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Effect of Sudden Shear Wave Velocity Contrast at Shallow Layer Interfaces on the Seismic Site Response for Charleston, SC

机译:浅层界面处突然的剪切波速度反差对南卡罗来纳州查尔斯顿地震现场响应的影响

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In practice, seismic site response analysis is often conducted with the entire soil profile being divided into a number of sub soil layers and site-specific parameters, such as shear wave velocity (V_s), damping and modulus reduction, are assumed to be constant within the extent of each layer. In this study, the effect of large contrast in V_s at shallow layer interfaces on the computed surface response is investigated considering the geologic and seismic settings for the Charleston, SC area. The Vs profiles with sudden contrast at shallow depth were smoothened systematically using various hypothetical gradients to obtain derived Vs profiles. The computed responses from the original and the derived profiles were then compared. The hypothetical profiles produced lesser shear strains and greater surface accelerations as compared to the corresponding original profiles with significant V_s contrast. Therefore, such simplification of V_s profiles should be avoided in site response analysis, unless they represent actual geologic conditions.
机译:在实践中,通常在将整个土壤剖面分为多个子土壤层的情况下进行地震场响应分析,并且假设特定于现场的参数(例如,剪切波速度(V_s),阻尼和模量减少)在恒定范围内。每层的范围。在这项研究中,考虑了南卡罗来纳州查尔斯顿地区的地质和地震环境,研究了浅层界面处V_s大对比度对计算的表面响应的影响。使用各种假设的梯度系统地平滑浅深度处具有突然对比的Vs轮廓,以获得派生的Vs轮廓。然后比较原始轮廓和派生轮廓的计算响应。与具有明显V_s对比的相应原始轮廓相比,假设轮廓产生的剪切应变较小,表面加速度较大。因此,在现场响应分析中应避免V_s剖面的这种简化,除非它们代表实际的地质条件。

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