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THE DEVELOPING OF GROUND RESPONSE SPECTRA FOR EXTREME SEISMIC EVENTS IN SOUTHERN FINLAND

机译:南部芬兰极端地震事件地面响应谱的发展

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The purpose of the current paper is to present the task, the methods and the results for the ground response spectra for nuclear construction sites in southern Finland. The results of this study will form a key design in formation for the design of the plant structures, piping and equipment. The first task of the study was the development of attenuation relationships for southern Finland. For this task the approach of tektonically and geologically similar regions was adopted. For these regions the Saguenay region and the southwestern Australia were chosen. The second task in the study was the division of the southern Finland to six source areas and the determination of magnitude recurrence relationships for these source areas. The identified sources for the study were: 1) Swedish coast, 2) Aland archipelago-Estonian coast strip, 3) Bothnian gulf-lake Ladoga strip, 4) the bottom of Bothnian gulf- White sea strip, 5) Riga bay - Latvia area, 6) background seismicity. The third task of the study was the seismic hazard determination of the investigated area it was done for the different frequencies. The frequency band investigated covered frequencies from 0.5Hz up to 50Hz and the number frequency points were about 10. The conclusion of the study is that ground response in southern Finlands low seismicity precambrian rocks is from 0.1- 0.15g for zero period acceleration and that the spectral shapes of the obtained spectra are quite flat, amplification factors being less than three and the spectral peaks are located at frequencies higher than 10Hz.
机译:本文的目的是介绍芬兰南部核建筑工地的地面响应谱的任务,方法和结果。这项研究的结果将构成工厂结构,管道和设备设计中的关键设计。这项研究的首要任务是发展芬兰南部的衰减关系。对于此任务,采用了在构造和地质上相似的地区的方法。对于这些地区,选择了萨格奈地区和澳大利亚西南部。该研究的第二项任务是将芬兰南部划分为六个源区,并确定这些源区的震级重复关系。确定的研究来源是:1)瑞典海岸,2)阿兰群岛-爱沙尼亚海岸带,3)博恩尼湾-拉多加湖带,4)博恩尼湾的底部-白海带,5)里加湾-拉脱维亚地区,6)背景抗震性。这项研究的第三项任务是确定被调查区域在不同频率下的地震危害。研究的频带覆盖了从0.5Hz到50Hz的频率,并且频率点数约为10个。研究结论是,芬兰南部低地震活动前寒武纪岩石在零周期加速度下的地面响应为0.1-0.15g,并且所获得频谱的频谱形状非常平坦,放大因子小于3,并且频谱峰值位于高于10Hz的频率处。

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