Site response studies and seismic microzoning in the Middle Aterno valley (L'aquila, Central Italy)

被引:66
作者
Lanzo, G. [1 ]
Silvestri, F. [2 ]
Costanzo, A. [3 ]
d'Onofrio, A. [2 ]
Martelli, L. [4 ]
Pagliaroli, A. [6 ]
Sica, S. [5 ]
Simonelli, A. [5 ]
机构
[1] Univ Roma La Sapienza, Dipartimento Ingn Strutturale & Geotecn, Rome, Italy
[2] Univ Naples Federico 2, Dipartimento Ingn Idraul Geotecn & Ambientale, Naples, Italy
[3] Univ Calabria, Dipartimento Difesa Suolo, I-87036 Arcavacata Di Rende, Italy
[4] Serv Geol Sism & Suoli, Bologna, Italy
[5] Univ Sannio, Dipartimento Ingn, Benevento, Italy
[6] CNR IGAG, Rome, Italy
关键词
Aterno River valley; Soil amplification; Dynamic properties; Numerical analyses; Microzonation maps;
D O I
10.1007/s10518-011-9278-y
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Following the April 6th, 2009 Abruzzo mainshock, the Italian Civil Protection Department promoted a multidisciplinary study aimed at developing seismic microzonation maps for post-earthquake reconstruction planning. In the framework of this project, a Working Group, including the authors, was assembled to carry out a microzonation study on six villages located in the Middle Aterno valley. This paper focuses on the villages of Castelnuovo and Poggio Picenze, which experienced MCS intensity values of IX-X and VIII-IX, respectively. 1D and 2D linear equivalent site response analyses were carried out on representative geological cross-sections through the damaged centres and the expansion zones. The subsoil models resulting from geological, geotechnical and geophysical investigations were calibrated by comparing numerical amplification functions, in the linear range, with horizontal-to-vertical spectral ratio derived from both aftershocks and noise recordings. The input motions adopted for the analyses were five artificial accelerograms compatible with three response spectra obtained from the Italian seismic code, as well as from ad hoc probabilistic and deterministic studies. The results were expressed in the form of horizontal profiles of amplification factors in terms of peak ground acceleration, F(PGA), as well as of the Housner intensity, FH, in two different range of periods; this latter parameter was shown to be almost independent of the input motion and allowed to express the dependency of site amplification on the frequency range. The amplification factors computed along the representative geological sections were finally extended with a rational procedure to the surrounding areas to draw Grade-3 microzonation maps.
引用
收藏
页码:1417 / 1442
页数:26
相关论文
共 28 条
[1]  
[Anonymous], 2004, SESAME European research project, Deliverable D23. 12., Project No. EVG1-CT-2000-00026
[2]  
Anti Dan L.Q., 2001, ADV LAB STRESS STRAI, P187
[3]  
Bardet J.P., 2000, EERA COMPUTER PROGRA
[4]  
BILOTTA E, 2011, P 5 ICEGE SANT
[5]  
Bosi C., 1970, Memorie della Societa Geologica Italiana, V9, P719
[6]  
COSTANZO A, 2007, THESIS U CALABRIA
[7]  
COSTANZO A, 2007, P 4 ICEGE THESS
[8]  
d'Onofrio A., 2010, P SUST DEV STRAT CON
[9]  
Di Capua G., 2009, RAPPORTO PROGETTO S4, P28
[10]  
Galli P., 2009, Report on the Effects of the Aquilano Earthquake of 6 April 2009, Quick Earthquake Survey Team-Final Report