The dynamic response of long structures (e.g., bridges) is sensitive to the spatial variability of strong ground motion (asynchronous motion). Ground motion differences increase from point to point with increasing foundation distance. This latter is due to two physical phenomena: soil-wave interaction, that causes the loss of coherence and local amplification; wave traveling with finite velocity, that causes signals time lag. This ground motion variability produces a different structural demand compared to the synchronous one, which is the only one considered by designers in the majority of cases. A few codes consider this type of actions, therefore further research efforts are necessary. In this study, asynchronous ground motions are gener...
Eurocode 8, part 2, presents various methods to incorporate asynchronous seismic excitation for brid...
This paper examines the impact of stochastic spatial variability of seismic ground motion on the sei...
Assessment of the local variability of the ground motion due to local lateral heterogeneities and to...
The dynamic response of long structures (e.g., bridges) is sensitive to the spatial variability of s...
The seismic actions used to design long structures, as bridges, should be attentively evaluated, sin...
The seismic motion is characterized by temporal and spatial variability, that become significant in ...
Nonstationary earthquakes are very complex ground motions and they vibrate structural systems in as...
It is recognized that the spatial variability of the ground motion has an important effect on the se...
Based on observed damage patterns from previous earthquakes and a rich history of analytical studies...
The seismic signals, recorded at different surface points during the propagation of the seismic wave...
During strong ground motion, it is expected that bridge structures are subjected to excitation that ...
During strong ground motion, it is expected that bridge structures are subjected to excitation that ...
The spatial variability of the earthquake strong ground motion (SVEGM) leads to significant aspects ...
The spatial variability of the earthquake strong ground motion (SVEGM) leads to significant aspects ...
Frequently long-span bridges provide deep valley crossings, which require special consideration due ...
Eurocode 8, part 2, presents various methods to incorporate asynchronous seismic excitation for brid...
This paper examines the impact of stochastic spatial variability of seismic ground motion on the sei...
Assessment of the local variability of the ground motion due to local lateral heterogeneities and to...
The dynamic response of long structures (e.g., bridges) is sensitive to the spatial variability of s...
The seismic actions used to design long structures, as bridges, should be attentively evaluated, sin...
The seismic motion is characterized by temporal and spatial variability, that become significant in ...
Nonstationary earthquakes are very complex ground motions and they vibrate structural systems in as...
It is recognized that the spatial variability of the ground motion has an important effect on the se...
Based on observed damage patterns from previous earthquakes and a rich history of analytical studies...
The seismic signals, recorded at different surface points during the propagation of the seismic wave...
During strong ground motion, it is expected that bridge structures are subjected to excitation that ...
During strong ground motion, it is expected that bridge structures are subjected to excitation that ...
The spatial variability of the earthquake strong ground motion (SVEGM) leads to significant aspects ...
The spatial variability of the earthquake strong ground motion (SVEGM) leads to significant aspects ...
Frequently long-span bridges provide deep valley crossings, which require special consideration due ...
Eurocode 8, part 2, presents various methods to incorporate asynchronous seismic excitation for brid...
This paper examines the impact of stochastic spatial variability of seismic ground motion on the sei...
Assessment of the local variability of the ground motion due to local lateral heterogeneities and to...