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首页> 外文期刊>European journal of environmental & engineering geophysics >Influence of geometrical and geophysical parameters on the seismic site amplification factor
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Influence of geometrical and geophysical parameters on the seismic site amplification factor

机译:几何和地球物理参数对地震现场放大因子的影响

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An evaluation of the intrinsic limits of 1D modelling for estimation of the site seismic response (DAF, Dynamic Amplification Factor) in the case a non-horizontal basement is presented and discussed. 1D models are still commonly used in engineering practice. Therefore it is important to understand the limits of the 1D modelling in order to simplify the problem without dangerous errors when evaluating the seismic response. Up-to-date and robust visco-elastic non-linear 1D and 2D algorithms were used. The reference accelerogram is relative to an Umbria earthquake (Colfiorito - Italy, 26/09/97, M = 5.6), recorded at the Department of Geophysics and Volcanology, University of Naples Federico II. The results indicate that in the case of a dipping bedrock, if the angle is less than 10 deg and the S-wave velocity contrast within the overburden is included between 1 - 0.5, the evaluation of the site response given by both the algorithms is similar. For dip values exceeding 10 deg, the DAF spectra start to diverge, both in terms of amplitude and peak periods. If the S-wave velocity contrast is less than 0.5 the 1D and 2D DAF spectra are substantially different even if the bedrock is horizontal and this is due to the different methods of DAF calculation used by the two algorithms. The results obtained with theoretical models were confirmed by comparing the 1D and the 2D response in two test sites characterised by a dipping volcanic tuff basement, in the city of Naples. The response of the 1D model in such geological conditions is inaccurate. Therefore the use of 1D algorithms for DAF evaluation during seismic site planning should be restricted to those sites having geophysical and geometrical properties compatible with those illustrated in the results.
机译:在非水平地下室的情况下,对一维建模的固有极限进行了评估,以估算现场地震响应(DAF,动态放大因子)。一维模型仍然是工程实践中常用的模型。因此,重要的是要了解一维建模的局限性,以便在评估地震响应时简化问题而无危险错误。使用了最新且鲁棒的粘弹性非线性一维和二维算法。参考加速度图是与那不勒斯费德里科二世大学地球物理与火山学系记录的翁布里亚地震(意大利科菲奥里托,97年9月26日,M = 5.6)有关的。结果表明,在倾覆基岩的情况下,如果角度小于10度,并且覆盖层内的S波速度反差介于1-0.5之间,则两种算法给出的位置响应评估相似。对于超过10度的倾角值,DAF谱在振幅和峰值周期方面都开始发散。如果S波速度对比值小于0.5,则即使基岩是水平的,一维和二维DAF光谱也将显着不同,这是由于两种算法使用的DAF计算方法不同。通过理论模型获得的结果通过在那不勒斯市两个以火山凝灰岩基底为特征的测试地点比较一维和二维响应而得到证实。一维模型在这种地质条件下的响应是不准确的。因此,应将一维算法用于地震现场规划期间的DAF评估,应仅限于具有与结果中说明的地球物理和几何属性兼容的那些现场。

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