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Undrained cyclic laboratory behavior of sandy soils

Articolo
Data di Pubblicazione:
2019
Abstract:
The complex cyclic shear stress path experienced by the soil during an earthquake, which could also induce liquefaction phenomena, can be approximated in the laboratory only by using sophisticated testing apparatuses. Cyclic triaxial tests have been widely used, especially for coarse grained soils, as in this study. In the framework of the design for the seismic retrofitting of the ''Ritiro viaduct'' foundations along the A20 motorway connecting Messina with Palermo (Italy), a soil liquefaction study was also carried out. With this aim, a detailed geological and geotechnical characterization of the area was performed by in situ and laboratory tests, including seismic dilatometer Marchetti tests (SDMTs), the combined resonant column (RCT) and cyclic loading torsional shear tests (CLTSTs), and undrained cyclic loading triaxial tests (CLTxTs). In particular, the paper presents the results of cyclic triaxial tests carried out on isotropically consolidated specimens of a sandy soil. The seismic retrofitting works include the reinforcement of the foundation and replacement of the decks with newly designed type and structural schemes, mixed steel, and concrete with continuous girder. During the investigation, data were acquired for the characterization of materials, for the definition of degradation phenomena with the relative identification of possible causes, and for the estimation of the residual performance characteristics of the building. The structural campaign of investigations necessary to determine all of the key parameters useful for a correct definition of the residual performance capabilities of the work was divided into two phases: One in situ and one in the laboratory.
Tipologia CRIS:
01.01 Articolo in rivista
Keywords:
Cyclic triaxial tests; In situ tests; Laboratory tests; Soil liquefaction
Elenco autori:
Cavallaro, ANTONIO MARIA FRANCESCO
Autori di Ateneo:
CAVALLARO ANTONIO MARIA FRANCESCO
Link alla scheda completa:
https://iris.cnr.it/handle/20.500.14243/364990
Pubblicato in:
GEOSCIENCES
Journal
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URL

https://www.mdpi.com/2076-3263/9/12/512
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