南海西沙典型珊瑚砂岛礁场地地震响应特征影响因素研究

    STUDY ON THE SEISMIC RESPONSE AND ITS INFLUENCE FACTORS OF CORAL REEF ISLAND IN XISHA ISLANDS, SOUTH CHINA SEA

    • 摘要: 针对南海珊瑚砂岛礁场地地震响应问题,本文以南海西沙某典型珊瑚砂岛礁为研究对象,综合考虑岛礁地形地貌以及工程地质条件,建立了岛礁非饱和珊瑚砂层-饱和珊瑚砂层-礁灰岩二维有限元分析模型,并通过现场三分量宽频带地震仪实测的地震数据对模型的适用性和准确性进行了验证。在此基础上,系统探究了珊瑚砂层厚度、珊瑚砂动力学参数、礁灰岩波速和地下水位高度这4个因素对岛礁场地地震响应的影响,主要研究结论如下:(1)在珊瑚砂层厚为15~35 m的条件下,随着珊瑚砂层厚度的增加,PGA放大因子、Arias强度、峰值加速度和残余位移均随之增大,并且PGA放大因子的峰值逐渐集中于1 Hz左右。(2)最大动剪切模量和参考剪应变的研究表明,岛礁珊瑚砂最大动剪切模量越大,岛礁地表的地震反应则越小,岛礁越安全,并且最大动剪切模量对残余位移的影响较参考剪应变更显著,最大动剪切模量和参考剪应变变化约10%时,前者的影响强度约为后者的3~5倍。(3)礁灰岩剪切波速(即珊瑚砂与礁灰岩界面的波速阻抗比)对放大因子的影响较大,对残余位移和峰值加速度的影响则很小。(4)随地下水位增长,各表征场地地震响应的参数值均逐渐增大,这表明地下水位越高,岛礁地震响应越强烈,但是由于正常潮位变化相对于岛礁来说占比很小,导致水位变化对岛礁地震响应的影响有限。(5)对不同变量的影响进行统一化的衡量,结果表明最大动剪切模量对残余位移影响最大,珊瑚砂厚度则对峰值加速度和总Arias强度影响最大。而对于PGA放大因子,礁灰岩的动力特性起到了显著的作用,其敏感性最高。

       

      Abstract: This study focuses on the seismic response and its influencing factors of a typical coral reef island in the Xisha Islands, South China Sea. A 2D FEM numerical model was established, considering the unsaturated condition of coral sand and the topographic, geomorphologic, and engineering geological conditions of the coral reef island. The numerical model was then verified through the recorded seismic data captured by the 3-channel seismometer on the island. The influence of factors such as coral sand thickness, soil dynamic parameters, shear wave velocity of the reef limestone, and groundwater level on the seismic response of the coral reef island was systematically analyzed based on the verified numerical model. The findings are as follows:(1) As the thickness of the coral sand layer increases, the characteristic parameters of seismic response, such as the PGA amplification and the Arias intensity, also increase, and the peak value of the PGA amplification factor gradually concentrates around 1 Hz. (2) Studies on the influence of maximum dynamic shear modulus and reference shear strain on seismic response have shown that the better the dynamic characteristics of coral sand on the island, the smaller the seismic response of the island surface. (3) The shear wave velocity of the reef limestone significantly impacts the PGA amplification factor, while it has a minor effect on residual displacement and peak acceleration. (4) As the groundwater level rises, the values of characteristic parameters of seismic response gradually increase. This result indicates that the higher the groundwater level, the stronger the seismic response of the coral reef island. (5) Normalizing the influence factors has shown that the maximum dynamic shear modulus has the greatest impact on residual displacement, while the coral sand thickness has the greatest influence on peak acceleration and total Arias intensity.

       

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