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Key issues in Seismic Microzonation studies: lessons from recent experiences in Italy

机译:地震微微型研究的关键问题:意大利最近经验的课程

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The Seismic Microzonation (SM) is nowadays a world-wide accepted tool for the mitigation of seismic risk. Despite the large number of SM studies in the literature and the publication of national and international guidelines, some open questions still exist in SM studies and are addressed in this paper. These key issues are discussed after a brief history of SM in Italy and the presentation of Italian and international guidelines on the matter. The SM is a complex process involving different disciplines ranging from Geology and Applied Seismology to Structural and Geotechnical Engineering. The outcome of a SM is presented on a zoning map in terms of ground shaking intensity and susceptibility to main ground instability (soil liquefaction, landslides, fault ruptures). In an advanced SM study for a given area, four main interdisciplinary steps can be recognized: 1) definition of the reference input motions, 2) construction of the subsoil model, 3) performing of numerical analyses, 4) identification of zones with different geotechnical hazard potential and drawing up of the SM map. The key issues and the controversial aspects of these steps are deeply discussed in the paper based on the experience of the Author gained in three recent Italian case studies: Middle Aterno valley, Central Archaeological Area of Rome and Fivizzano. Earthquake-induced permanent soil deformations are out of the scope of the paper being the attention focused on soil amplification phenomena. The paper closes with some remarks on the differences between local seismic hazard assessment for SM mapping and for the seismic design (according to the Italian building code NTC08), and with some proposals on the use of SM output in supporting design.
机译:如今,地震微微突变(SM)是一种全球可接受的抗震风险的接受工具。尽管文献中有大量的SM研究以及国家和国际指南的出版物,但SM研究中仍存在一些开放性问题,并在本文中解决。在意大利的SM简史和关于此事方面的介绍之后讨论了这些关键问题。 SM是一种复杂的过程,包括从地质和应用地震学到结构和岩土工程的不同学科。在地面摇动强度和易感性易稳定性(土壤液化,山体滑坡,故障破裂)方面,SM的结果在分区图上呈现。在给定区域的高级SM研究中,可以识别出四个主要跨学科步骤:1)参考输入运动的定义,2)构建底层模型,3)进行数值分析,4)识别不同的岩土危险潜力和绘制SM地图。本文根据三个意大利案例研究中获得的作者的经验深入讨论了这些步骤的关键问题和争议方面:罗马和费范州中央考古区的艾尔纳河谷。地震诱导的永久性土壤变形是本文的范围,即重点关注土壤扩增现象。本文结束了一些关于SM映射和地震设计的当地地震危害评估的差异(根据意大利建筑码NTC08)的差异,以及一些关于使用SM输出在支持设计中的建议。

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