Damage to a house in Richmond. A brick chimney has visibly twisted and there are gaps between the bricks. The photographer comments, "One chimney is damaged but still standing - for now. (It was taken down on the morning of Day 2, just as well)".
Damage to a house in Richmond. A brick chimney has visibly twisted and there are gaps between the bricks. The photographer comments, "Damaged chimney. We'll have to get this taken down tidily, but our roofer friends are a bit busy... (It was taken down on the morning of Day 2, just as well)".
Damage to a house in Richmond. A large crack runs diagonally through a brick wall. The photographer comments, "More cracked brickwork".
Damage to a house in Richmond. A brick chimney has partially collapsed. The photographer comments, "The chimney above our bedroom crumbled - glad it didn't come down in one piece".
A large crack runs through the garden of a house in Richmond. The photographer comments, "Cracks in the vege garden, moving the paving slabs".
Damage to a house in Richmond. Bricks have fallen from a wall, exposing the wooden framing beneath. The photographer comments, "The foundation and a section of the wall of the dining room have shifted and cracked. The dining room floor is very springy".
Damage to a house in Richmond. Part of the brick wall is visibly out of alignment, leaving large gaps at the corner of the house. The photographer comments, "Dining room exterior wall".
Damage to a house in Richmond. Two parts of the house have moved apart, leaving a large gap. The photographer comments, "Dining room exterior wall".
Damage to a house in Richmond. There is a large crack in the driveway, and cracks in the brickwork of a house. The photographer comments, "Tarsealed driveways have numerous cracks".
Residents walk along River Road past large cracks where the road has slumped towards the river. The photographer comments, "Lateral spreading cracks in River Rd; the land left of the crack moved towards the river. The Banks Ave/Dallington Tce end of our block is impassable".
Jane's Bar in the Henry Africa's building is cordoned off with danger tape. The photographer comments, "My local bar is unsafe and can't open. Sad".
Road cones cordon off a large crack in River Road where the road has slumped towards the river. The photographer comments, "Lateral spreading towards the river is very obvious here".
A family walk their dogs down Avonside Drive, while a boy walks past carrying a shovel. In the background, power poles are leaning at extreme angles. The photographer comments, "Power poles in Avonside Drive developed an alarming lean".
Footprints in liquefaction silt on the side of a residential street. The photographer comments, "Silt has accumulated everywhere".
The twisted and broken Medway Street bridge, cordoned off with emergency tape. The photographer comments, "The twisted footbridge at the Medway St corner".
A man photographs large cracks in River Road where the road has slumped towards the river. The photographer comments, "Cracking in River Rd. The Banks Ave/Dallington Tce end of our block is impassable".
The twisted and broken Medway Street bridge, cordoned off with emergency tape. The photographer comments, "The twisted footbridge at the Medway St corner".
The latest two great earthquake sequences; 2010- 2011 Canterbury Earthquake and 2016 Kaikoura Earthquake, necessitate a better understanding of the New Zealand seismic hazard condition for new building design and detailed assessment of existing buildings. It is important to note, however, that the New Zealand seismic hazard map in NZS 1170.5.2004 is generalised in effort to cover all of New Zealand and limited to a earthquake database prior to 2001. This is “common” that site-specific studies typically provide spectral accelerations different to those shown on the national map (Z values in NZS 1170.5:2004); and sometimes even lower. Moreover, Section 5.2 of Module 1 of the Earthquake Geotechnical Engineering Practice series provide the guidelines to perform site- specific studies.
A house in Richmond, seen before the earthquakes.
A house in Avonside, seen before the earthquakes.
A photograph of the earthquake-damaged output shaft from the top-plate of the Townsend Telescope's clock drive. The output shaft was bent out of shape during the 22 February 2011 earthquake.
A paper prepared for the Bulletin of the New Zealand Society for Earthquake Engineering, Vol. 44, no. 4, December 2011.
This paper presents on-going challenges in the present paradigm shift of earthquakeinduced ground motion prediction from empirical to physics-based simulation methods. The 2010-2011 Canterbury and 2016 Kaikoura earthquakes are used to illustrate the predictive potential of the different methods. On-going efforts on simulation validation and theoretical developments are then presented, as well as the demands associated with the need for explicit consideration of modelling uncertainties. Finally, discussion is also given to the tools and databases needed for the efficient utilization of simulated ground motions both in specific engineering projects as well as for near-real-time impact assessment.
