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Improving the Italian strong ground motion attenuation relationship: preliminary results with an updated accelerometric data set

机译:改善意大利强大的地面运动衰减关系:初步结果和更新的加速度数据集

摘要

Strong ground motion attenuation relationships are fundamental tools for seismic hazardevaluation. In Italy the most widely used attenuation relationship is the Sabetta andPugliese (1987 and 1996, here afters referred to as SP96) for evaluating peak groundacceleration, peak ground velocity, Arias intensity and pseudovelocity response spectra,of the Italian territory. The equation has been derived using 95 records relative to17 earthquakes with magnitude ranging from 4.6 to 6.8. The SP96 relation is basedon the strongest events since the installation of accelerometric instruments in Italy,dated 1972, such as Friuli 1976, Valnerina 1979, Irpinia 1980, and Lazio-Abruzzo1984, which is the most recent event. In the time span 1984 – 2007 other moderateseismic events occurred in Italy, namely the East Sicily 1991, Umbria-Marche 1997-1998, Pollino 1998 and Molise 2002, with moment magnitude > 5, and huge datasets have been obtained due to the installation of many temporary stations and digitalinstruments. The Umbria-Marche and Molise accelerometric data sets allowed the calculationof regional attenuation relationships that show a considerably different trendcompared to the SP96. In this time span a project for an updated Italian accelerometricdata base construction has been started with the aim of collecting all the accelerationtime histories recorded since 1972 and re-evaluating, updating and improving eventparameters, data processing and station geological/geotechnical characteristics.The aim of this research is the implementation of a new weighted regression analysis with the expanded and updated database, including coefficients to model themagnitude-dependent decay rate, the faulting mechanism, the local site effects andthe magnitude-dependent variance. In addition, the fit of the SP96 equation to the newaccelerometric data set spanning from 1972 to 2004 is evaluated with the aid of differentstatistic techniques, in order to verify the need of deriving a new attenuationequation.
机译:强大的地震动衰减关系是地震危险性评估的基本工具。在意大利,最广泛使用的衰减关系是Sabetta andPugliese(1987和1996,以下简称SP96),用于评估意大利领土的峰值地面加速度,峰值地面速度,Arias强度和拟速度响应谱。该方程是使用95条记录(相对于17次地震,范围为4.6至6.8)推导出来的。 SP96关系基于自1972年在意大利安装加速度测量仪器以来最强劲的事件,例如最近的事件,例如Friuli 1976,Valnerina 1979,Irpinia 1980和Lazio-Abruzzo1984。在1984年至2007年这段时间里,意大利发生了其他中等地震事件,即东西西里1991年,翁布里亚-马尔什1997-1998年,波利诺1998年和莫利塞2002年,矩震级大于5,并且由于安装了大地震数据集许多临时电台和数字仪器。 Umbria-Marche和Molise加速度计数据集可以计算区域衰减关系,与SP96相比,该区域的变化趋势明显不同。在这段时间里,已经开始了一个更新意大利加速度计数据库建设的项目,目的是收集自1972年以来记录的所有加速时间历史记录,并重新评估,更新和改进事件参数,数据处理和台站地质/地质技术特征。这项研究是通过扩展和更新的数据库实施新的加权回归分析,其中包括建模与幅度相关的衰减率,断层机制,局部场地效应和与幅度相关的方差的系数。此外,借助于不同的统计技术,对SP96方程与1972年至2004年之间的新加速度数据集的拟合度进行了评估,以验证是否需要推导新的衰减方程。

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