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ISSN 2096-7780 CN 10-1665/P

天津港填海造陆区地震场地效应分析

Analysis of seismic site effects in Tianjin Port sea reclamation region

  • 摘要: 为了更好的分析填海造陆区的地震场地效应,为工程建设抗震设计提供科学依据。本文以天津市东疆港填海造陆区为例,利用一体化短周期流动地震计采集场地的地脉动噪声,基于噪声水平和垂直向谱比法(H/V谱比法),通过26天固定点位的长时间观测采集场地地脉动噪声,分析了研究场地H/V曲线峰值的一致性。基于固定点位的观测经验,利用卓越频率和深度的转换关系式,通过H/V曲线数据归一化处理得出测线归一化处理剖面图,分析东疆港填海造陆区下低频段有不稳定的H/V峰值,推测在浅层存在吹填土的弱波阻抗界面,在50~200 m深度附近存在较为明显的软沉积界面,场地卓越频率在0.6~1.6 Hz之间,具有1.96~3.99倍的放大倍数下限。本文对东疆港填海造陆区的场地效应估计提供一定的参考价值。

     

    Abstract: In order to better analyze the seismic site effects of land reclamation areas and provide scientific basis for earthquake-resistant design of engineering construction, this paper takes the DongJiang Port land reclamation area in Tianjin as an example. It uses integrated short-period flow seismometers to collect ground motion noise at the site and analyzes the consistency of H/V curve peaks based on noise level and horizontal-to-vertical spectral ratio (H/V ratio) method. Based on long-term observations at 26 fixed points, the ground motion noise at the site is collected, and a normalized profile map is obtained by normalizing H/V curve data using a conversion formula based on excellent frequency and depth. The analysis reveals unstable H/V peak values in the low-frequency range below 50-200 m depth, suggesting weak wave impedance interfaces caused by backfill soil exist in shallow layers, with relatively obvious soft sediment interfaces near depths of 50-200 m. The dominant frequencies at the site are between 0.6 Hz and 1.6 Hz, with amplification factors ranging from 1.96 to 3.99 times lower limit. This study provides some reference value for estimating site effects in Dongjiang Port land reclamation area.

     

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