A video of an address by Dr. Mark Quigley, Associate Professor of Active Tectonics and Geomorphology at the University of Canterbury. This talk was given at the 2015 Seismics and the City forum and addresses changes to the lie of the land - both physical and metaphorical.
A video of an address by Russell Stanners, CEO of Vodafone, at the 2015 Seismics and the City forum. This talk focuses on smart buildings and new ways of working.
A video of an address by Corrine Haines, Managing Director of Trimble, at the 2015 Seismics and the City forum. This talk focuses on smart buildings and new ways of working.
A video of an address by David Ayers, Mayor of Waimakariri District, at the 2015 Seismics and the City forum. The talk is about providing opportunities for input and feedback.
A video of an address by Carolyn Robertson, Libraries and Information Manager of Christchurch Libraries, at the 2015 Seismics and the City forum. The talk is about providing opportunities for input and feedback.
A video of an address by Keith Land, Head of Canterbury Land Settlement, EQC, at the 2015 Seismics and the City forum. This talk is about learning from complex claims and local knowledge.
A video of an address by developer Stephen Collins, at the 2015 Seismics and the City forum. This talk focuses on commercial development progress, and opportunities and issues in Central Christchurch and beyond.
A video of an address by Dr. Duncan Webb, Partner of Lane Neave, at the 2015 Seismics and the City forum. This talk is about learning from complex claims and local knowledge.
A video of an address by Geoff Cavell, Managing Director of Winnie Bagoes Holding Ltd, at the 2015 Seismics and the City forum. This talk is about learning from complex claims and local knowledge.
A video of an address by Blair Chapell, CPIT graduand, at the 2015 Seismics and the City forum. Mr. Chapell shares his aspirations for a renewed Christchurch and his goals for contributing to this.
A video of an address by Evan Smith, Co-Chair of the Avon-Otakaro Network and Programme Manager of Eastern Vision, at the 2015 Seismics and the City forum. The talk is about providing opportunities for input and feedback.
A video of an address by Kevin Lynn, General Manager of Commercial Operations at Schneider Electric NZ, at the 2015 Seismics and the City forum. This talk focuses on smart buildings and new ways of working.
A video of an address by Megan Veitch, University of Canterbury student, at the 2015 Seismics and the City forum. Ms. Veitch shares her aspirations for a renewed Christchurch and her goals for contributing to this.
A video of an address by Peter Rose, Chief Executive of Southern Response Earthquake Services Limited, at the 2015 Seismics and the City forum. This talk is about learning from complex claims and local knowledge.
A video of an address by Nick Hunt, Managing Director of Lichfield Holdings Ltd, at the 2015 Seismics and the City forum. This talk focuses on commercial development progress, and opportunities and issues in Central Christchurch and beyond.
A video of an address by Tom Beaumont, Founder and CEO of Clean Streams, at the 2015 Seismics and the City forum. Mr. Beaumont shares his aspirations for a renewed Christchurch and his goals for contributing to this.
A video of an address by Brian Parker, Project Manager of Canterbury Communities' Earthquake Recovery Network (CanCERN) and Managing Director of Sharp Teaching, at the 2015 Seismics and the City forum. This talk is about learning from complex claims and local knowledge.
A video of an address by John Ombler, Acting CEO of CERA, at the 2015 Seismics and the City forum. In this talk, Mr. Ombler shares his take on the progress if the rebuild, positive signs of advancement and what's in the pipeline; and how the main obstacles can be resolved.
A video of an address by Ian Simpson, CEO of CERA, at the 2015 Seismics and the City forum. In this talk, Mr. Simpson shares his take on the progress of the rebuild, positive signs of advancement and what's in the pipeline; and how the main obstacles can be resolved.
A video of an address by Joanna Norris, Editor of The Press, at the 2015 Seismics and the City forum. In this talk, Ms. Norris shares her take on the progress of the rebuild, positive signs of advancement and what's in the pipeline; and how the main obstacles can be resolved.
