Loading…

Spatial variation of magnitude scaling factors during the 2010 Darfield and 2011 Christchurch, New Zealand, earthquakes

The combination of well-documented liquefaction response during the Darfield and Christchurch, New Zealand, earthquakes, densely-recorded ground motions for the events, and detailed subsurface characterization provides an unprecedented opportunity to investigate the significance of the spatial varia...

Full description

Saved in:
Bibliographic Details
Published in:Soil dynamics and earthquake engineering (1984) 2016-12, Vol.91, p.175-186
Main Authors: Carter, W.L., Green, R.A., Bradley, B.A., Wotherspoon, L.M., Cubrinovski, M.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-a477t-bac2d268f9109cdab554ac67b37237b53537eeca7966a7d232b7def1de38a6bd3
cites cdi_FETCH-LOGICAL-a477t-bac2d268f9109cdab554ac67b37237b53537eeca7966a7d232b7def1de38a6bd3
container_end_page 186
container_issue
container_start_page 175
container_title Soil dynamics and earthquake engineering (1984)
container_volume 91
creator Carter, W.L.
Green, R.A.
Bradley, B.A.
Wotherspoon, L.M.
Cubrinovski, M.
description The combination of well-documented liquefaction response during the Darfield and Christchurch, New Zealand, earthquakes, densely-recorded ground motions for the events, and detailed subsurface characterization provides an unprecedented opportunity to investigate the significance of the spatial variation of magnitude scaling factors (MSF) on liquefaction triggering. Towards this end, MSF were computed at 15 SMS sites across Christchurch and its surroundings using two established approaches. Trends in the spatial variation of the MSF computed using number of equivalent cycles (neq) from both approaches were similar, with the spatial variation being more significant for the Christchurch earthquake than the Darfield earthquake. However, there was no consistent trend for regions with lower computed MSF having experienced more severe or widespread liquefaction. Additionally, there is a general correlation between MSF and amax, but because amax ranges more widely than MSF it has a greater influence on the resulting seismic demand imposed on the soil than MSF does. Nevertheless, the spatial variation of the MSF is deemed significant enough that it warrants being considered for incorporation into future variants of simplified liquefaction evaluation procedures. •This study investigates the spatial variation of magnitude scaling factors.•Two well-documented earthquakes in New Zealand were used to investigate the spatial variation of MSF.•A general trend was identified that MSF correlate with PGA.•From a seismic demand perspective, PGA is more influential on liquefaction triggering than MSF.
doi_str_mv 10.1016/j.soildyn.2016.09.044
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1956032823</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0267726116303372</els_id><sourcerecordid>1956032823</sourcerecordid><originalsourceid>FETCH-LOGICAL-a477t-bac2d268f9109cdab554ac67b37237b53537eeca7966a7d232b7def1de38a6bd3</originalsourceid><addsrcrecordid>eNqFUMtO3DAUtRCVGCifgGSJLUn9SOxkhdAAbSXULlokxMa6sW-Ih5AMtgPi7-vRsO_qvs5D9xByxlnJGVffNmWc_eg-plLksWRtyarqgKx4o9tCVvzhkKyYULrQQvEjchzjhjGueaNW5P3PFpKHkb5B8LmbJzr39AWeJp8WhzRaGP30RHuwaQ6RuiXsxjQgzWaMXkPoPY6OwuR2G07XQ_Ax2WEJdrigv_CdPiKM-XxBEUIaXhd4xviVfOlhjHj6WU_I_e3N3_WP4u7395_rq7sCKq1T0YEVTqimbzlrrYOuriuwSndSC6m7WtZSI1rQrVKgnZCi0w577lA2oDonT8j5Xncb5tcFYzKbeQlTtjS8rRWTohEyo-o9yoY5xoC92Qb_AuHDcGZ2GZuN-czY7DI2rDU548y73PMwv_DmMZhoPU4WnQ9ok3Gz_4_CPz6aiKc</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1956032823</pqid></control><display><type>article</type><title>Spatial variation of magnitude scaling factors during the 2010 Darfield and 2011 Christchurch, New Zealand, earthquakes</title><source>ScienceDirect Freedom Collection</source><creator>Carter, W.L. ; Green, R.A. ; Bradley, B.A. ; Wotherspoon, L.M. ; Cubrinovski, M.</creator><creatorcontrib>Carter, W.L. ; Green, R.A. ; Bradley, B.A. ; Wotherspoon, L.M. ; Cubrinovski, M.</creatorcontrib><description>The combination of well-documented liquefaction response during the Darfield and Christchurch, New Zealand, earthquakes, densely-recorded ground motions for the events, and detailed subsurface characterization provides an unprecedented opportunity to investigate the significance of the spatial variation of magnitude scaling factors (MSF) on liquefaction triggering. Towards this end, MSF were computed at 15 SMS sites across Christchurch and its surroundings using two established approaches. Trends in the spatial variation of the MSF computed using number of equivalent cycles (neq) from both approaches were similar, with the spatial variation being more significant for the Christchurch earthquake than the Darfield earthquake. However, there was no consistent trend for regions with lower computed MSF having experienced more severe or widespread liquefaction. Additionally, there is a general correlation between MSF and amax, but because amax ranges more widely than MSF it has a greater influence on the resulting seismic demand imposed on the soil than MSF does. Nevertheless, the spatial variation of the MSF is deemed significant enough that it warrants being considered for incorporation into future variants of simplified liquefaction evaluation procedures. •This study investigates the spatial variation of magnitude scaling factors.