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Discussion of the paper 'An empirical attenuation relationship for Northwestern Turkey ground motion using a random effects approach'

机译:讨论论文“使用随机效应方法对土耳其西北部地面运动的经验衰减关系”

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摘要

Ozbey et al. [1] have worked out a new attenuation relationship applicable to northwestern Turkey based on recent ground motion data recorded during the 1999 Turkey earthquakes and a few of their following events. Because of our own work along similar lines we believe the evolution of ground motion predictions for the same or similar regions is of interest even though our own models are intended to be applicable to the whole of Turkey. Ground motion predictions based on records made in Turkey are affected by two influences. One is the relative uncertainty that shrouds the local site character. A good many sites do not have borehole or other data to establish their local site descriptor. The other is the interference from the buildings where the sensor may have been placed. In spite of these shortcomings, we have utilized available data from 47 stations that recorded 93 horizontal components during 19 distinct events to report prediction expressions in [2]. We have now updated this study by considering 57 earthquakes during 1976-2003 containing 112 records with 223 horizontal acceleration time series, to be reported in [3]. In 1999, Kocaeli earthquake data comprises 46 and 35% of our database assembled in [2,3], respectively.
机译:Ozbey等。 [1]根据最近在1999年土耳其地震中记录的地面运动数据及其随后的一些事件,得出了适用于土耳其西北部的新衰减关系。由于我们的工作类似,因此我们相信对相同或相似区域的地面运动预测的发展很有意义,即使我们自己的模型打算适用于整个土耳其。基于土耳其的记录进行的地面运动预测受到两个方面的影响。一是笼罩当地特色的相对不确定性。很多站点没有钻孔或其他数据来建立其本地站点描述符。另一个是来自可能已放置传感器的建筑物的干扰。尽管存在这些缺点,我们还是利用了来自47个台站的可用数据,这些台站在19个不同事件中记录了93个水平分量,以报告[2]中的预测表达式。现在,我们通过考虑1976-2003年间的57次地震来更新此研究,该地震包含112条记录和223个水平加速度时间序列,将在[3]中进行报告。在1999年,科贾埃利地震数据分别占我们在[2,3]中汇编的数据库的46%和35%。

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