A video of an address by Raf Manji, Finance Spokesperson at the Christchurch City Council, at the 2015 Seismics and the City forum. In this talk, Mr. Manji shares his take on the progress of the rebuild, positive signs of advancement and what's in the pipeline; and how the main obstacles can be resolved.
A video of an address by Hon. Nicky Wagner, Associate Minister for the Canterbury Earthquake Recovery, at the 2015 Seismics and the City forum. In this talk, Minister Wagner shares her take on the progress of the rebuild, positive signs of advancement and what's in the pipeline; and how the main obstacles can be resolved.
A video of an address by Peter Townsend, CEO of Canterbury Employers Chamber of Commerce, at the 2015 Seismics and the City forum. In this talk, Mr. Townsend shares his take on the progress of the rebuild, positive signs of advancement and what's in the pipeline; and how the main obstacles can be resolved.
A video of a panel summary at the 2015 Seismics and the City forum, featuring Hon. Nicky Wagner, Associate Minister for the Canterbury Earthquake Recovery; John Ombler, Acting CEO of CERA; Ian Townsend, CEO of CERA; Raf Manji, Finance Spokesperson at the Christchurch City Council; Peter Townsend, CEO of Canterbury Employers Chamber of Commerce; and Joanna Norris, Editor of The Press.
This paper presents an examination of ground motion observations from 20 near-source strong motion stations during the most significant 10 events in the 2010-2011 Canterbury earthquake to examine region-specific systematic effects based on relaxing the conventional ergodic assumption. On the basis of similar site-to-site residuals, surfical geology, and geographical proximity, 15 of the 20 stations are grouped into four sub-regions: the Central Business District; and Western, Eastern, and Northern suburbs. Mean site-to-site residuals for these sub-regions then allows for the possibility of non-ergodic ground motion prediction over these sub-regions of Canterbury, rather than only at strong motion station locations. The ratio of the total non-ergodic vs. ergodic standard deviation is found to be, on average, consistent with previous studies, however it is emphasized that on a site-by-site basis the non-ergodic standard deviation can easily vary by ±20%.
The 2010-2011 Canterbury earthquakes were recorded over a dense strong motion network in the near-source region, yielding significant observational evidence of seismic complexities, and a basis for interpretation of multi-disciplinary datasets and induced damage to the natural and built environment. This paper provides an overview of observed strong motions from these events and retrospective comparisons with both empirical and physics-based ground motion models. Both empirical and physics-based methods provide good predictions of observations at short vibration periods in an average sense. However, observed ground motion amplitudes at specific locations, such as Heathcote Valley, are seen to systematically depart from ‘average’ empirical predictions as a result of near surface stratigraphic and topographic features which are well modelled via sitespecific response analyses. Significant insight into the long period bias in empirical predictions is obtained from the use of hybrid broadband ground motion simulation. The comparison of both empirical and physics-based simulations against a set of 10 events in the sequence clearly illustrates the potential for simulations to improve ground motion and site response prediction, both at present, and further in the future.
he strong motion station at Heathcote Valley School (HVSC) recorded unusually high peak ground accelerations (2.21g vertical and 1.41g horizontal) during the February 2011 Christchurch earthquake. Ground motions recorded at HVSC in numerous other events also exhibited consistently higher intensities compared with nearby strong motion stations. We investigated the underlying causes of such high intensity ground motions at HVSC by means of 2D dynamic finite element analyses, using recorded ground motions during the 2010-2011 Canterbury earthquake sequence. The model takes advantage of a LiDAR-based digital elevation model (DEM) to account for the surface topography, while the geometry and dynamic properties of the surficial soils are characterized by seismic cone penetration tests (sCPT) and Multi-Channel Analyses of Surface Waves (MASW). Comparisons of simulated and recorded ground motions suggests that our model performs well for distant events, while for near-field events, ground motions recorded at the adopted reference station at Lyttelton Port are not reasonable input motions for the simulation. The simulations suggest that Rayleigh waves generated at the inclined interface of the surficial colluvium and underlying volcanic rock strongly affect the ground motions recorded at HVSC, in particular, being the dominant contributor to the recorded vertical motions.
