Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/95194
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorZhou, Cen_US
dc.creatorFong, KYen_US
dc.creatorNg, CWWen_US
dc.date.accessioned2022-09-14T08:32:37Z-
dc.date.available2022-09-14T08:32:37Z-
dc.identifier.issn0363-9061en_US
dc.identifier.urihttp://hdl.handle.net/10397/95194-
dc.language.isoenen_US
dc.publisherJohn Wiley & Sonsen_US
dc.rights© 2017 John Wiley & Sons, Ltd.en_US
dc.rightsThis is the peer reviewed version of the following article: Zhou, C., Fong, K. Y., and Ng, C. W. W. (2017) A new bounding surface model for thermal cyclic behaviour. Int. J. Numer. Anal. Meth. Geomech., 41: 1656– 1666. doi: 10.1002/nag.2688., which has been published in final form at https://doi.org/10.1002/nag.2688. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions. This article may not be enhanced, enriched or otherwise transformed into a derivative work, without express permission from Wiley or by statutory rights under applicable legislation. Copyright notices must not be removed, obscured or modified. The article must be linked to Wiley’s version of record on Wiley Online Library and any embedding, framing or otherwise making available the article or pages thereof by third parties from platforms, services and websites other than Wiley Online Library must be prohibited.en_US
dc.subjectConstitutive relationsen_US
dc.subjectCyclicen_US
dc.subjectThermal effectsen_US
dc.titleA new bounding surface model for thermal cyclic behaviouren_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage1656en_US
dc.identifier.epage1666en_US
dc.identifier.volume41en_US
dc.identifier.issue16en_US
dc.identifier.doi10.1002/nag.2688en_US
dcterms.abstractTo accurately predict soil volume changes under thermal cycles is of great importance for analysing the performance of many earth structures such as the energy pile and energy storage system. Most of the existing thermo-mechanical models focus on soil behaviour under monotonic thermal loading only, and they are not able to capture soil volume changes under thermal cycles. In this study, a constitutive model is proposed to simulate volume changes of saturated soil subjected to cyclic heating and cooling. Two surfaces are defined and used: a bounding surface and a memory surface. The bounding surface and memory surface are mainly controlled by the preconsolidation pressure (a function of plastic volumetric strain) and the maximum stress experienced by the soil, respectively. Under thermal cycles, the distance of the two surfaces and plastic modulus increase with an accumulation of plastic strain. By adopting the double surface concept, a new elastoplastic model is derived from an existing single bounding surface thermo-mechanical model. Comparisons between model predictions and experimental results reveal that the proposed model is able to capture soil volume changes under thermal cycles well. The plastic strain accumulates under thermal cycles, but at a decreasing rate, until stabilization.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationInternational journal for numerical and analytical methods in geomechanics, Nov. 2017, v. 41, no. 16, p. 1656-1666en_US
dcterms.isPartOfInternational journal for numerical and analytical methods in geomechanicsen_US
dcterms.issued2017-11-
dc.identifier.scopus2-s2.0-85015085719-
dc.identifier.eissn1096-9853en_US
dc.description.validate202209 bcvcen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberRGC-B2-1188-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Natural Science Foundation of Chinaen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryGreen (AAM)en_US
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