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Response Spectra for Design Purpose of Stiff Structures on Rock Sites

机译:用于岩石场地刚性结构设计的响应谱

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Based on analyses of earthquake ground motion records on rock, we propose an empirical method for evaluatingresponse spectra and time-dependent features of horizontal and vertical earthquake ground motions on free rock surfaces.This method is aimed at aseismic design of nuclear power facilities. A response spectrum of horizontal earthquake groundmotion on seismic bedrock is given by a control point in the matrix formed by four magnitudes M = 6.0, 7.0, 8.0, and 8.5;and four equivalent hypocentral distances X_(eq) defined as very near, near, intermediate, and far. The response spectra for other M and X_(eq) e are determined by interpolation between values in the matrix. The response spectra of the horizontal and vertical ground motions on the free rock surface are determined by multiplying the horizontal motion on the seismicbedrock by the amplifications of horizontal and vertical motions due to surface layers. The amplifications by the surfacelayers are given as a function of S-wave velocities V s from 0.5 to 2.7 km/s for horizontal components and as a function ofP-wave velocities V_p from 1.7 to 5.5 km/s for vertical components on the free rock surface. The time-dependent envelopeand the correction coefficient of the response spectrum due to a damping factor are given as functions of M and X_(eq).Examination of the evaluation equation's applicability using observations from inside and outside Japan show that theevaluation method can adequately explain both the observation records of large earthquakes and of near-source regions.
机译:在对岩石地震地震动记录进行分析的基础上,提出了一种评估自由岩石表面水平和垂直地震地震动响应谱和时变特征的经验方法,该方法针对核动力设施的抗震设计。地震基岩上水平地震地震动的响应谱由矩阵中的一个控制点给出,该控制点由四个量级M = 6.0、7.0、8.0和8.5组成;四个等效下摆距离X_(eq)定义为非常近,非常近,中级和远级。其他M和X_(eq)e的响应谱是通过矩阵值之间的插值确定的。通过将地震基岩上的水平运动乘以表层引起的水平和垂直运动的放大倍数,可以确定自由岩石表面上水平和垂直地面运动的响应谱。对于自由分量,表层的放大率是水平分量的S波速度V s从0.5至2.7 km / s的函数,垂直分量的P波速度V_p从1.7至5.5 km / s的函数给出的表面。给出了随时间变化的包络线和由阻尼因子引起的响应谱的校正系数,作为M和X_(eq)的函数。使用日本国内外的观察结果对评估方程的适用性进行检验,表明评估方法可以充分解释大地震和近震源地区的观测记录。

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