Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/101861
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorBentil, OTen_US
dc.creatorZhou, Cen_US
dc.creatorBentil, OTen_US
dc.creatorZhou, Cen_US
dc.date.accessioned2023-09-20T04:40:54Z-
dc.date.available2023-09-20T04:40:54Z-
dc.identifier.issn1090-0241en_US
dc.identifier.urihttp://hdl.handle.net/10397/101861-
dc.language.isoenen_US
dc.publisherHong Kong Polytechnic University, Department of Civil and Structural Engineeringen_US
dc.rights© 2022 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)GT.1943-5606.0002822.en_US
dc.subjectTemperatureen_US
dc.subjectThermal cyclesen_US
dc.subjectElastic shear modulusen_US
dc.subjectLateritic soilen_US
dc.subjectClaysen_US
dc.titleEffects of temperature and thermal cycles on the elastic shear modulus of saturated clayen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume148en_US
dc.identifier.issue7en_US
dc.identifier.doi10.1061/(ASCE)GT.1943-5606.0002822en_US
dcterms.abstractThermomechanical behavior of soils has attracted great attention in recent years because of its great importance in some emerging geotechnical applications such as energy piles. So far, the thermoplasticity (e.g., the influence of temperature on the yield surface) has been well understood, but the thermoelasticity has not been purposely studied. In this study, a temperature-controlled oedometer equipped with bender elements was developed and then used to mainly investigate effects of temperature and thermal cycles on the elastic shear modulus (G0) of a saturated lateritic clay. In addition, one test was performed on kaolin clay to investigate the influence of thermal cycles on G0. Two types of thermomechanical paths were considered at different temperatures and stresses, including constant-temperature loading–unloading and constant-stress cyclic heating–cooling. Results from these tests consistently reveal that at a given stress, G0 is smaller at a higher temperature. This can be attributed to the reduction of interparticle force during the heating of saturated clay, according to the double layer theories. Furthermore, G0 of the lateritic clay increases by about 12% and 16% after four thermal cycles for overconsolidated and normally consolidated specimens, respectively. This can be due to soil densification and particle rearrangement during the heating–cooling cycles. These results are useful for improving the modeling of thermoelasticity and also for the analysis of thermally active structures such as energy piles.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geotechnical and geoenvironmental engineering, July 2022, v. 148, no. 7, 06022006en_US
dcterms.isPartOfJournal of geotechnical and geoenvironmental engineeringen_US
dcterms.issued2022-07-
dc.identifier.eissn1943-5606en_US
dc.identifier.artn06022006en_US
dc.description.validate202309 bcchen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumbera2432-
dc.identifier.SubFormID47672-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNSFCen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryGreen (AAM)en_US
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