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Re-evaluation of code-specified stratigraphic amplification factors based on Italian experimental records and numerical seismic response analyses

机译:根据意大利的实验记录和数值地震响应分析,对规范规定的地层放大因子进行重新评估

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For several engineering and seismological applications, site effects can be synthetically evaluated as a soil amplification factor of the reference ground motion on a rock outcrop leading to the peak ground acceleration and/or the response spectrum expected at a soil site, classified according to its equivalent shear wave velocity, V-s,V-30. In this work, nonlinear stratigraphic amplification factors as specified by Eurocode 8 (EC-8) and National Technical Code (NTC) were assessed with reference to selected accelerometric records of the Italian seismic network and well-characterized recording stations classified according to V-s,V-3o. A first set of 'empirical' amplification factors has been identified, by selecting those stations on deformable soil for which records of the same events exist also at a nearby reference station located on outcropping rock (4 sites, 102 records). A second set of 'semi-empirical' data has been obtained by analysing the accelerograms recorded at stations where the geotechnical characterization was comprehensive and the reference motion could be back-figured by de-convolution to the bedrock (7 sites, 50 records). A third set of 'analytical' data was obtained from ID numerical simulations of seismic site response performed on virtual stratigraphic profiles, consistent with the ground classification adopted by EC-8 and NTC, and subjected to 80 acceleration time histories of 22 Italian earthquakes, recorded at 19 stations of the Italian Network classified as rock sites. Empirical, semi-empirical and analytical data have been therefore integrated to express the stratigraphic amplification factor of peak ground acceleration and spectral intensity as a function of the corresponding reference ground motion value for each class of subsoil.
机译:对于一些工程和地震学应用,可以将场地效应综合评估为岩石露头上参考地面运动的土壤放大因子,从而导致峰值加速度和/或在土壤场所预期的响应谱,并根据其等效项进行分类横波速度,Vs,V-30。在这项工作中,参照意大利地震台网的选定加速度测量记录和根据Vs,V分类的性能良好的记录站,评估了欧洲规范8(EC-8)和国家技术规范(NTC)规定的非线性地层放大因子。 -3o。通过选择在可变形土壤上那些同样事件记录也存在于露头岩石附近参考站上的站,已经确定了第一组“经验”放大因子(4个站点,102条记录)。通过分析在岩土特征全面的站点记录的加速度图获得第二组“半经验”数据,并且可以通过反褶积到基岩将参考运动反绘(7个站点,50条记录)。从在虚拟地层剖面上进行的地震现场响应的ID数值模拟中获得第三组“分析”数据,这与EC-8和NTC所采用的地面分类一致,并且经历了22次意大利地震的80个加速时间历史记录在意大利网络的19个被分类为岩点的站点。因此,已整合了经验,半经验和分析数据,以表示地面加速度峰值和频谱强度的地层放大因子,作为每种地下土壤的相应参考地面运动值的函数。

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