0
  • DE
  • EN
  • FR
  • Base de données et galerie internationale d'ouvrages d'art et du génie civil

Publicité

Seismic Fragility Curves using Natural and Synthetic Ground Motions

 Seismic Fragility Curves using Natural and Synthetic Ground Motions
Auteur(s): , ,
Présenté pendant IABSE Symposium: Engineering the Future, Vancouver, Canada, 21-23 September 2017, publié dans , pp. 1274-1280
DOI: 10.2749/vancouver.2017.1274
Prix: € 25,00 incl. TVA pour document PDF  
AJOUTER AU PANIER
Télécharger l'aperçu (fichier PDF) 0.19 MB

Fragility curves are useful tools for the probabilistic assessment of the seismic performance of buildings. Nonlinear structural analyses with uncertainties in load and resistance are required to d...
Lire plus

Détails bibliographiques

Auteur(s): (National Institute of Technology Rourkela, Odisha, India)
(National Institute of Technology Rourkela, Odisha, India)
(Vel Tech Dr. RR & Dr. SR Technical University, Chennai, TN, India)
Médium: papier de conférence
Langue(s): anglais
Conférence: IABSE Symposium: Engineering the Future, Vancouver, Canada, 21-23 September 2017
Publié dans:
Page(s): 1274-1280 Nombre total de pages (du PDF): 7
Page(s): 1274-1280
Nombre total de pages (du PDF): 7
Année: 2017
DOI: 10.2749/vancouver.2017.1274
Abstrait:

Fragility curves are useful tools for the probabilistic assessment of the seismic performance of buildings. Nonlinear structural analyses with uncertainties in load and resistance are required to develop fragility curves. A statistically sufficient number of earthquake ground motion records should ideally be obtained from past records of the region of interest to have a satisfying fragility curve. However, the number of available earthquake records in many seismically active zones is limited. In such a situation, use of the synthetic ground motions is an accepted alternative for fragility analyses of buildings. This paper compares the seismic fragility curves obtained from synthetic and natural ground motion records. It is found that synthetic ground motions result in conservative fragility curves with lesser dispersion in drift demand when compared with natural recorded ground motions.