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Study of pore pressure variation during liquefaction using two constitutive models for sand
Numerical analyses of liquefiable sand are presented in this paper. Liquefaction phenomenon is an undrained response of saturated sandy soils when they are subjected to static or dynamic loads. A fully coupled dynamic computer code is developed to predict the liquefaction potential of a saturated sa...
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Published in: | Soil dynamics and earthquake engineering (1984) 2007, Vol.27 (1), p.60-72 |
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container_title | Soil dynamics and earthquake engineering (1984) |
container_volume | 27 |
creator | Taiebat, Mahdi Shahir, Hadi Pak, Ali |
description | Numerical analyses of liquefiable sand are presented in this paper. Liquefaction phenomenon is an undrained response of saturated sandy soils when they are subjected to static or dynamic loads. A fully coupled dynamic computer code is developed to predict the liquefaction potential of a saturated sandy layer. Coupled dynamic field equations of extended Biot's theory with
u–
P formulation are used to determine the responses of pore fluid and soil skeleton. Generalized Newmark method is employed for integration in time. The soil behavior is modelled by two constitutive models; a critical state two-surface plasticity model, and a densification model. A class ‘B’ analysis of a centrifuge experiment is performed to simulate the dynamic response of level ground sites. The results of the numerical analyses demonstrate the capability of the critical sate two-surface plasticity model in producing pore pressures that are consistent with observations of the behavior of liquefiable sand in the centrifuge test. |
doi_str_mv | 10.1016/j.soildyn.2006.03.004 |
format | article |
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u–
P formulation are used to determine the responses of pore fluid and soil skeleton. Generalized Newmark method is employed for integration in time. The soil behavior is modelled by two constitutive models; a critical state two-surface plasticity model, and a densification model. A class ‘B’ analysis of a centrifuge experiment is performed to simulate the dynamic response of level ground sites. The results of the numerical analyses demonstrate the capability of the critical sate two-surface plasticity model in producing pore pressures that are consistent with observations of the behavior of liquefiable sand in the centrifuge test.</description><identifier>ISSN: 0267-7261</identifier><identifier>EISSN: 1879-341X</identifier><identifier>DOI: 10.1016/j.soildyn.2006.03.004</identifier><identifier>CODEN: SDEEEJ</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Bounding surface ; Constitutive model ; Critical state ; Densification ; Earth sciences ; Earth, ocean, space ; Earthquakes, seismology ; Engineering and environment geology. Geothermics ; Engineering geology ; Exact sciences and technology ; Finite element ; Fully coupled analysis ; Internal geophysics ; Liquefaction ; Natural hazards: prediction, damages, etc ; Plasticity</subject><ispartof>Soil dynamics and earthquake engineering (1984), 2007, Vol.27 (1), p.60-72</ispartof><rights>2006 Elsevier Ltd</rights><rights>2006 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a506t-e6abb78bccde7d231e85ffcbbb70bfb23ff32dfdf17de5b51add1f48a45324433</citedby><cites>FETCH-LOGICAL-a506t-e6abb78bccde7d231e85ffcbbb70bfb23ff32dfdf17de5b51add1f48a45324433</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,4010,27900,27901,27902</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=18126025$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Taiebat, Mahdi</creatorcontrib><creatorcontrib>Shahir, Hadi</creatorcontrib><creatorcontrib>Pak, Ali</creatorcontrib><title>Study of pore pressure variation during liquefaction using two constitutive models for sand</title><title>Soil dynamics and earthquake engineering (1984)</title><description>Numerical analyses of liquefiable sand are presented in this paper. Liquefaction phenomenon is an undrained response of saturated sandy soils when they are subjected to static or dynamic loads. A fully coupled dynamic computer code is developed to predict the liquefaction potential of a saturated sandy layer. Coupled dynamic field equations of extended Biot's theory with
u–
