Seismic Ground Response Analysis of Some Typical Sites of Guwahati City

IF 0.5 Q4 ENGINEERING, GEOLOGICAL International Journal of Geotechnical Earthquake Engineering Pub Date : 2013-01-01 DOI:10.4018/JGEE.2013010106
S. Kumar, A. Krishna
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引用次数: 33

Abstract

In this study, one dimensional equivalent–linear ground response analyses were performed for some typical sites in the Guwahati city, India. Six bore locations covering about 250 km2 area of the city were considered for the analyses. As the strong motion significantly influences the ground response, seven different recorded ground motions, varying in magnitude (6.1 to 8.1) and other ground motion parameters, were adopted. Seismic site analyses were carried out for all layers of borelogs using all the seven earthquakes. Results are presented in terms of surface acceleration histories, strain and shear stress ratio variation, response spectrum, Fourier amplitude ratio versus frequency. The results indicate that accelerations were amplified the most at the surface level. The range of peak ground acceleration (PGA) values obtained at the ground surface is about 0.2 g to 0.79 for a range of PGA considered at bedrock level (rigid half space at bottom of borelog) of 0.1 g to 0.34 g. The Fourier amplifications of ground motion at surface are in the range of 4.14 – 8.99 for a frequency band of 1.75 Hz to 3.13 Hz. The maximum spectral acceleration at six locations varies in the range of 1.0 g – 4.71 g for all the seven earthquakes. The study clearly demonstrated the role for site effect and the type of ground motion on the ground response. For a given earthquake motion, amplification factors at surface level change by almost about 20% to 70% depending on local site conditions.
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古瓦哈提市典型场地地震反应分析
在本研究中,对印度古瓦哈蒂市的一些典型场地进行了一维等效 -线性地面响应分析。分析考虑了覆盖城市面积约250平方公里的6个钻孔地点。由于强震对地面响应的影响较大,因此采用了7种不同震级(6.1 ~ 8.1)的记录地震动及其他地震动参数。利用所有7次地震对钻孔的所有层进行了地震现场分析。结果包括表面加速度历史,应变和剪应力比变化,响应谱,傅立叶振幅比与频率。结果表明,地表加速度放大最大。在基岩水平(钻孔底部的刚性半空间)考虑的峰值地面加速度(PGA)范围为0.1 g至0.34 g,在地表获得的峰值地面加速度(PGA)值范围约为0.2 g至0.79。在1.75 Hz到3.13 Hz的频带范围内,地表地面运动的傅里叶放大在4.14 - 8.99之间。7次地震在6个地点的最大谱加速度在1.0 g - 4.71 g范围内变化。该研究清楚地表明了场地效应和地面运动类型对地面反应的作用。对于给定的地震运动,根据当地的场地条件,地表的放大因子变化约为20%至70%。
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来源期刊
CiteScore
1.90
自引率
25.00%
发文量
11
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