首页> 外文期刊>Geomatics,Natural Hazards & Risk >Validation of strong-motion stochastic model using observed ground motion records in north-east India
【24h】

Validation of strong-motion stochastic model using observed ground motion records in north-east India

机译:利用印度东北部观测到的地面运动记录验证强运动随机模型

获取原文
           

摘要

We focused on validation of applicability of semi-empirical technique (spectral models and stochastic simulation) for the estimation of ground-motion characteristics in the northeastern region (NER) of India. In the present study, it is assumed that the point source approximation in far field is valid. The one-dimensional stochastic point source seismological model of Boore (1983) (Boore, DM. 1983. Stochastic simulation of high frequency ground motions based on seismological models of the radiated spectra. Bulletin of Seismological Society of America, 73, 1865?¢????1894.) is used for modelling the acceleration time histories. Total ground-motion records of 30 earthquakes of magnitudes lying between M W 4.2 and 6.2 in NER India from March 2008 to April 2013 are used for this study. We considered peak ground acceleration (PGA) and pseudospectral acceleration (response spectrum amplitudes) with 5% damping ratio at three fundamental natural periods, namely: 0.3, 1.0, and 3.0 s. The spectral models, which work well for PGA, overestimate the pseudospectral acceleration. It seems that there is a strong influence of local site amplification and crustal attenuation (kappa), which control spectral amplitudes at different frequencies. The results would allow analysing regional peculiarities of ground-motion excitation and propagation and updating seismic hazard assessment, both the probabilistic and deterministic approaches.
机译:我们专注于验证半经验技术(谱模型和随机模拟)在印度东北地区(NER)地面运动特征估计中的适用性。在本研究中,假设远场中的点源近似是有效的。 Boore(1983)(Boore,DM。1983.基于辐射光谱地震模型的高频地震动的随机模拟)一维随机点源地震模型,《美国地震学会通报》,73,1865年。 1894.)用于对加速时间历史进行建模。这项研究使用了2008年3月至2013年4月在印度东北部发生的M W 4.2和6.2之间的30次地震的总地面运动记录。我们考虑了在三个基本自然周期(即0.3、1.0和3.0 s)具有5%阻尼比的峰值地面加速度(PGA)和伪频谱加速度(响应频谱幅度)。适用于PGA的光谱模型高估了伪光谱加速度。似乎对局部放大和地壳衰减(kappa)有很大的影响,它们会控制不同频率下的频谱幅度。结果将有助于分析地震动激发和传播的区域特性,并更新概率和确定性方法的地震危险性评估。

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