The banks of the Avon River along Avonside Drive have been built up with gravel. In the distance, portaloos and road cones can be seen.
Cars slow for road works on Lineside Road, outside Kaiapoi, near the intersection with Revells Road. A truck is dumping gravel to fill cracks in the road surface.
Photograph captioned by BeckerFraserPhotos, "Gough House, 90 Hereford Street. The gravel spread in front of this building is a signal it will shortly be demolished".
A road roller parked on the side of Banks Avenue. The street is under repair and has a gravel surface. The photographer comments, "Road works in Banks Avenue".
Liquefaction silt which has been partly cleared from in front of businesses on Ferry Road. A damaged part of the footpath has also been filled in with gravel.
A pile of gravel in Avonside used to fill up the gaps created by seismic activity and liquefaction. The cracks in this curb side have not been filled yet.
A pile of gravel and tarseal in front of a house in Richmond during repairs to River Road. The photographer comments, "Our house was becoming progressively more shattered with each aftershock".
The banks of the Avon River along Avonside Drive have been built up with gravel. The street is flooded, and has been closed off with fencing and road cones.
The banks of the Avon River along Avonside Drive have been built up with gravel. The street is flooded, and has been closed off with fencing and road cones.
A pile of gravel and tarseal in front of a house in Richmond. The photographer comments, "River Rd repairs. We weren't living in our house, we'd moved out after the September 2010 shake".
Damage to Avonside Drive. The street is closed off with cones and a "Road closed" sign, and portaloos line the street. The banks of the Avon River have been built up with gravel.
A gravel walkway in the process of being paved next to the Avon River. On the side are piles of dirt that has been dug up to make way for the walkway.
A gravel walkway in the process of being paved next to the Avon River. On the side are piles of dirt that has been dug up to make way for the walkway.
A portaloo sits outside a house on River Road. The road is under repair, and the tarmac has been removed leaving a gravel surface. The photographer comments, "Our old house was given a portaloo; I'm not sure why".
Liquefaction and flooding on Avonside Drive. The street is closed off with cones and a "Road closed" sign, and portaloos line the street. The banks of the Avon River have been built up with gravel.
A view of Colombo Street, looking north from Kilmore Street. Many of the buildings on the left side have been demolished, and on the right they are badly damaged. Piles of gravel have been heaped on the side of the road.
The sunken footpath around the base of a power pole on Bracken Street in Avonside. Dry silt from liquefaction can be seen mixed in with the gravel around it as a result of the 4 September 2010 earthquake.
A gutter on Bracken Street in Avonside showing cracks from the 4 September 2010 earthquake. The edges of the footpath above it have fallen away, and the gutter has filled with the loose gravel which was used to fill pot holes in the road.
The laying of new sewers in Bridge Street, South Brighton. Road cones have been placed along the road works. Temporary road signs indicate that the current speed limit is 30 km/h. Diggers, four-wheel drive vehicles and a truck are parked beside piles of gravel and a yellow sewer pump.
During the 2011 M7.8 Kaikōura earthquake, ground motions recorded near the epicentre showed a significant spatial variation. The Te Mara farm (WTMC) station, the nearest to the epicentre, recorded 1g and 2.7g of horizontal and vertical peak ground accelerations (PGA), respectively. The nearby Waiu Gorge (WIGC) station recorded a horizontal PGA of 0.8g. Interestingly, however, the Culverden Airlie Farm (CULC) station that was very closely located to WIGC recorded a horizontal PGA of only 0.25g. This poster demonstrates how the local geological condition could have contributed to the spatially variable ground motions observed in the North Canterbury, based on the results of recently conducted geophysical investigations. The surficial geology of this area is dominated by alluvial gravel deposits with traces of silt. A borehole log showed that the thickness of the sediments at WTMC is over 76 metres. Interestingly, the shear wave velocity (Vs) profiles obtained from the three strong motion sites suggest unusually high shear wave velocity of the gravelly sediments. The velocity of sediments and the lack of clear peaks in the horizontal-to-vertical (H/V) spectral ratio at WTMC suggest that the large ground motion observed at this station was likely caused by the proximity of the station to the causative fault itself; the site effect was likely insignificant. Comparisons of H/V spectral ratios and Vs profiles suggest that the sediment thickness is much smaller at WIGC compared with CULC; the high PGA at WIGC was likely influenced by the high-frequency amplification caused by the response of shallow sediments.
