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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorXiao, Yen_US
dc.creatorWang, Cen_US
dc.creatorZhang, Zen_US
dc.creatorLiu, Hen_US
dc.creatorYin, ZYen_US
dc.date.accessioned2023-03-06T01:18:20Z-
dc.date.available2023-03-06T01:18:20Z-
dc.identifier.issn1532-3641en_US
dc.identifier.urihttp://hdl.handle.net/10397/97419-
dc.language.isoenen_US
dc.publisherAmerican Society of Civil Engineersen_US
dc.rights© 2021 American Society of Civil Engineers.en_US
dc.rightsThis material may be downloaded for personal use only. Any other use requires prior permission of the American Society of Civil Engineers. This material may be found at https://doi.org/10.1061/(ASCE)GM.1943-5622.0001987.en_US
dc.subjectConstitutive modelen_US
dc.subjectCritical stateen_US
dc.subjectDilatancyen_US
dc.subjectParticle breakageen_US
dc.subjectPlasticityen_US
dc.subjectState parameteren_US
dc.titleConstitutive modeling for two sands under high pressureen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume21en_US
dc.identifier.issue5en_US
dc.identifier.doi10.1061/(ASCE)GM.1943-5622.0001987en_US
dcterms.abstractParticle breakage is a typical characteristic of crushable granular soil under high pressure, which has great effects on its stress-strain behaviors. The phenomenon of the critical state line (CSL) shifting downward in the compression plane caused by particle breakage was depicted by a breakage-dependent critical state plane (BCSP). Particle breakage was incorporated into a void ratio-pressure state parameter to modify Rowe's stress-dilatancy equation, and then, the state parameter was incorporated into the bounding stress ratio and plastic modulus. Due to the impact of high pressure on particle breakage, the pressure-dependent plastic modulus parameters were introduced. A breakage-dependent bounding surface plasticity model was proposed to capture the influence of particle breakage on the state-dependent stress-strain behaviors for silica and coral sands, and the transition of complex breakage-dependent critical states resulted from the competition between the contraction due to particle breakage and the dilatancy due to particle rearrangement.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationInternational journal of geomechanics, May 2021, v. 21, no. 5, 04021042en_US
dcterms.isPartOfInternational journal of geomechanicsen_US
dcterms.issued2021-05-
dc.identifier.scopus2-s2.0-85101245412-
dc.identifier.eissn1943-5622en_US
dc.identifier.artn04021042en_US
dc.description.validate202203 bcfcen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberCEE-0350-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNSFC; Natural Science Foundation of Chongqingen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS45843029-
dc.description.oaCategoryGreen (AAM)en_US
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