Post February 22 Earthquake Damage PWS-2011-03-09-DSC9932
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9949
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9921
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9924
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9923
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9952
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9942
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9950
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9938
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9940
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9929
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9927
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9935
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9956
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9941
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9948
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9944
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9934
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9922
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9953
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9955
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9931
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9928
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9954
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9947
Observations in major earthquakes have shown that rockable structures suffered less to no damage. During rocking, that is, partial and temporary footing separations, the influx of seismic energy is interrupted and thus the impact of the base excitation is reduced. Rocking causes the structure to deform more rigid like. Consequently, the structure experiences less deformation along the height and thus a lower damage potential. Although many researchers have studied the influence of rockable footings, most of these are either analytical or numerical, and only a very few structures have been built with rockable footings worldwide, for example, the chimney at Christchurch Airport and the South Rangitikei Viaduct in New Zealand. Despite these studies, a thorough and understanding is not yet available, especially with respect to experimental validations. This work is the first to investigate the rocking behaviour of bridges with different slenderness using large‐scale shake table experiments. To limit the number of influence factors, a stiff footing support and the same fixed‐base fundamental frequency of the bridges were assumed. The result shows that the girder displacement and the footing rotation of the tall bridge do not always move in phase, which cannot be observed in the short bridge. The results demonstrate the important role of slenderness in the overall responses of rockable bridges. This behaviour cannot be observed in bridges with a commonly assumed fixed base since the slenderness effect cannot be activated.
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9930
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9925
Post February 22 Earthquake Damage PWS-2011-03-09-DSC9951
Post February 22 Earthquake Damage Corner Opawa Road and Aynsley Terrace, Opawa PWS-2011-03-09-DSC9937