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Elastic and Large-Strain Nonlinear Seismic Site Response from Analysis of Vertical Array Recordings

机译:垂直阵列记录分析的弹性和大应变非线性地震现场响应

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摘要

Strong ground motions from the M_w = 6.6 2007 Niigata-ken Chuetsu-oki earthquake were recorded by a free-field downhole array at a nuclear power plant. Site conditions consist of about 70 m of medium-dense sands overlying clayey bedrock, with groundwater located at 45 m. Ground shaking at the bedrock level had a geometric mean peak acceleration of 0.55g, which reduced to 0.4g at the ground surface, indicating nonlinear site response. One-dimensional ground response analysis of relatively weak motion aftershock data provides good matches of the observed resonant site frequencies and amplification levels, provided small-strain damping levels somewhat larger than those from laboratory tests are applied. Nonlinear ground response analyses of strong-motion data using laboratory-based modulus reduction and damping relations valid up to moderate strain levels (<~0.5%) produce unrealistic strain localization at a velocity contrast. A procedure is presented to more realistically represent the large-strain portion of backbone curves by asymptotically approaching the shear strength at large strains, which removes strain localization for this application and provides reasonable matches of observed and computed ground motions.
机译:通过核电厂的自由场井下阵列记录了M_w = 6.6 2007年新泻县中越冲木地震的强烈地面运动。场地条件包括覆盖在粘土质基岩上的约70 m中等密度沙子,地下水位于45 m处。基岩水平的地面震动具有0.55g的几何平均峰值加速度,在地面上降低到0.4g,表明非线性的场地响应。相对较弱的运动余震数据的一维地面响应分析提供了所观察到的共振点频率和放大水平的良好匹配,前提是小应变阻尼水平要比实验室测试的水平大一些。使用基于实验室的模量减少和阻尼关系对强运动数据进行非线性地面响应分析,直到有效的中等应变水平(<〜0.5%)为止,阻尼关系在速度对比下产生不切实际的应变局部化。通过渐近逼近大应变时的剪切强度,提出了一种方法来更现实地表示主干曲线的大应变部分,这消除了此应用的应变局部性,并提供了观测和计算的地面运动的合理匹配。

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