首页> 外文期刊>NRIAG Journal of Astronomy and Geophysics >Earthquake ground motion simulation at Zoser pyramid using the stochastic method: A step toward the preservation of an ancient Egyptian heritage
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Earthquake ground motion simulation at Zoser pyramid using the stochastic method: A step toward the preservation of an ancient Egyptian heritage

机译:使用随机方法模拟Zoser金字塔的地震地震动:迈向保存古埃及遗产的一步

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Strong ground shaking during earthquakes can greatly affect the ancient monuments and subsequently demolish the human heritage. On October 12th 1992, a moderate earthquake (Ms = 5.8) shocked the greater Cairo area causing widespread damages. Unfortunately, the focus of that earthquake is located about 14 km to the south of Zoser pyramid. After the earthquake, the Egyptian Supreme council of antiquities issued an alarm that Zoser pyramid is partially collapsed and international and national efforts are exerted to restore this important human heritage that was built about 4000 years ago. Engineering and geophysical work is thus needed for the restoration process. The definition of the strong motion parameters is one of the required studies since seismically active zone is recorded in its near vicinity. The present study adopted the stochastic method to determine the peak ground motion (acceleration, velocity and displacement) for the three largest earthquakes recorded in the Egypt’s seismological history. These earthquakes are Shedwan earthquake with magnitude Ms = 6.9, Aqaba earthquake with magnitude Mw = 7.2 and Cairo (Dahshour earthquake) with magnitude Ms = 5.8. The former two major earthquakes took place few hundred kilometers away. It is logic to have the predominant effects from the epicentral location of the Cairo earthquake; however, the authors wanted to test also the long period effects of the large distance earthquakes expected from the other two earthquakes under consideration. In addition, the dynamic site response was studied using the Horizontal to vertical spectral ratio (HVSR) technique. HVSR can provide information about the fundamental frequency successfully; however, the amplification estimation is not accepted. The result represented as either peak ground motion parameters or response spectra indicates that the effects from Cairo earthquake epicenter are the largest for all periods considered in the present study. The level of strong motion as indicated by peak ground acceleration reaches the value of 250 gals which is considerably high. At the end, it is worth to mention that the information resulted from the present work may be useful for the planned restoration decision of the Zoser pyramid site.
机译:地震期间强烈的地面震动会极大地影响古代遗迹,并随后破坏人类遗产。 1992年10月12日,中度地震(Ms = 5.8)震撼了开罗大区,造成了广泛的破坏。不幸的是,那场地震的焦点位于Zoser金字塔以南约14公里处。地震后,埃及最高古物理事会发出警报,称Zoser金字塔已部分倒塌,国际社会和国家为恢复这座建于4000年前的重要人类遗产做出了努力。因此,恢复过程需要进行工程和地球物理工作。定义强运动参数是必需的研究之一,因为地震活动带被记录在附近。本研究采用随机方法来确定埃及地震史上记录的三场最大地震的峰值地面运动(加速度,速度和位移)。这些地震是Ms = 6.9级的Shedwan地震,Mw = 7.2级的亚喀巴地震和Ms = 5.8级的开罗(达斯豪地震)。前两次大地震发生在几百公里之外。在开罗地震的震中位置产生主要影响是合乎逻辑的。但是,作者还想测试考虑中的其他两次地震带来的长距离地震的长期影响。此外,使用水平与垂直光谱之比(HVSR)技术研究了动态站点响应。 HVSR可以成功提供有关基频的信息;但是,不接受放大估计。以峰值地面运动参数或响应谱表示的结果表明,在本研究中考虑的所有时期,开罗地震震中的影响最大。峰值地面加速度表示的强运动水平达到250加仑,这是相当高的值。最后,值得一提的是,从当前工作中获得的信息可能对Zoser金字塔遗址的计划修复决定很有用。

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