Site effect estimation using H/V microtremor and shallow seismic prospecting, Elkawamel, Sohag, Egypt

A. Abudeif, Marwa Marwa M. Masoud
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Abstract

: Shallow seismic refraction survey and Microtremor measurements together were conducted and found out to be an effective approach to study the site effect and also to establish a seismic hazard microzonation overview. The amplification and fundamental resonance frequency and of ground motion at different frequencies were estimated using the microtremor data measured at ten sites in the new industrial zone around the urban areas in Sohag Governorate, Egypt. Also, site effects were calculated applying a numerical technique using shear wave velocities observed from measured profiles at the study area utilizing 24-channel shallow seismic refraction seismograph. The results show variations in the fundamental resonance frequency values from one site to another depending on its distance from the Eocene plateau scarp that located at the southern and southwestern sides of the study area, where it becomes higher close to the plateau foot. In case of the low frequency, the amplification of the ground motion shows variation from site to the other site depending on its vicinity to the plateau, while in case of high frequency the variation depends on the thickness of the sediment layers. The results using the microtremor technique emphasize that given by the shallow seismic refraction method.
利用H/V微震和浅层地震勘探估算埃及Sohag Elkawamel地区场地效应
浅层地震折射测量和微震测量相结合,是研究场地效应和建立地震危险性微分区概况的有效方法。利用在埃及Sohag省城市周围新工业区的十个地点测量的微震数据,估计了不同频率下地面运动的放大和基本共振频率。此外,利用24通道浅层折射地震仪从研究区实测剖面观测到的横波速度,应用数值技术计算了场地效应。结果表明,不同测点的基本共振频率值随其与始新世高原陡坡(位于研究区南部和西南两侧)的距离而变化,在靠近高原脚的地方频率值越高。在低频情况下,地面运动的放大表现出不同地点之间的变化,这取决于其与高原的距离,而在高频情况下,这种变化取决于沉积层的厚度。微震技术的结果强调了浅层地震折射法的结果。
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