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Site Classification of the Strong Motion Stations of Uttarakhand, India, Based on the Model Horizontal to Vertical Spectral Ratio

机译:基于水平与垂直光谱比模型的印度北阿坎德邦强运动台站点分类

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In order to monitor the ongoing seismicity in different parts of the active regions of India, 300 state of the art digital strong motion accelerographs are installed. The accelerograms from the recording stations are available in PESMOS website. The recording stations are classified based on the physical description of local geology and not based on in-situ field tests. Thus, there exist an ambiguity in the assessment of local site conditions for these recording stations. Unless the site class (SC) is known, recorded ground motions cannot be used with confidence. Several research efforts have been directed towards the use of horizontal to vertical spectral ratio (HVSR) technique as a tool to access the local site condition. There is consensus among the scientific community regarding the peak frequency (f_(peak)) obtained from the HVSR method to identify the soil fundamental frequency. In this study, theoretical HVSR curves for 12 recording stations located in the Tarai region of Uttarakhand are generated using a Matlab tool called Model HVSR to obtain the fpeak and peak amplification (A_(peak)). Further, these values of fpeak and Apeak for all the 12 recording stations are estimated using the HVSR based on strong ground motion records. Results obtained from both the above methods show 1:1 correspondence. The values of fpeak obtained for 12 stations range from 1 Hz to 5 Hz based on model HVSR and from 1.1 Hz to 3.3 Hz using the HVSR based on strong ground motion records. These findings are also matching with the existing field studies. Present analyses show a clear difference in the SCs suggested by PESMOS and the one obtained from the present study. Once correct information on SC is known, recorded ground motion at each station can be used with confidence.
机译:为了监测印度活跃地区不同地区的地震活动,安装了300台先进的数字式强震动加速度计。在PESMOS网站上可以找到来自记录站的加速度图。记录站是根据本地地质的物理描述而不是根据现场测试进行分类的。因此,在对这些记录站的本地站点条件的评估中存在歧义。除非知道站点类别(SC),否则不能放心使用记录的地面运动。已经进行了一些研究工作,以利用水平对垂直光谱比(HVSR)技术作为访问本地现场条件的工具。对于通过HVSR方法确定土壤基频的峰值频率(f_(peak)),科学界达成共识。在这项研究中,使用称为HVSR的Matlab工具生成了位于北阿坎德邦塔莱地区的12个记录站的理论HVSR曲线,以获得峰值和峰值放大率(A_(peak))。此外,基于强地面运动记录,使用HVSR估算了所有12个记录站的fpeak和Apeak值。从以上两种方法获得的结果均显示为1:1对应。基于HVSR模型,从12个站点获得的fpeak值范围从1 Hz到5 Hz,而基于强地面运动记录,使用HVSR获得的fpeak值从1.1 Hz到3.3 Hz。这些发现也与现有的现场研究相吻合。目前的分析表明,PESMOS建议的SC与从本研究获得的SC之间存在明显的差异。一旦知道了关于SC的正确信息,就可以放心地使用每个站上记录的地面运动。

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