Photographs of the Brick Art unveiling, Greening the Rubble, on the former Asko site - corner of Victoria and Salisbury Streets, Christchurch 8 February 2011. From the collection of Christchurch City Libraries CCL-Brickart-2011-IMG_2458
Photographs of the Brick Art unveiling, Greening the Rubble, on the former Asko site - corner of Victoria and Salisbury Streets, Christchurch 8 February 2011. From the collection of Christchurch City Libraries CCL-Brickart-2011-IMG_2512
Photographs of the Brick Art unveiling, Greening the Rubble, on the former Asko site - corner of Victoria and Salisbury Streets, Christchurch 8 February 2011. From the collection of Christchurch City Libraries CCL-Brickart-2011-IMG_2471
Photographs of the Brick Art unveiling, Greening the Rubble, on the former Asko site - corner of Victoria and Salisbury Streets, Christchurch 8 February 2011. From the collection of Christchurch City Libraries CCL-Brickart-2011-IMG_2504
Three diggers clearing rubble side by side on the site of the CTV Building, with members of the New Zealand and Chinese Urban Search and Rescue Teams looking on.
A photograph of a pianist playing a painted piano. The piano is on the site of Wayne Youle's mural, 'I seem to have temporarily misplaced my sense of humour'.
A photograph of a mural on a wall in the former site of a building on Norwich Quay in Lyttelton. Construction material has been laid up against the mural.
A photograph captioned by BeckerFraserPhotos, "Detail of the cracks in the building at the front of the Crichton Cobbers Youth and Community Club site on Fitzgerald Avenue".
This paper summarizes the development of a high-resolution surficial shear wave velocity model based on the combination of the large high-spatial-density database of cone penetration test (CPT) logs in and around Christchurch, New Zealand and a recently-developed Christchurch-specific empirical correlation between soil shear wave velocity and CPT. This near-surface shear wave velocity model has applications for site characterization efforts via the development of maps of time-averaged shear wave velocities over specific depths, as well as use in site response analysis and ground motion simulation.
This poster discusses several possible approaches by which the nonlinear response of surficial soils can be explicitly modelled in physics-based ground motion simulations, focusing on the relative advantages and limitations of the various methodologies. These methods include fully-coupled 3D simulation models that directly allow soil nonlinearity in surficial soils, the domain reduction method for decomposing the physical domain into multiple subdomains for separate simulation, conventional site response analysis uncoupled from the simulations, and finally, the use of simple empirically based site amplification factors We provide the methodology for an ongoing study to explicitly incorporate soil nonlinearity into hybrid broadband simulations of the 2010-2011 Canterbury, New Zealand earthquakes.
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
A photograph of a vacant site on the corner of Manchester Street and Worcester Street. This is to be the location of the Archrobatics project, which is part of LUXCITY.
A photograph of a vacant site on the corner of Manchester Street and Worcester Street. This is to be the location of the Archrobatics project, which is part of LUXCITY.
A photograph of a vacant site on the corner of Manchester Street and Worcester Street. This is to be the location of the Archrobatics project, which is part of LUXCITY.
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
Photograph captioned by BeckerFraserPhotos, "The intersection of Colombo and Cashel Streets, looking east along Cashel Street to the big crane on the demolition site of the Westpac building".
A photograph of the former site of Donna Allfrey's house at 406 Oxford Terrace, taken from the footpath in front. Allfrey's house was demolished after her land was zoned Red.
Photograph captioned by BeckerFraserPhotos, "Copthorne Hotel on Colombo Street with the demolition site of the Allan McLean building to the left. Liquefaction is visible in the foreground".
A photograph of a vacant site on the corner of Manchester Street and Worcester Street. This is to be the location of the Archrobatics project, which is part of LUXCITY.
Workers building the 10m2 office building, soon to be the Gap Filler Headquarters in Sydenham. A sign out front reads, "Gap Filler project in progress on this site".
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
Photograph captioned by BeckerFraserPhotos, "Looking from Gloucester Street across the demolition site of the Coachman towards the Heritage Hotel in Cathedral Square with Hotel Grand Chancellor (left background)".
A photograph of the Gap Filler Dance-O-Mat talk and speed dancing session on site at the Gap Filler Dance-O-Mat. The event was part of FESTA 2012.
Liquefaction is a phenomenon that results in a loss of strength and stability of a saturated soil mass due to dynamic excitation such as that imposed by an earthquake. The granular nature of New Zealand soils and the location of many of our cities and towns on fluvial foundations are such that the effects of liquefaction can be very important. Research was undertaken to build on the past work undertaken at the University of Canterbury studying the effects of the 1929 Murchison earthquake, the 1968 Inangahua earthquake and the 1991 Hawks Crag earthquakes on the West Coast. Additional archival information has been gathered from newspapers and reports and from discussions with people who experienced one or all of these large earthquakes that occurred on the West Coast during the 20th Century. Further, some twenty Cone Penetrometer Tests were carried out, with varying success, in Greymouth and Karamea using the Department of Civil Engineering's Drilling Rig. These, combined with the basic site investigation information, consolidate and add to the liquefaction case history data bank at the University of Canterbury. Many of the sites have liquefied in some but not all of the three earthquakes and thus provide both upper and lower bounds for the calibration of empirical models. While a lack of knowledge of the 1929 source location reduces the value of information from that event, the data form a useful set of liquefaction case histories and will become more so as further earthquakes occur. A list of critical sites for checking of the future earthquakes is provided and recommendations are made for the installation of downhole arrays of accelerometers and pore water pressure transducers at a number of sites.
A number of field testing techniques, such as standard penetration test (SPT), cone penetration test (CPT), and Swedish weight sounding (SWS), are popularly used for in-situ characterisation. The screw driving sounding (SDS) method, which has been recently developed in Japan, is an improved version of the SWS technique and measures more parameters, including the required torque, load, speed of penetration and rod friction; these provide more robust way of characterising soil stratigraphy. It is a cost-efficient technique which uses a machine-driven and portable device, making it ideal for testing in small-scale and confined areas. Moreover, with a testing depth of up to 10-15m, it is suitable for liquefaction assessment. Thus, the SDS method has great potential as an in-situ testing method for geotechnical site characterisation, especially for residential house construction. In this paper, the results of SDS tests performed at a variety of sites in New Zealand are presented. The soil database was employed to develop a soil classification chart based on SDS-derived parameters. Moreover, using the data obtained following the 2010-2011 Christchurch Earthquake Se-quence, a methodology was established for liquefaction potential evaluation using SDS data. http://www.isc5.com.au/wp-content/uploads/2016/09/1345-2-ORENSE.pdf