•Two well-documented earthquakes in New Zealand were used to investigate the spatial variation of MSF.•A general trend was identified that MSF correlate with PGA.•From a seismic demand perspective, PGA is more influential on liquefaction triggering than MSF.</description><identifier>ISSN: 0267-7261</identifier><identifier>EISSN: 1879-341X</identifier><identifier>DOI: 10.1016/j.soildyn.2016.09.044</identifier><language>eng</language><publisher>Barking: Elsevier Ltd</publisher><subject>Canterbury earthquakes ; Christchurch ; Computation ; Earthquakes ; Liquefaction ; Magnitude scaling factors ; Scaling ; Scaling factors ; Seismic activity ; Seismic response ; Seismology ; Studies ; Variation</subject><ispartof>Soil dynamics and earthquake engineering (1984), 2016-12, Vol.91, p.175-186</ispartof><rights>2016 Elsevier Ltd</rights><rights>Copyright Elsevier BV Dec 2016</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a477t-bac2d268f9109cdab554ac67b37237b53537eeca7966a7d232b7def1de38a6bd3</citedby><cites>FETCH-LOGICAL-a477t-bac2d268f9109cdab554ac67b37237b53537eeca7966a7d232b7def1de38a6bd3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Carter, W.L.</creatorcontrib><creatorcontrib>Green, R.A.</creatorcontrib><creatorcontrib>Bradley, B.A.</creatorcontrib><creatorcontrib>Wotherspoon, L.M.</creatorcontrib><creatorcontrib>Cubrinovski, M.</creatorcontrib><title>Spatial variation of magnitude scaling factors during the 2010 Darfield and 2011 Christchurch, New Zealand, earthquakes</title><title>Soil dynamics and earthquake engineering (1984)</title><description>The combination of well-documented liquefaction response during the Darfield and Christchurch, New Zealand, earthquakes, densely-recorded ground motions for the events, and detailed subsurface characterization provides an unprecedented opportunity to investigate the significance of the spatial variation of magnitude scaling factors (MSF) on liquefaction triggering. Towards this end, MSF were computed at 15 SMS sites across Christchurch and its surroundings using two established approaches. Trends in the spatial variation of the MSF computed using number of equivalent cycles (neq) from both approaches were similar, with the spatial variation being more significant for the Christchurch earthquake than the Darfield earthquake. However, there was no consistent trend for regions with lower computed MSF having experienced more severe or widespread liquefaction. Additionally, there is a general correlation between MSF and amax, but because amax ranges more widely than MSF it has a greater influence on the resulting seismic demand imposed on the soil than MSF does. Nevertheless, the spatial variation of the MSF is deemed significant enough that it warrants being considered for incorporation into future variants of simplified liquefaction evaluation procedures. •This study investigates the spatial variation of magnitude scaling factors.•Two well-documented earthquakes in New Zealand were used to investigate the spatial variation of MSF.•A general trend was identified that MSF correlate with PGA.•From a seismic demand perspective, PGA is more influential on liquefaction triggering than MSF.</description><subject>Canterbury earthquakes</subject><subject>Christchurch</subject><subject>Computation</subject><subject>Earthquakes</subject><subject>Liquefaction</subject><subject>Magnitude scaling factors</subject><subject>Scaling</subject><subject>Scaling factors</subject><subject>Seismic activity</subject><subject>Seismic response</subject><subject>Seismology</subject><subject>Studies</subject><subject>Variation</subject><issn>0267-7261</issn><issn>1879-341X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqFUMtO3DAUtRCVGCifgGSJLUn9SOxkhdAAbSXULlokxMa6sW-Ih5AMtgPi7-vRsO_qvs5D9xByxlnJGVffNmWc_eg-plLksWRtyarqgKx4o9tCVvzhkKyYULrQQvEjchzjhjGueaNW5P3PFpKHkb5B8LmbJzr39AWeJp8WhzRaGP30RHuwaQ6RuiXsxjQgzWaMXkPoPY6OwuR2G07XQ_Ax2WEJdrigv_CdPiKM-XxBEUIaXhd4xviVfOlhjHj6WU_I_e3N3_WP4u7395_rq7sCKq1T0YEVTqimbzlrrYOuriuwSndSC6m7WtZSI1rQrVKgnZCi0w577lA2oDonT8j5Xncb5tcFYzKbeQlTtjS8rRWTohEyo-o9yoY5xoC92Qb_AuHDcGZ2GZuN-czY7DI2rDU548y73PMwv_DmMZhoPU4WnQ9ok3Gz_4_CPz6aiKc</recordid><startdate>20161201</startdate><enddate>20161201</enddate><creator>Carter, W.L.</creator><creator>Green, R.A.</creator><creator>Bradley, B.A.</creator><creator>Wotherspoon, L.M.</creator><creator>Cubrinovski, M.