The sequence of earthquakes that has affected Christchurch and Canterbury since September 2010 has caused damage to a great number of buildings of all construction types. Following post-event damage surveys performed between April 2011 and June 2011, an inventory of the stone masonry buildings in Christchurch and surrounding areas was carried out in order to assemble a database containing the characteristic features of the building stock, as a basis for studying the vulnerability factors that might have influenced the seismic performance of the stone masonry building stock during the Canterbury earthquake sequence. The damage suffered by unreinforced stone masonry buildings is reported and different types of observed failures are described using a specific survey procedure currently in use in Italy. The observed performance of seismic retrofit interventions applied to stone masonry buildings is also described, as an understanding of the seismic response of these interventions is of fundamental importance for assessing the utility of such strengthening techniques when applied to unreinforced stone masonry structures. AM - Accepted Manuscript
The need for a simple but rigorous seismic assessment procedure to predict damage to reinforced concrete buildings during a seismic event has been highlighted following the Canterbury Earthquake sequence. Such simplified assessment procedure, applied to individual structure or large building inventory, should not only have low requirement in terms of input information and involve straightforward analyses, but also should be capable to provide reliable predictive results within short timeframe. This research provides a general overview and critical comparison of alternative simplified assessment procedures adopted in NZSEE 2006 Guidelines (Assessment and Improvement of the Structural Performance of Buildings in Earthquakes), ASCE 41-13 (Seismic Evaluation and Retrofit of Existing Buildings), and EN: 1998-3: 2005 (Assessment and Retrofitting of Buildings). Particular focus is given to the evaluation of the capability of Simplified Lateral Mechanism Analysis (SLaMa), which is an analytical pushover method adopted in NZSEE 2006 Guidelines. The predictive results from SLaMa are compared to damages observed for a set of reinforced concrete buildings in Christchurch, as well as the results from more detailed assessment procedure based on numerical modelling. This research also suggests improvements to SLaMa, together with validation of the improvements, to include assessment of local mechanism by strength hierarchy evaluation, as well as to develop assessment of global mechanism including post-yield mechanism sequence based on local mechanism.
Documenting earthquake-induced ground deformation is significant to assess the characteristics of past and contemporary earthquakes and provide insight into seismic hazard. This study uses airborne light detection and ranging (LiDAR) and conducts multi-disciplinary field techniques to document the surface rupture morphology and evaluate the paleoseismicity and seismic hazard parameters of the Hurunui segment of the Hope Fault in the northern South Island of New Zealand. It also documents and evaluates seismically induced features and ground motion characteristics of the 2010 Darfield and 2011 Christchurch earthquakes in the Port Hills, south of Christchurch. These two studies are linked in that they investigate the near-field coseismic features of large (Mw ~7.1) earthquakes in New Zealand and produce data for evaluating seismic hazards of future earthquakes. In the northern South Island of New Zealand, the Australian-Pacific plate boundary is characterised by strike-slip deformation across the Marlborough Fault System (MFS). The ENE-striking Hope Fault (length: ~230 km) is the youngest and southernmost fault in the MFS, and the second fastest slipping fault in New Zealand. The Hope Fault is a major source of seismic hazard in New Zealand and has ruptured (in-part) historically in the Mw 7.1 1888 Amuri earthquake. In the west, the Hurunui segment of the Hope Fault is covered by beech forest. Hence, its seismic hazard parameters and paleoearthquake chronology were poorly constrained and it was unknown whether the 1888 earthquake ruptured this segment or not and if so, to what extent. Utilising LiDAR and field data, a 29 km-long section of the Hurunui segment of the Hope Fault is mapped. LiDAR-mapping clearly reveals the principal slip zone (PSZ) of the fault and a suite of previously unrecognised structures that form the fault deformation zone (FDZ). FDZ width measurements from 415 locations