P formulation are used to determine the responses of pore fluid and soil skeleton. Generalized Newmark method is employed for integration in time. The soil behavior is modelled by two constitutive models; a critical state two-surface plasticity model, and a densification model. A class ‘B’ analysis of a centrifuge experiment is performed to simulate the dynamic response of level ground sites. The results of the numerical analyses demonstrate the capability of the critical sate two-surface plasticity model in producing pore pressures that are consistent with observations of the behavior of liquefiable sand in the centrifuge test.</description><subject>Bounding surface</subject><subject>Constitutive model</subject><subject>Critical state</subject><subject>Densification</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Earthquakes, seismology</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Engineering geology</subject><subject>Exact sciences and technology</subject><subject>Finite element</subject><subject>Fully coupled analysis</subject><subject>Internal geophysics</subject><subject>Liquefaction</subject><subject>Natural hazards: prediction, damages, etc</subject><subject>Plasticity</subject><issn>0267-7261</issn><issn>1879-341X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNqFkEtLLDEQhYMoOI7-BCGb667bPLrT7UpErg8QXKgguAjppCIZejpjKj0y_96eOwN36aqKwzl1io-Qc85Kzri6XJQYQ-82QykYUyWTJWPVAZnxtrkqZMXfD8mMCdUUjVD8mJwgLhjjDW_VjHy85NFtaPR0FRPQVQLEcVrWJgWTQxyoG1MYPmkfvkbwxv7TRtxK-TtSGwfMIY85rIEuo4MeqY-JohncKTnypkc42885ebv7-3r7UDw93z_e3jwVpmYqF6BM1zVtZ62DxgnJoa29t90kss53QnovhfPO88ZB3dXcOMd91ZqqlqKqpJyTi93dVYrTk5j1MqCFvjcDxBG1aNuKM7U11jujTRExgderFJYmbTRneotSL_Qepd6i1EzqCeWU-7MvMGhN75MZbMD_4ZYLxUQ9-a53vokCrAMkjTbAYMGFBDZrF8MvTT-OzJCV</recordid><startdate>2007</startdate><enddate>2007</enddate><creator>Taiebat, Mahdi</creator><creator>Shahir, Hadi</creator><creator>Pak, Ali</creator><general>Elsevier Ltd</general><general>Elsevier Science</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SC</scope><scope>7SM</scope><scope>8FD</scope><scope>FR3</scope><scope>JQ2</scope><scope>KR7</scope><scope>L7M</scope><scope>L~C</scope><scope>L~D</scope></search><sort><creationdate>2007</creationdate><title>Study of pore pressure variation during liquefaction using two constitutive models for sand</title><author>Taiebat, Mahdi ; Shahir, Hadi ; Pak, Ali</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a506t-e6abb78bccde7d231e85ffcbbb70bfb23ff32dfdf17de5b51add1f48a45324433</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>Bounding surface</topic><topic>Constitutive model</topic><topic>Critical state</topic><topic>Densification</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Earthquakes, seismology</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Engineering geology</topic><topic>Exact sciences and technology</topic><topic>Finite element</topic><topic>Fully coupled analysis</topic><topic>Internal geophysics</topic><topic>Liquefaction</topic><topic>Natural hazards: prediction, damages, etc</topic><topic>Plasticity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Taiebat, Mahdi</creatorcontrib><creatorcontrib>Shahir, Hadi</creatorcontrib><creatorcontrib>Pak, Ali</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Computer and Information Systems Abstracts</collection><collection>Earthquake Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>ProQuest Computer Science Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Computer and Information Systems Abstracts Academic</collection><collection>Computer and Information Systems Abstracts Professional</collection><jtitle>Soil dynamics and earthquake engineering (1984)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Taiebat, Mahdi</au><au>Shahir, Hadi</au><au>Pak, Ali</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Study of pore pressure variation during liquefaction using two constitutive models for sand</atitle><jtitle>Soil dynamics and earthquake engineering (1984)</jtitle><date>2007</date><risdate>2007</risdate><volume>27</volume><issue>1</issue><spage>60</spage><epage>72</epage><pages>60-72</pages><issn>0267-7261</issn><eissn>1879-341X</eissn><coden>SDEEEJ</coden><abstract>Numerical analyses of liquefiable sand are presented in this paper. Liquefaction phenomenon is an undrained response of saturated sandy soils when they are subjected to static or dynamic loads. A fully coupled dynamic computer code is developed to predict the liquefaction potential of a saturated sandy layer. Coupled dynamic field equations of extended Biot's theory with
u–
P formulation are used to determine the responses of pore fluid and soil skeleton. Generalized Newmark method is employed for integration in time. The soil behavior is modelled by two constitutive models; a critical state two-surface plasticity model, and a densification model. A class ‘B’ analysis of a centrifuge experiment is performed to simulate the dynamic response of level ground sites. The results of the numerical analyses demonstrate the capability of the critical sate two-surface plasticity model in producing pore pressures that are consistent with observations of the behavior of liquefiable sand in the centrifuge test.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.soildyn.2006.03.004</doi><tpages>13</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Bounding surface Constitutive model Critical state Densification Earth sciences Earth, ocean, space Earthquakes, seismology Engineering and environment geology. Geothermics Engineering geology Exact sciences and technology Finite element Fully coupled analysis Internal geophysics Liquefaction Natural hazards: prediction, damages, etc Plasticity |
title | Study of pore pressure variation during liquefaction using two constitutive models for sand |
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