</creator><general>Elsevier Ltd</general><general>Elsevier BV</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>KL.</scope><scope>KR7</scope><scope>SOI</scope></search><sort><creationdate>20161201</creationdate><title>Spatial variation of magnitude scaling factors during the 2010 Darfield and 2011 Christchurch, New Zealand, earthquakes</title><author>Carter, W.L. ; Green, R.A. ; Bradley, B.A. ; Wotherspoon, L.M. ; Cubrinovski, M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a477t-bac2d268f9109cdab554ac67b37237b53537eeca7966a7d232b7def1de38a6bd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Canterbury earthquakes</topic><topic>Christchurch</topic><topic>Computation</topic><topic>Earthquakes</topic><topic>Liquefaction</topic><topic>Magnitude scaling factors</topic><topic>Scaling</topic><topic>Scaling factors</topic><topic>Seismic activity</topic><topic>Seismic response</topic><topic>Seismology</topic><topic>Studies</topic><topic>Variation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Carter, W.L.</creatorcontrib><creatorcontrib>Green, R.A.</creatorcontrib><creatorcontrib>Bradley, B.A.</creatorcontrib><creatorcontrib>Wotherspoon, L.M.</creatorcontrib><creatorcontrib>Cubrinovski, M.</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Soil dynamics and earthquake engineering (1984)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Carter, W.L.</au><au>Green, R.A.</au><au>Bradley, B.A.</au><au>Wotherspoon, L.M.</au><au>Cubrinovski, M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatial variation of magnitude scaling factors during the 2010 Darfield and 2011 Christchurch, New Zealand, earthquakes</atitle><jtitle>Soil dynamics and earthquake engineering (1984)</jtitle><date>2016-12-01</date><risdate>2016</risdate><volume>91</volume><spage>175</spage><epage>186</epage><pages>175-186</pages><issn>0267-7261</issn><eissn>1879-341X</eissn><abstract>The combination of well-documented liquefaction response during the Darfield and Christchurch, New Zealand, earthquakes, densely-recorded ground motions for the events, and detailed subsurface characterization provides an unprecedented opportunity to investigate the significance of the spatial variation of magnitude scaling factors (MSF) on liquefaction triggering. Towards this end, MSF were computed at 15 SMS sites across Christchurch and its surroundings using two established approaches. Trends in the spatial variation of the MSF computed using number of equivalent cycles (neq) from both approaches were similar, with the spatial variation being more significant for the Christchurch earthquake than the Darfield earthquake. However, there was no consistent trend for regions with lower computed MSF having experienced more severe or widespread liquefaction. Additionally, there is a general correlation between MSF and amax, but because amax ranges more widely than MSF it has a greater influence on the resulting seismic demand imposed on the soil than MSF does. Nevertheless, the spatial variation of the MSF is deemed significant enough that it warrants being considered for incorporation into future variants of simplified liquefaction evaluation procedures. •This study investigates the spatial variation of magnitude scaling factors.•Two well-documented earthquakes in New Zealand were used to investigate the spatial variation of MSF.•A general trend was identified that MSF correlate with PGA.•From a seismic demand perspective, PGA is more influential on liquefaction triggering than MSF.</abstract><cop>Barking</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.soildyn.2016.09.044</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0267-7261
ispartof Soil dynamics and earthquake engineering (1984), 2016-12, Vol.91, p.175-186
issn 0267-7261
1879-341X
language eng
recordid cdi_proquest_journals_1956032823
source ScienceDirect Freedom Collection
subjects Canterbury earthquakes
Christchurch
Computation
Earthquakes
Liquefaction
Magnitude scaling factors
Scaling
Scaling factors
Seismic activity
Seismic response
Seismology
Studies
Variation
title Spatial variation of magnitude scaling factors during the 2010 Darfield and 2011 Christchurch, New Zealand, earthquakes
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T19%3A39%3A28IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Spatial%20variation%20of%20magnitude%20scaling%20factors%20during%20the%202010%20Darfield%20and%202011%20Christchurch,%20New%20Zealand,%20earthquakes&rft.jtitle=Soil%20dynamics%20and%20earthquake%20engineering%20(1984)&rft.au=Carter,%20W.L.&rft.date=2016-12-01&rft.volume=91&rft.spage=175&rft.epage=186&rft.pages=175-186&rft.issn=0267-7261&rft.eissn=1879-341X&rft_id=info:doi/10.1016/j.soildyn.2016.09.044&rft_dat=%3Cproquest_cross%3E1956032823%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a477t-bac2d268f9109cdab554ac67b37237b53537eeca7966a7d232b7def1de38a6bd3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1956032823&rft_id=info:pmid/&rfr_iscdi=true