that struck Turkey on February 6, 2023, was a typical shallow-source strike-slip earthquake. It caused large-scale surface fractures and unexpectedly strong ground tremors in the near-fault area, leading to the collapse of a large number of buildings. Based on strong-motion records within a 60 km range on both sides of the earthquake fault in Turkey, the spatial distribution characteristics of the peak, spectrum and duration of ground motion in the strong earthquake area are systematically studied, and the influence law of the average shear wave velocity (VS30) within a 30-meter range of the site surface on the ground motion characteristics is deeply analyzed. A comparative analysis of the actual seismic response spectrum near faults in Turkey and the seismic design response spectrum in China is comprehensively carried out, with a focus on discussing differences between characteristic parameters of actual response spectrum and the values taken in Chinese design code. The results show that: (1) In the 60 km area on both sides of the earthquake fault in Turkey, the sites are mainly of type Ⅰ1 and type Ⅱ. The intense ground movements with peak accelerations greater than 0.40g and peak acceleration ratios exceeding 3 are mainly distributed within 30 km of the fault, and they are generally velocity pulse type ground motions. (2) The fitting result of the peak acceleration ratio attenuation with VS30 is very close to the empirical relationship, while the variation law of energy duration with VS30 is not obvious. (3) Both the characteristic period and the dynamic amplification factor of response spectrum decrease with the increase of VS30 91.7% of the characteristic periods and 29.2% of the dynamic amplification factors of response spectrum exceed the values specified in Chinese design code. (4) Similar to the recent earthquake in Turkey, if it occurred in a 9-degree seismic fortification area of China, the design spectrum for site class Ⅰ1 and design earthquake group 1 in the period range of 0.65~2.30 s, and that for site class Ⅱ and design earthquake group 1 in the period range of 0.50~2.45 s, neither of which can meet the requirements of seismic fortification. It is advisable to appropriately increase the height of the design response spectrum platform and the width of the platform section to adapt to the high-intensity seismic action.

       

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