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首页> 外文期刊>Journal of King Saud University >Engineering bedrock depth estimation and ground response analysis of the northern Jeddah urban area, western Saudi Arabia
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Engineering bedrock depth estimation and ground response analysis of the northern Jeddah urban area, western Saudi Arabia

机译:北部吉达市区北部沙特阿拉伯的工程基岩深度估算与地基响应分析

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The engineering bedrock depth was determined in the northern Jeddah urban area via multichannel analysis of surface waves (MASW) conducted at 76 locations. Depths corresponding to the velocity ranges were estimated below the ground surface and mapped. The engineering bedrock depth was evaluated and it varies from 0 to approximately 36.23?m whereas the depth increased eastward. Further, ground response analysis was conducted to assess the seismic hazard in terms of peak ground acceleration, where it ranges from 3.37 to 17.71?cm/s2, considering the fundamental resonance frequency and amplification potential at the sites of measurement. These variations are due to differences in the soil profile at each location; ground surface acceleration increased at sites with thick layers of soft sediments. In addition, the spectral acceleration and response spectra were assessed at the ground surface with a 5% damping ratio for the identified lithological units. Peak spectral acceleration varies from 16.8 to 62.6?cm/s2. The eastern zone has a higher spectral acceleration than the western zone while the frequency corresponding to the spectral acceleration varies from 1.05 to 14.28?Hz. The spectral acceleration and response spectra are used for assessment the spectrum of structures. Ground response analysis shows that because of the soil condition, potential amplification of wave amplitudes is observed at the ground surface when compared to the engineering bedrock level acceleration. These results should be provided to civil engineers, land-used planners, and decision makers during the designing of either new buildings or rehabilitation of pre-existing structures.
机译:通过在76个地点进行的表面波(MasW)的多通道分析,在吉德达市区北部北部北部城市地区确定了工程基岩深度。对应于速度范围的深度估计在地面下方并映射。评估工程基岩深度,其变化从0到大约36.23Ω·m,而深度向东增加。此外,进行地面响应分析以评估峰接地加速度的地震危害,其中它范围为3.37至17.71〜3m / s2,考虑到测量部位的基本共振频率和放大潜力。这些变化是由于每个位置的土壤轮廓的差异;地面加速度在厚厚的软沉积物层的位置增加。另外,在接地表面上评估光谱加速度和响应光谱,具有识别的岩性单元的5%阻尼比。峰值谱加速度从16.8到62.6?cm / s2变化。东部区具有比西方区更高的光谱加速度,而对应于光谱加速度的频率从1.05到14.28?Hz变化。光谱加速度和响应光谱用于评估结构的光谱。地面响应分析表明,由于土壤条件,与工程基岩水平加速相比,在地面观察到地面的波幅的潜在放大。这些结果应在设计新建筑物或预先存在的结构的康复期间向土木工程师,土地使用的规划者和决策者提供。

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