KUET输入地震运动及场地放大系数的地面反应分析

S. Akter
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引用次数: 1

摘要

地面运动是由于爆炸或地震波的传播引起的地球表面的运动。在抗震设计过程中,地面反应分析评估了地震时当地土壤条件的影响。然而,在地震易发地区,确定土壤沉积物的动力场地响应是困难的。结构损伤对输入地震动的选择有很大的影响,在本研究中强调了基岩运动对土壤响应的重要性。具体场地响应分析通过“DEEPSOIl”软件进行评估,采用等效线性分析方法。选择Kobe、LomaGilroy、Northridge和Chi-Chi 4种输入运动,得到归一化响应谱。本研究旨在通过对库尔纳工程技术大学Bangabandhu Sheikh Mujibor Rahman大厅的详细场址分析,获得基于横波速度的地震动场址放大、峰值谱加速度(PSA)和最大峰值地加速度(PGA)。得到的最大横波速度为205 m/s,刚性基岩的放大系数在4.01 ~ 1.8之间。此外,神户地震对基岩的PSA值最高(4.3g),北岭地震对基岩的PSA值最低(1.08g), Vs=205 m/s。地面PGA值在0.254g(北岭)~ 0.722g(神户)之间,神户地震的最大应变值在0.016 ~ 0.303之间。因此,神户地震运动的地表加速度值非常高(>0.12g)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seismic Ground Response Analysis of Input Earthquake Motion and Site Amplification Factor at KUET
Ground motion is the movement of the earth's surface due to explosions or the propagation of seismic waves. In the seismic design process, ground response analysis evaluates the impact of local soil conditions during earthquake shaking. However, it is difficult to determine the dynamic site response of soil deposits in earthquake hazard-prone areas. Structural damage has a great influence on the selection of input ground motion, and in this study, the importance of bedrock motion upon the response of soil is highlighted. The specific site response analysis is assessed through “DEEPSOIl" software with an equivalent linear analysis method. Furthermore, four input motions including Kobe, LomaGilroy, Northridge, and Chi-Chi were selected to obtain normalized response spectra. This study aims to obtain the site amplification of ground motion, peak spectral acceleration (PSA), and maximum peak ground acceleration (PGA) based on shear wave velocity from the detailed site-specific analysis of Bangabandhu Sheikh Mujibor Rahman hall at Khulna University of Engineering & Technology. The maximum shear wave velocity obtained was 205 m/s while the amplification factor varied from 4.01 (Kobe) to 1.8 (Northridge) for rigid bedrock properties. Furthermore, the Kobe earthquake produced the highest (4.3g) PSA and the Northridge earthquake produced the lowest (1.08g) PSA for bedrock, with Vs=205 m/s. The surface PGA values were acquired in the range of 0.254g (Northridge) to 0.722g (Kobe), and the maximum strain values for Kobe earthquakes were in the range of 0.016 to .303. Therefore, the surface acceleration values were very high (>0.12g) for the Kobe earthquake motion.
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