The earthquake of 26 September 1997 in Central Italy is one of the largest seismic events of the last 20 years in Italy. Two main events that caused significant damage in a large area of Umbria and Marche regions and site amplification phenomena were recorded even at large distances from the epicenter. After the emergency period, a detailed study of the surface effects was necessary for the post-earthquake reconstruction, but in a way it should be carried out rapidly enough to allow urban planners to give instructions and codes to public administrators. A team of surveyors were trained to collect field information such as geologic and geomorphologic features and, where possible, pre-existing geotechnic or geophysic information. Information was collected and analyzed with the aid of dynamic codes to calculate the possible local site effects. A one-dimensional code, analyzing single soil columns, Shake, as well as the two-dimensional codes working with finite or boundary elements, Quad4 and Besoil, were used and the results are presented as response spectra or amplification coefficients.

A correlation between slope failures and accelerometric parameters: the 26 september 1997 earthquake (Umbria-Marche, Italy)

PERGALANI, FLORIANA
2000-01-01

Abstract

The earthquake of 26 September 1997 in Central Italy is one of the largest seismic events of the last 20 years in Italy. Two main events that caused significant damage in a large area of Umbria and Marche regions and site amplification phenomena were recorded even at large distances from the epicenter. After the emergency period, a detailed study of the surface effects was necessary for the post-earthquake reconstruction, but in a way it should be carried out rapidly enough to allow urban planners to give instructions and codes to public administrators. A team of surveyors were trained to collect field information such as geologic and geomorphologic features and, where possible, pre-existing geotechnic or geophysic information. Information was collected and analyzed with the aid of dynamic codes to calculate the possible local site effects. A one-dimensional code, analyzing single soil columns, Shake, as well as the two-dimensional codes working with finite or boundary elements, Quad4 and Besoil, were used and the results are presented as response spectra or amplification coefficients.
2000
Umbria–Marche; Site effects; Earthquake
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11311/563304
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