首页> 外文期刊>Georisk >Selection and quantification of near-fault velocity pulses owing to source directivity
【24h】

Selection and quantification of near-fault velocity pulses owing to source directivity

机译:源方向性导致的近断层速度脉冲的选择和量化

获取原文
获取原文并翻译 | 示例
       

摘要

Design ground motions are typically governed by large earthquakes at close distances, but the increasing number of near-field recordings manifest the large variability in near-source ground-motion amplitudes which result in significant differences in the building response. In the near-field, this variability arises mainly from source-directivity effects, which generate strong near-fault velocity pulses. We investigate the effect of source complexity on the generation of velocity pulses using a geometrical approach to quantify directivity at near-fault sites based on kinematic rupture models. We propose selection algorithms that can be implemented as search strategies for directivity-related strong ground motion records which may serve as ground motion selection tools in large databases for structural analysis and liquefaction studies. We find that the existence of directivity pulses is strongly related to slip heterogeneity on the fault plane, i.e. that the location and size of asperities (large slip areas) determine directivity pulse generation. In this context we quantify several pulse properties, testing a variety of approaches, and develop predictive relationships between a number of source parameters and pulse properties. We find strong dependence of pulse period on total area of asperities, as well as on a geometrical directivity parameter. The empirical observations on velocity pulse generation determined by the proposed selection procedure are compared with the predictions using the geometrical directivity model. The results are important for determining the probability of observing a pulse at a site as a function of magnitude, distance, and slip heterogeneity on the fault plane.
机译:设计地震动通常由近距离的大地震控制,但是近场记录数量的增加表明近源地震动振幅存在很大的变化,从而导致建筑物响应的显着差异。在近场中,这种可变性主要是由源方向性效应引起的,源性方向性效应会产生强大的近故障速度脉冲。我们使用几何学方法,基于运动学破裂模型,通过定量方法确定近断层位置的方向性,研究了源复杂度对速度脉冲产生的影响。我们提出了可以用作与方向性相关的强地面运动记录的搜索策略的选择算法,这些算法可以用作大型数据库中用于结构分析和液化研究的地面运动选择工具。我们发现方向性脉冲的存在与断层平面上的滑动非均质性密切相关,即凹凸不平的位置和大小(较大的滑动区域)决定了方向性脉冲的产生。在这种情况下,我们量化了几种脉冲特性,测试了各种方法,并开发了许多源参数和脉冲特性之间的预测关系。我们发现,脉冲周期对粗糙区域的总面积以及几何方向性参数的依赖性都很高。将通过拟议的选择程序确定的关于速度脉冲产生的经验观察与使用几何方向性模型的预测进行比较。这些结果对于确定在故障平面上观察到某个位置处的脉冲的概率,其大小,距离和滑动非均质性具有重要意义。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号