Integrated subsoil model for seismic microzonation in the Central Archaeological Area of Rome (Italy)

被引:0
|
作者
Massimiliano, Moscatelli [1 ]
Alessandro, Pagliaroli [1 ]
Marco, Mancini [1 ]
Francesco, Stigliano [1 ]
Giuseppe, Cavuoto [1 ]
Maurizio, Simionato [1 ]
Edoardo, Peronace [1 ]
Bruno, Quadrio [1 ]
Paolo, Tommasi [1 ]
Paolo, Cavinato Gian [1 ]
Vincenzo, Di Fiore [2 ]
Antimo, Angelino [2 ]
Giuseppe, Lanzo [3 ]
Salvatore, Piro [4 ]
Daniela, Zamuner [4 ]
Emiliano, Di Luzio [4 ]
Sabatino, Piscitelli [5 ]
Alessandro, Giocoli [5 ]
Angela, Perrone [5 ]
Enzo, Rizzo [5 ]
Gerardo, Romano [5 ]
Giuseppe, Naso [6 ]
Sergio, Castenetto [6 ]
Angelo, Corazza [6 ]
Sandro, Marcucci [6 ]
Roberto, Cecchi [7 ]
Pia, Petrangeli [7 ]
机构
[1] CNR IGAG, Ist Geol Ambientale & Geoingn, Area Ric Roma 1, I-00015 Monterotondo, RM, Italy
[2] CNR IAMC, Ist Ambiente Marino & Costiero, I-80133 Naples, Italy
[3] Univ Roma La Sapienza, DISG, I-00197 Rome, Italy
[4] CNR ITABC, Ist Tecnol Applicate Beni Culturali, Area Ric Roma 1, I-00015 Monterotondo, RM, Italy
[5] CNR IMAA, Ist Metodol Anal Ambientale, I-85050 Tito, PZ, Italy
[6] DPC, I-00189 Rome, Italy
[7] MiBAC, I-00186 Rome, Italy
来源
DISASTER ADVANCES | 2012年 / 5卷 / 03期
关键词
Integrated subsoil model; seismic microzonation; archaeological area; Palatine hill; Rome;
D O I
暂无
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
An integrated subsoil model for seismic microzonation in the Central Archaeological Area of Rome is presented in this study. This model was created in the framework of a research project aimed at evaluating the geohazard level affecting Palatine hill, Roman Forum and Coliseum. A multidisciplinary survey was carried out mainly in 2010 including continuous-coring boreholes, in situ and laboratory geotechnical tests, MASW, Cross and Down-Hole tests, ambient noise measurements, Electrical Resistivity Tomographies, Ground Penetrating Radar surveys. The surveying methodologies adopted in the surveying campaign are also presented here. A three step procedure adopted for creating the integrated subsoil model of Palatine hill and surrounding areas is described in detail. This procedure first involves the construction of a geological model starting mainly from boreholes' data interpretation and correlation. Geological formations are here interpreted in terms of lithofacies following their sedimentological features and then characterized by means of their main physical properties (i.e. grain size distribution, void ratio, unit weight, plasticity index) to define a scheme of lithotypes. The lithotypes represent the "framework" to be characterized in terms of dynamical properties to produce the final inputs for 1D and 2D numerical modeling of ground motion amplification effects aimed at the construction of seismic microzonation maps.
引用
收藏
页码:109 / 124
页数:16
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