Liquefaction Assessment of a Loose Silty Sand Site in the 2008 Mw 6.3 Ölfus Earthquake
Seismicity in Iceland is related to the Mid-Atlantic plate boundary and primarily consolidated in two complex fracture zones. Liquefaction was observed after the Mw 6.3 Ölfus earthquake in 2008 at the site Arnarbaeli. The site consists of a thick silty sand stratum on the banks of the estuary of the...
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ftopinvisindi:oai:opinvisindi.is:20.500.11815/3826 2023-05-15T16:50:19+02:00 Liquefaction Assessment of a Loose Silty Sand Site in the 2008 Mw 6.3 Ölfus Earthquake Fattahi, Seyed Javad Olafsdottir, Elin Asta Erlingsson, Sigurdur Bessason, Bjarni Rupakhety, Rajesh Umhverfis- og byggingarverkfræðideild (HÍ) Faculty of Civil and Environmental Engineering (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland 2022-09-04 108 - 117 https://hdl.handle.net/20.500.11815/3826 en eng Conspress European Conference on Earthquake Engineering & Seismology;2022(3) https://hdl.handle.net/20.500.11815/3826 info:eu-repo/semantics/openAccess Liquefaction hazard Seismic Zones Equivalent-linear site response analysis Jarðskjálftaverkfræði info:eu-repo/semantics/conferenceObject 2022 ftopinvisindi https://doi.org/20.500.11815/3826 2023-01-11T23:50:54Z Seismicity in Iceland is related to the Mid-Atlantic plate boundary and primarily consolidated in two complex fracture zones. Liquefaction was observed after the Mw 6.3 Ölfus earthquake in 2008 at the site Arnarbaeli. The site consists of a thick silty sand stratum on the banks of the estuary of the river Ölfusa, and it is located less than 10 km from the earthquake epicentre. Based on nearby time history registrations, the estimated acceleration at the site was 0.6 - 0.7g. Using a simplified method, the safety factor against liquefaction based on the equivalent linear (EL) approach has been estimated. The analysis is built on in-situ field test data (i.e., MASW, and SPT). The analysis reveals the liquefaction depth, 4.4 m. It is shown that not only the current procedure is capable of predicting the occurrence of liquefaction, but also the safety factor which is in good agreement with the observed surface evidence of liquefaction at the site. This work was supported by the Icelandic Research Fund (Rannis), Grants number: 206793-052 and 218149-051. Peer Reviewed Conference Object Iceland Opin vísindi (Iceland) |
institution |
Open Polar |
collection |
Opin vísindi (Iceland) |
op_collection_id |
ftopinvisindi |
language |
English |
topic |
Liquefaction hazard Seismic Zones Equivalent-linear site response analysis Jarðskjálftaverkfræði |
spellingShingle |
Liquefaction hazard Seismic Zones Equivalent-linear site response analysis Jarðskjálftaverkfræði Fattahi, Seyed Javad Olafsdottir, Elin Asta Erlingsson, Sigurdur Bessason, Bjarni Rupakhety, Rajesh Liquefaction Assessment of a Loose Silty Sand Site in the 2008 Mw 6.3 Ölfus Earthquake |
topic_facet |
Liquefaction hazard Seismic Zones Equivalent-linear site response analysis Jarðskjálftaverkfræði |
description |
Seismicity in Iceland is related to the Mid-Atlantic plate boundary and primarily consolidated in two complex fracture zones. Liquefaction was observed after the Mw 6.3 Ölfus earthquake in 2008 at the site Arnarbaeli. The site consists of a thick silty sand stratum on the banks of the estuary of the river Ölfusa, and it is located less than 10 km from the earthquake epicentre. Based on nearby time history registrations, the estimated acceleration at the site was 0.6 - 0.7g. Using a simplified method, the safety factor against liquefaction based on the equivalent linear (EL) approach has been estimated. The analysis is built on in-situ field test data (i.e., MASW, and SPT). The analysis reveals the liquefaction depth, 4.4 m. It is shown that not only the current procedure is capable of predicting the occurrence of liquefaction, but also the safety factor which is in good agreement with the observed surface evidence of liquefaction at the site. This work was supported by the Icelandic Research Fund (Rannis), Grants number: 206793-052 and 218149-051. Peer Reviewed |
author2 |
Umhverfis- og byggingarverkfræðideild (HÍ) Faculty of Civil and Environmental Engineering (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland |
format |
Conference Object |
author |
Fattahi, Seyed Javad Olafsdottir, Elin Asta Erlingsson, Sigurdur Bessason, Bjarni Rupakhety, Rajesh |
author_facet |
Fattahi, Seyed Javad Olafsdottir, Elin Asta Erlingsson, Sigurdur Bessason, Bjarni Rupakhety, Rajesh |
author_sort |
Fattahi, Seyed Javad |
title |
Liquefaction Assessment of a Loose Silty Sand Site in the 2008 Mw 6.3 Ölfus Earthquake |
title_short |
Liquefaction Assessment of a Loose Silty Sand Site in the 2008 Mw 6.3 Ölfus Earthquake |
title_full |
Liquefaction Assessment of a Loose Silty Sand Site in the 2008 Mw 6.3 Ölfus Earthquake |
title_fullStr |
Liquefaction Assessment of a Loose Silty Sand Site in the 2008 Mw 6.3 Ölfus Earthquake |
title_full_unstemmed |
Liquefaction Assessment of a Loose Silty Sand Site in the 2008 Mw 6.3 Ölfus Earthquake |
title_sort |
liquefaction assessment of a loose silty sand site in the 2008 mw 6.3 ölfus earthquake |
publisher |
Conspress |
publishDate |
2022 |
url |
https://hdl.handle.net/20.500.11815/3826 |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
European Conference on Earthquake Engineering & Seismology;2022(3) https://hdl.handle.net/20.500.11815/3826 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/20.500.11815/3826 |
_version_ |
1766040487196622848 |