reveal a spatially-variable, active FDZ up to ~500 m wide with an average width of 200 m. Kinematic analysis of the fault structures shows that the Hurunui segment strikes between 070° and 075° and is optimally oriented for dextral strike-slip within the regional stress field. This implies that the wide FDZ observed is unlikely to result from large-scale fault mis-orientation with respect to regional stresses. The analysis of FDZ width indicates that it increases with increased hanging wall topography and increased topographic relief suggesting that along-strike topographic perturbations to fault geometry and stress states increase fault zone complexity and width. FDZ width also increases where the tips of adjacent PSZ strands locally vary in strike, and where the thickness of alluvial deposits overlying bedrock increases. LiDAR- and photogrammetrically-derived topographic mapping indicates that the boundary between the Hurunui and Hope River segments is characterised by a ~850-m-wide right stepover and a 9º-14° fault bend. Paleoseismic trenching at Hope Shelter site reveals that 6 earthquakes occurred at A.D. 1888, 1740-1840, 1479-1623, 819-1092, 439-551, and 373- 419. These rupture events have a mean recurrence interval of ~298 ± 88 yr and inter-event times ranging from 98 to 595 yrs. The variation in the inter-event times is explained by (1) coalescing rupture overlap from the adjacent Hope River segment on to the Hurunui segment at the study site, (2) temporal clustering of large earthquakes on the Hurunui segment, and/or (3) ‘missing’ rupture events. It appears that the first two options are more plausible to explain the earthquake chronologies and rupture behaviour on the Hurunui segment, given the detailed nature of the geologic and chronologic investigations. This study provides first evidence for coseismic multi-segment ruptures on the Hope Fault by identifying a rupture length of 44-70 km for the 1888 earthquake, which was not confined to the Hope River segment (primary source for the 1888 earthquake). LiDAR data is also used to identify and measure dextral displacements and scarp heights from the PSZ and structures within the FDZ along the Hurunui segment. Reconstruction of large dextrally-offset geomorphic features shows that the vertical component of slip accounts for only ~1% of the horizontal displacements and confirms that the fault is predominantly strike-slip. A strong correlation exists between the dextral displacements and elevations of geomorphic features suggesting the possibility of age correlation between the geomorphic features. A mean single event displacement (SED) of 3.6 ± 0.7 m is determined from interpretation of sets of dextral displacements of ≤ 25 m. Using the available surface age data and the cumulative dextral displacements from Matagouri Flat, McKenzie Fan, Macs Knob and Hope River sites, and the mean SED, a mean slip rate of 12.2 ± 2.4 mm/yr, and a mean recurrence interval of ~320 ± 120 yr, and a potential earthquake magnitude of Mw 7.2 are determined for the Hurunui segment. This study suggests that the fault slip rate has been constant over the last ~15000 yr. Strong ground motions from the 2010 Darfield (Canterbury) earthquake displaced boulders and caused ground damage on some ridge crests in the Port Hills. However, the 2011 Christchurch earthquake neither displaced boulders nor caused ground damage at the same ridge crests. Documentation of locations (~400 m a.s.l.), lateral displacements (8-970 cm), displacement direction (250° ± 20°) of displaced boulders, in addition to their hosting socket geometries (< 1 cm to 50 cm depth), the orientation of the ridges (000°-015°) indicate that boulders have been displaced in the direction of instrumentally recorded transient peak ground horizontal displacements nearby and that the seismic waves have been amplified at the study sites. The co-existence of displaced and non-displaced boulders at proximal sites suggests small-scale ground motion variability and/or varying boulder-ground dynamic interactions relating to shallow phenomena such as variability in soil depth, bedrock fracture density and/or microtopography on the bedrock-soil interface. Shorter shaking duration of the 2011 Christchurch event, differing frequency contents and different source characteristics were all factors that may have contributed to generating circumstances less favourable to boulder displacement in this earthquake. Investigating seismically induced features, fault behaviour, site effects on the rupture behaviour, and site response to the seismic waves provides insights into fault rupture hazards.