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Site Response Studies in Pondicherry Region

机译:本地治里地区的现场响应研究

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Site response studies were conducted in Pondicherry region based on the ambient noise recording for short duration to determine the ground response frequencies and corresponding amplifications of soils at eighty three selected locations of Pondicherry. These studies were carried out using short duration data of ambient seismic noise and hammer source. Besides this, multichannel analysis of surface waves (MASW) technique was conducted at these locations to estimate the shear wave velocity to compute the predominant frequencies using frequency-shear wave velocity relationships. Both the studies reveal that the southern part of the study area with alluvial and thick soil cover exhibits low frequency in the range 1 to 3 Hz and the higher frequencies are observed in the northern part of Pondicherry which comprises sandstone/limestone.
机译:在Pondicherry地区根据短时的环境噪声记录进行了场地响应研究,以确定Pondicherry选定的83个地点的地面响应频率和相应的土壤放大率。这些研究是使用环境地震噪声和锤源的短期数据进行的。除此之外,在这些位置进行了多通道表面波分析(MASW)技术,以估计剪切波速度,并使用频率-剪切波速度关系来计算主要频率。两项研究都表明,研究区的南部有冲积层和厚厚的土壤覆盖层,其低频范围为1至3 Hz,而在包括砂岩/石灰岩的本地治里北部则观察到较高的频率。

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