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首页> 外文期刊>Bulletin of the Seismological Society of America >Empirical Prediction Equations for Peak Ground Velocity Derived from Strong-Motion Records from Europe and the Middle East
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Empirical Prediction Equations for Peak Ground Velocity Derived from Strong-Motion Records from Europe and the Middle East

机译:从欧洲和中东的强运动记录推导出峰值地面速度的经验预测方程

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摘要

Peak ground velocity (PGV) has many applications in earthquake engineering, but there are relatively few prediction equations for this parameter in comparison with the large numbers of equations for estimating peak ground acceleration and response spectral ordinates. This lack of empirical equations for PGV has led to widespread use of the practice of scaling peak velocity from the 5%-damped response spectral ordinate at 1 sec, which is a poor substitute for direct prediction of the parameter. Responding to the need to provide equations for the prediction of PGV, this article derives new equations using the strong-motion database for the seismically active areas of Europe and the Middle East, following a new processing of all of the records. A total of 532 strong-motion accelerograms recorded at distances of up to 100 km from 131 earthquakes with moment magnitudes ranging from M 5 to 7.6 are used to derive equations for both the larger and the geometric mean of the horizontal components. The predictions are found to be broadly consistent with those from previous European equations, and also with preliminary results from the Next Generation of Attenuation (NGA) project, suggesting that systematic differences in ground motions from active crustal regions, if any, are sufficiently small not to prevent the combined use of strong-motion data from southern Europe, western North America, and other tectonically active areas of shallow crustal seismicity.
机译:峰值地面速度(PGV)在地震工程中有许多应用, ,但是与大量的估计方程相比,该参数 的预测方程相对较少峰值地面加速度和响应频谱纵坐标。 PGV经验公式的这种 不足,导致从5%阻尼的 响应光谱纵坐标缩放峰值速度的实践得到广泛使用。 1秒,这不能很好地替代 来直接预测参数。响应 需要提供用于预测PGV的方程,本文 使用强运动数据库为地震活动区域 推导了新方程。 之后,对欧洲和中东地区的所有记录进行了新处理。总共记录了532次强地震加速度图 ,记录了131次地震中距100 km的距离,矩 的震级范围从M 5到7.6,用于推导 都是水平分量的较大平均值和几何平均值。 发现预测与以前的欧洲方程中的 大致上一致,并且与初步 来自下一代衰减(NGA)项目的结果, 提出,来自 活动地壳区域(如果有)的地震动的系统差异足够大不能 防止来自南部 的强运动数据的组合使用,以及其他构造活跃的 浅地壳地震活动区。

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