A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
This report describes in-plane experimental testing and numerical modelling of timberconcrete floor diaphragms. The experimental tests investigated the in-plane stiffness of the diaphragm and the stiffness and strength of different connections between the diaphragm and the lateral load resisting system. The test model was 1/3 scale and three meters square in plan. Seven tests with a different kind of connection between the floor and the rigid lateral supports (which simulated a timber lateral load resisting system) have been performed. The results of the experimental testing are used to calibrate numerical models which are used to investigate the effects of the floor flexibility on the seismic behaviour of post-tensioned timber buildings. For the experimental tests, screw and nail fasteners were used to connected to floor unit to the lateral supports. These fasteners were embedded into the concrete slab or timber edge joints at different orientations. The stiffness of the diaphragm connections was vastly different for each detail. Screws installed at a 45? angle (inclined) to the lateral supports were four times stiffer than the screws installed orthogonal to the lateral supports. The initial stiffness of the inclined fasteners was similar for timber-to-timber and concrete-to-timber connections. For the timberto- timber connections the orientation did not seem to influence the strength of the connection. The tested diaphragm had an uncracked stiffness of 4000 kN/mm and a cracked stiffness of 300 kN/mm. For the tested floor unit it was concluded that the influence of the diaphragm flexibility was negligible compared to the connector flexibility. The floor flexibility can be idealized as three different parts, the deformation of the connectors, the shear deformation of the diaphragm and the flexural deformation of the diaphragm. The numerical analyses showed that in most perceivable situations the connection deformation will govern the in-plane seismic response of the floor. Hence, it is justified to model it as a single-degree-of-freedom (SDOF) element. The influence of the floor flexibility on the seismic response of post-tensioned timber buildings is small. In most cases neglecting the floor flexibility is a conservative approach for the structural design of the building. However, structures with stiff walls and long floor spans there can be a significant amplification of the seismic response. For that case, a simple SDOF representation is proposed. Code-based recommendations for predicting the peak floor accelerations are found to be inadequate. A methodology is proposed to more accurately predict the expected peak floor accelerations for design
This paper presents site-specific and spatially-distributed ground-motion intensity estimates which have been utilized in the aftermath of the 2010-2011 Canterbury, New Zealand earthquakes. The methodology underpinning the ground motion intensity estimation makes use of both prediction models for ground motion intensity and its within-event spatial correlation. A key benefit of the methodology is that the estimated ground motion intensity at a given location is not a single value but a distribution of values. The distribution is comprised of both a mean and standard deviation, with the standard deviation being a function of the distance to nearby observations at strong motion stations. The methodology is illustrated for two applications. Firstly, maps of conditional peak ground acceleration (PGA) have been developed for the major events in the Canterbury earthquake sequence, which among other things, have been utilized for assessing liquefaction triggering susceptibility of land in residential areas. Secondly, the conditional distribution of response spectral ordinates is obtained at the location of the Canterbury Television building (CTV), which catastrophically collapsed in the 22 February 2011 earthquake. The conditional response spectra provide insight for the selection of ground motion records for use in forensic seismic response analyses of important structures at locations where direct recordings are absent.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of a workshop in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of an office in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.
A photograph of a resource room in the Department of Civil and Natural Resources Engineering at the University of Canterbury after the 4 September 2010 earthquake.