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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 the Tianjin port sea reclamation region

  • 摘要: 为了更好地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 d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。分析得出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。本文可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: To better analyze the seismic site effects in land reclamation areas and provide a scientific basis for earthquake-resistant engineering design, this study investigates the Dongjiang port land reclamation area in Tianjin. Integrated short-period flow seismometers were used to collect ground motion noise at the site, and the consistency of horizontal-to-vertical (H/V) spectral ratio peaks was analyzed using noise level and H/V ratio methods. Based on long-term observations at 26 fixed points, ground motion noise was recorded, and a normalized profile map was generated by converting the H/V curve data using a formula based on dominant frequency and depth. The analysis revealed unstable H/V peak values in the low-frequency range below depths of 50~200 m, suggesting that weak wave impedance interfaces caused by backfill soil exist in the shallow subsurface, with relatively distinct soft sediment interfaces near depths of 50~200 m. The dominant frequencies at the site range from 0.6 Hz to 1.6 Hz, with amplification factors between 1.96 and 3.99. This study provides a useful reference for estimating site effects in the Dongjiang port land reclamation area.

     

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