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1D and 2D site amplification effects at Tarcento(Friuli, NE Italy), 30 years later

机译:30年后在Tarcento(意大利东北部弗留利)的一维和二维位点放大效应

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摘要

A temporary accelerometer network has been installed in Tarcento (Friuli, NE Italy), a small town heavily hit by the 1976–1977 Friuli earthquake sequence, as a part of an ongoing research\udproject aimed at ground motion simulation and generation of shakemaps in the near-field of an earthquake. The network operated from October 2008 to April 2010 and consisted of three\udK2 accelerographs with internal Episensor, distributed over a linear array of about 1.5 km length. Tarcento town had been chosen, at the end of the 1970s, as the ideal site for a pilot microzonation study, the first of this kind in Italy, in which a substantial number of field (and laboratory) tests were carried out in order to assess the mechanical properties of local alluvium deposits and their complex (3D) geometrical configuration. The data from the temporary network, illustrated herein, allow for proper verification and review of some of the quantitative predictions formulated in the 1980 study. As argued in the discussion section, we also believe that the data are apt to provide\udvaluable information of more general interest on the complex seismic response of alluvium-filled valleys, and we show therein how the observations can be interpreted in the light of presently available parametric simulation studies and simplified criteria for handling basin amplification effects.
机译:作为正在进行的研究\ udproject的一部分,该网络的一个临时加速度计网络已安装在Tarcento(意大利东北部的弗留利,内布拉斯加州,弗留利,1976-1977年的地震序列受重创)中,该项目旨在模拟地面运动并生成地震图。地震的近场。该网络于2008年10月至2010年4月运行,由三个带有内部Episensor的udK2加速度计组成,分布在大约1.5公里长的线性阵列上。 1970年代末,塔尔琴托镇被选为微区划试验研究的理想地点,这是意大利的第一个此类试验,在那里进行了大量的现场(和实验室)测试以评估局部冲积沉积物的力学性能及其复杂的(3D)几何构型。此处显示的来自临时网络的数据可以对1980年研究中制定的一些定量预测进行适当的验证和审查。如讨论部分所述,我们还认为该数据易于提供关于冲积谷的复杂地震响应的更有价值的有价值的信息,并且在其中展示了如何根据目前的观点来解释观测结果。现有的参数模拟研究和简化的标准来处理盆地放大效应。

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