This study analyses the performance of residential buildings in the town of Hveragerði in South Iceland during the 29 May 2008 Mw 6.3 Ölfus Earthquake. The earthquake occurred very close to the town, approximately 3–4 km from it. Ground shaking caused by the earthquake was recorded by a dense strong-motion array in the town. The array provided high-quality three-component ground acceleration data which is used to quantify a hazard scenario. In addition, surveys conducted in the town in the aftermath of the earthquake have provided information on macroseismic intensity at various locations in the town. Detailed information regarding the building stock in the town is collected, and their seismic vulnerability models are created by using building damage data obtained from the June 2000 South Iceland earthquakes. Damage to buildings are then simulated by using the scenario hazard and vulnerability models. Damage estimates were also obtained by conducting a survey. Simulated damage based on the scenario macroseismic intensity is found to be similar to damage estimated from survey data. The buildings performed very well during the earthquake—damage suffered was only 5 % of the insured value on the average. Correlation between actual damage and recorded ground-motion parameters is found to be statistically insignificant. No significant correlation of damage was observed, even with macroseismic intensity. Whereas significant correlation was observed between peak ground velocity and macroseismic intensity, neither of them appear to be good indicators of damage to buildings in the study area. This lack of correlation is partly due to good seismic capacity of buildings and partly due to the ordinal nature of macroseismic intensity scale. Consistent with experience from many past earthquakes, the survey results indicate that seismic risk in South Iceland is not so much due to collapse of buildings but rather due to damage to non-structural components and building contents.
[1]
Benedikt Halldorsson,et al.
The Mw6.3 Ölfus earthquake at 15:45 UTC on 29 May 2008 in South Iceland: ICEARRAY strong-motion recordings
,
2009
.
[2]
R. Rupakhety,et al.
Rotation-invariant mean duration of strong ground motion
,
2014,
Bulletin of Earthquake Engineering.
[3]
R. Sigbjörnsson,et al.
Macroseismic effects related to strong ground motion: a study of the South Iceland earthquakes in June 2000
,
2007
.
[4]
Roger M. W. Musson,et al.
The comparison of macroseismic intensity scales
,
2010
.
[5]
Freysteinn Sigmundsson,et al.
The 2008 May 29 earthquake doublet in SW Iceland
,
2010
.
[6]
Ragnar Sigbjörnsson,et al.
Rotation-invariant measures of earthquake response spectra
,
2013,
Bulletin of Earthquake Engineering.
[7]
A. Papageorgiou,et al.
Quantification of ground-motion parameters and response spectra in the near-fault region
,
2011
.
[8]
David A. Rhoades,et al.
Probabilistic Relationships between Ground‐Motion Parameters and Modified Mercalli Intensity in California
,
2012
.
[9]
R. Sigbjörnsson,et al.
Estimating coseismic deformations from near source strong motion records: methods and case studies
,
2010
.
[10]
J. Th. Snæbjörnsson,et al.
A note on the Mw 6.3 earthquake in Iceland on 29 May 2008 at 15:45 UTC
,
2009
.