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Investigating the influence of topographic irregularities and two-dimensional effects on surface ground motion intensity with one-and two-dimensional analyses

机译:用一维和二维分析研究地形不规则性和二维效应对地表运动强度的影响

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In this work, the surface ground motion that occurs during an earthquake in ground sections having different topographic forms has been examined with one and two dynamic site response analyses. One-dimensional analyses were undertaken using the Equivalent-Linear Earthquake Response Analysis (EERA) program based on the equivalent linear analysis principle and the Deepsoil program which is able to make both equivalent linear and nonlinear analyses and two-dimensional analyses using the Plaxis 8.2 software. The viscous damping parameters used in the dynamic site response analyses undertaken with the Plaxis 8.2 software were obtained using the DeepSoil program. In the dynamic site response analyses, the synthetic acceleration over a 475-year return period representing the earthquakes in Istanbul was used as the basis of the bedrock ground motion. The peak ground acceleration obtained different depths of soils and acceleration spectrum values have been compared. The surface topography and layer boundaries in the 5-50 cross section which cuts across the study area west to east were selected in order to examine the effect of the land topography and layer boundaries on the analysis results, and were flattened and compared with the actual status. The analysis results showed that the characteristics of the surface ground motion change in relation to the varying local soil conditions and land topography.
机译:在这项工作中,通过一次和两次动态场地响应分析,研究了地震在具有不同地形形式的地段中发生的地表地面运动。使用基于等效线性分析原理的等效线性地震响应分析(EERA)程序和Deepsoil程序进行一维分析,该程序能够使用Plaxis 8.2软件进行等效线性和非线性分析以及二维分析。使用DeepSoil程序获得使用Plaxis 8.2软件进行的动态场地响应分析中使用的粘性阻尼参数。在动态场地响应分析中,代表伊斯坦布尔地震的475年回归期内的综合加速度被用作基岩地面运动的基础。获得了不同深度土壤的峰值加速度,并比较了加速度谱值。为了研究陆地地形和层边界对分析结果的影响,选择了从研究区域西向东横切的5-50横截面中的表面地形和层边界,并将其展平并与实际进行比较。状态。分析结果表明,地表运动特征随当地土壤条件和地形的变化而变化。

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