The influence of nonlinear soil-foundation-structure interaction (SFSI) on the performance of multi-storey buildings during earthquake events has become increasingly important in earthquake resistant design. For buildings on shallow foundations, SFSI refers to nonlinear geometric effects associated with uplift of the foundation from the supporting soil as well as nonlinear soil deformation effects. These effects can potentially be beneficial for structural performance, reducing forces transmitted from ground shaking to the structure. However, there is also the potential consequence of residual settlement and rotation of the foundation. This Thesis investigates the influence of SFSI in the performance of multi-storey buildings on shallow foundations through earthquake observations, experimental testing, and development of spring-bed numerical models that can be incorporated into integrated earthquake resistant design procedures. Observations were made following the 22 February 2011 Christchurch Earthquake in New Zealand of a number of multi-storey buildings on shallow foundations that performed satisfactorily. This was predominantly the case in areas where shallow foundations, typically large raft foundations, were founded on competent gravel and where there was no significant manifestation of liquefaction at the ground surface. The properties of these buildings and the soils they are founded on directed experimental work that was conducted to investigate the mechanisms by which SFSI may have influenced the behaviour of these types of structure-foundation systems. Centrifuge experiments were undertaken at the University of Dundee, Scotland using a range of structure-foundation models and a layer of dense cohesionless soil to simulate the situation in Christchurch where multi-storey buildings on shallow foundations performed well. Three equivalent single degree of freedom (SDOF) models representing 3, 5, and 7 storey buildings with identical large raft foundations were subjected to a range of dynamic Ricker wavelet excitations and Christchurch Earthquake records to investigate the influence of SFSI on the response of the equivalent buildings. The experimental results show that nonlinear SFSI has a significant influence on structural response and overall foundation deformations, even though the large raft foundations on competent soil meant that there was a significant reserve of bearing capacity available and nonlinear deformations may have been considered to have had minimal effect. Uplift of the foundation from the supporting soil was observed across a wide range of input motion amplitudes and was particularly significant as the amplitude of motion increased. Permanent soil deformation represented by foundation settlement and residual rotation was also observed but mainly for the larger input motions. However, the absolute extent of uplift and permanent soil deformation was very small compared to the size of the foundation meaning the serviceability of the building would still likely be maintained during large earthquake events. Even so, the small extent of SFSI resulted in attenuation of the response of the structure as the equivalent period of vibration was lengthened and the equivalent damping in the system increased. The experimental work undertaken was used to validate and enhance numerical modelling techniques that are simple yet sophisticated and promote interaction between geotechnical and structural specialists involved in the design of multi-storey buildings. Spring-bed modelling techniques were utilised as they provide a balance between ease of use, and thus ease of interaction with structural specialists who have these techniques readily available in practice, and theoretically rigorous solutions. Fixed base and elastic spring-bed models showed they were unable to capture the behaviour of the structure-foundation models tested in the centrifuge experiments. SFSI spring-bed models were able to more accurately capture the behaviour but recommendations were proposed for the parameters used to define the springs so that the numerical models closely matched experimental results. From the spring-bed modelling and results of centrifuge experiments, an equivalent linear design procedure was proposed along with a procedure and recommendations for the implementation of nonlinear SFSI spring-bed models in practice. The combination of earthquake observations, experimental testing, and simplified numerical analysis has shown how SFSI is influential in the earthquake performance of multi-storey buildings on shallow foundations and should be incorporated into earthquake resistant design of these structures.