A document which outlines SCIRT's post-earthquake asset assessment process.
An entry from Deborah Fitchett's blog for 4 September 2010, posted to Livejournal. The entry is titled, "In which an earthquake".The entry was downloaded on 14 April 2015.
An entry from Deborah Fitchett's blog for 4 September 2010, posted to Dreamwidth. The entry is titled, "In which an earthquake".The entry was downloaded on 17 April 2015.
We examined the stratigraphy of alluvial fans formed at the steep range front of the Southern Alps at Te Taho, on the north bank of the Whataroa River in central West Coast, South Island, New Zealand. The range front coincides with the Alpine Fault, an Australian-Pacific plate boundary fault, which produces regular earthquakes. Our study of range front fans revealed aggradation at 100- to 300-year intervals. Radiocarbon ages and soil residence times (SRTs) estimated by a quantitative profile development index allowed us to elucidate the characteristics of four episodes of aggradation since 1000 CE. We postulate a repeating mode of fan behaviour (fan response cycle [FRC]) linked to earthquake cycles via earthquake-triggered landslides. FRCs are characterised by short response time (aggradation followed by incision) and a long phase when channels are entrenched and fan surfaces are stable (persistence time). Currently, the Te Taho and Whataroa River fans are in the latter phase. The four episodes of fan building we determined from an OxCal sequence model correlate to Alpine Fault earthquakes (or other subsidiary events) and support prior landscape evolution studies indicating ≥M7.5 earthquakes as the main driver of episodic sedimentation. Our findings are consistent with other historic non-earthquake events on the West Coast but indicate faster responses than other earthquake sites in New Zealand and elsewhere where rainfall and stream gradients (the basis for stream power) are lower. Judging from the thickness of fan deposits and the short response times, we conclude that pastoral farming (current land-use) on the fans and probably across much of the Whataroa River fan would be impossible for several decades after a major earthquake. The sustainability of regional tourism and agriculture is at risk, more so because of the vulnerability of the single through road in the region (State Highway 6).
A conference paper about the Pipe Damage Assessment Tool (PDAT).
Knowing how to rapidly rebuild disaster-damaged infrastructure, while deciding appropriate recovery strategies and catering for future investment is a matter of core interest to government decision makers, utility providers, and business sectors. The purpose of this research is to explore the effects of decisions and outcomes for physical reconstruction on the overall recovery process of horizontal infrastructure in New Zealand using the Canterbury and Kaikoura earthquakes as cases. A mixed approach including a systematic review, questionnaire survey and semi-structured interviews is used to capture perspectives of those involved in reconstruction process and gain insights into the effect of critical elements on infrastructure downtime. Findings from this research will contribute towards advancements of a systems dynamics model considering critical decision-making variables across phases of the reconstruction process to assess how these variables affect the rebuild process and the corresponding downtime. This project will improve the ability to explore alternative resilience improvement pathways and test the efficacy of alternative means for facilitating a faster and better reconstruction process.
The 2010-2011 Christchurch earthquakes generated damage in several Reinforced Concrete (RC) buildings, which had RC walls as the principal resistant element against earthquake demand. Despite the agreement between structural engineers and researchers in an overall successfully performance there was a lack of knowledge about the behaviour of the damaged structures, and even deeper about a repaired structure, which triggers arguments between different parties that remains up to these days. Then, it is necessary to understand the capacity of the buildings after the earthquake and see how simple repairs techniques improve the building performance. This study will assess the residual capacity of ductile slender RC walls according to current standards in New Zealand, NZS 3101.1 2006 A3. First, a Repaired RC walls Database is created trying to gather previous studies and to evaluate them with existing international guidelines. Then, an archetype building is designed, and the wall is extracted and scaled. Four half-scale walls were designed and will be constructed and tested at the Structures Testing Laboratory at The University of Auckland. The overall dimensions are 3 [m] height, 2 [m] length and 0.175 [m] thick. All four walls will be identical, with differences in the loading protocol and the presence or absence of a repair technique. Results are going to be useful to assess the residual capacity of a damaged wall compare to the original behaviour and also the repaired capacity of walls with simpler repair techniques. The expected behaviour is focussed on big changes in stiffness, more evident than in previously tested RC beams found in the literature.