Abstract

The Kaikōura earthquake brought the concept of basin effects to the forefront of conversation about building in the Wellington CBD. Local exceedances of ULS design spectra were observed in many waterfront sites in the 1.5-2.5s period range. This, coupled with low yield levels and certain structural forms present in previous generations of building design, meant that significant damage occurred in many buildings around the Wellington waterfront. A primary cause for the high spectral accelerations was the geological structure of the Wellington CBD. This paper will focus on the behaviour of generic buildings in response to these particular ground motions and suggest how lessons from this can inform the design of future buildings. It uses the Kaikōura Earthquake as the centre point for discussions about the relationship between building behaviour on soft soils and the effects on this of different forms of damping. More broadly, the aim is to help spark debate in the earthquake engineering community on the question: What sorts of structures should we be building on soft soil sites? This paper has been written in the wake of a number of damaging earthquakes throughout New Zealand, and with the concurrent increase in sophistication and spread of tools for analysing the effects of the ground motions induced by these earthquakes. The genesis of the ideas presented herein was in analysis of many waterfront buildings following the Kaikoura earthquake, and the attempts, often in vain, to match modelled building behaviour- where small tweaks in assumptions could have a radical effect on results- with actual observed damage – where cracks may have been seen in concrete or in partitions, but assessment of actual plastic strains reached in steel bars or beams was basically conjecture. This paper is broad in scope, therefore cannot possibly give each aspect the coverage of a series of papers which consider them in isolation and in detail. We nonetheless strongly believe that a holistic view of all topics is critical for design, and that the authors as ‘front line’ structural engineers are well positioned to present this. Sincere attempts have been made to justify our point of view with a strong basis in first principles, and backed by nonlinear time history analysis, or by reference to the work of others. We acknowledge that our beliefs are not shared by everyone and that some conclusions are provocative. It is neither the intent nor even the hope that we have the last word on this topic.

Highlights

  • INTRODUCTIONThe Wellington CBD is dominated by two geological basins. One is on what was the Te Aro Swamp, and consists primarily of swamp sediments and colluvium intersected by alluvial deposits of current and former streams

  • Wellington GeologyThe Wellington CBD is dominated by two geological basins

  • Science in the construction industry should be the handmaiden to good building design

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Summary

INTRODUCTION

The Wellington CBD is dominated by two geological basins. One is on what was the Te Aro Swamp, and consists primarily of swamp sediments and colluvium intersected by alluvial deposits of current and former streams. The basic analysis tools a structural engineer uses to account for inelastic behaviour - the equal displacement principle in forcebased-design, and equivalent viscous damping and effective stiffness-based period shift in displacement-based design – are intended to be a simple and generic approach to many different types of ground motions. The hysteretic damping reduction factors for the Kaikōura ground motion records are less than average for the Soil D Records at periods just under that of the peak spectral accelerations This is partially due to the dip in amplification at these periods, and partially due to the period elongation previously mentioned, which in this case may move the structure in phase with the dominant ground motion frequency. Further deformation is not met with a corresponding increase in force resistance, resulting in significantly increased relative displacement between the ground and the structure as the structure is ‘dragged’ in phase, to use a simplistic analogy

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