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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的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 I 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,但是与估计峰值地面加速度和响应谱纵坐标的大量方程相比,该参数的预测方程相对较少。 PGV经验公式的缺乏导致了在5%衰减的响应光谱纵坐标上以1 sec缩放峰速度的实践的广泛使用,这无法直接预测参数。为提供预测PGV的方程式的需要,本文对所有记录进行了新的处理,然后使用强运动数据库推导了欧洲和中东地震活跃地区的新方程式。在131个地震的最大100 km距离处记录的532个强运动加速度图,矩量级在M 5到7.6之间,用于导出水平分量的较大平均值和几何平均值的方程。发现这些预测与先前的欧洲方程式的预测基本一致,也与下一代衰减(NGA)项目的初步结果相一致,这表明活动地壳区域(如果有的话)的地震动的系统差异足够小而不是以防止合并使用来自南欧,北美洲西部和其他浅地壳地震活动的构造活跃地区的强运动数据。

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