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Assessment of predominant frequencies using ambient vibration in the Kachchh region of western India: implications for earthquake hazards

机译:利用印度西部卡奇地区的环境振动评估主要频率:对地震危害的影响

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The Kachchh region is the second most seismically active region in India after the Himalaya. One of the disastrous Indian earthquakes of the millennium was the Bhuj earthquake of January 26, 2001, which caused about 14,000 casualties and huge property damage. The main reason for such devastation is due to lack of earthquake awareness and poor construction practices. Hence, an increase in the knowledge and awareness, based on improved seismic hazard assessment, is required to mitigate damage due to an earthquake. Natural predominant ground frequencies have been investigated in the Kachchh region of western India using ambient vibrations. The horizontal-to-vertical spectral ratio technique has been applied to estimate the predominant frequency at 126 sites. The ambient vibration measurements were conducted for about 1 h at each site in the continuous mode recording at 100 samples/s. We have validated the estimated predominant frequency with earthquake data recorded at six broadband stations in the region. It has been observed that geological time period has a significant effect on predominant frequency of the ground. The estimated predominant frequencies vary from 0.24 to 2.25 Hz for the Quaternary, 0.41-2.34 Hz for the Tertiary, 0.32-4.91 Hz for the Cretaceous, and 0.39-8.0 Hz for the Jurassic/Mesozoic. In the Deccan trap, it varies from 1.30 to 3.80 Hz. We found distinct variation of predominant frequencies of sites associated with hard rock and soft soil. The predominant frequencies were related to the thickness of the sediments, which are deduced by other geophysical and geological methods in the region. Our results suggest that frequencies of the region reveals the site characteristics that can be considered for studying the seismic risks to evolve a plan for disaster risk mitigation for the region
机译:Kachchh地区是仅次于喜马拉雅山的印度第二大地震活跃地区。 2001年1月26日的布杰地震是印度在本世纪造成的灾难性地震之一,造成约14,000人伤亡和巨大的财产损失。造成这种破坏的主要原因是由于缺乏地震意识和不良的施工惯例。因此,需要基于改进的地震危险性评估来增加知识和意识,以减轻由于地震造成的破坏。在印度西部的Kachchh地区,利用环境振动对自然主导的地面频率进行了研究。水平对垂直频谱比率技术已应用于估算126个站点的主要频率。在连续模式下以100个样本/秒的速度在每个位置进行大约1小时的环境振动测量。我们已使用该地区六个宽带站记录的地震数据验证了估计的主要频率。已经观察到,地质时间段对地面的主要​​频率具有显着影响。估计的主要频率在第四纪为0.24至2.25 Hz,第三纪为0.41-2.34 Hz,白垩纪为0.32-4.91 Hz,侏罗纪/中生代为0.39-8.0 Hz。在Deccan陷波器中,它的变化范围是1.30至3.80 Hz。我们发现与硬岩和软土有关的站点的主要频率有明显的变化。主要频率与沉积物的厚度有关,沉积物的厚度由该地区的其他地球物理和地质方法推论得出。我们的结果表明,该区域的频率揭示了可用于研究地震风险以制定该区域减灾计划的站点特征

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