Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/111744
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorSun, L-
dc.creatorTang, X-
dc.creatorAboayanah, KR-
dc.creatorZhao, Q-
dc.creatorLiu, Q-
dc.creatorGrasselli, G-
dc.date.accessioned2025-03-14T03:56:48Z-
dc.date.available2025-03-14T03:56:48Z-
dc.identifier.issn1674-7755-
dc.identifier.urihttp://hdl.handle.net/10397/111744-
dc.language.isoenen_US
dc.publisher科学出版社 (Kexue Chubanshe,Science Press)en_US
dc.rights© 2024 Institute of Rock and Soil Mechanics, Chinese Academy of Sciences. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).en_US
dc.rightsThe following publication Sun, L., Tang, X., Aboayanah, K. R., Zhao, Q., Liu, Q., & Grasselli, G. (2024). A coupled cryogenic thermo-hydro-mechanical model for frozen medium: Theory and implementation in FDEM. Journal of Rock Mechanics and Geotechnical Engineering, 16(11), 4335-4353 is available at https://doi.org/10.1016/j.jrmge.2023.09.007.en_US
dc.subjectCombined finite-discrete element method (FDEM)en_US
dc.subjectFrost heaveen_US
dc.subjectHeat transferen_US
dc.subjectLow temperatureen_US
dc.subjectThermo-hydro-mechanical (THM) couplingen_US
dc.subjectWater migrationen_US
dc.titleA coupled cryogenic thermo-hydro-mechanical model for frozen medium : theory and implementation in FDEMen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage4335-
dc.identifier.epage4353-
dc.identifier.volume16-
dc.identifier.issue11-
dc.identifier.doi10.1016/j.jrmge.2023.09.007-
dcterms.abstractThis paper presents the development of a coupled modeling approach to simulate cryogenic thermo-hydro-mechanical (THM) processes associated with a freezing medium, which is then implemented in the combined finite-discrete element method code (FDEM) for multi-physics simulation. The governing equations are deduced based on energy and mass conservation, and static equilibrium equations, considering water/ice phase change, where the strong couplings between multi-fields are supplemented by critical coupling parameters (e.g. unfrozen water content, permeability, and thermal conductivity). The proposed model is validated against laboratory and field experiments. Results show that the cryogenic THM model can well predict the evolution of strongly coupled processes observed in frozen media (e.g. heat transfer, water migration, and frost heave deformation), while also capturing, as emergent properties of the model, important phenomena (e.g. latent heat, cryogenic suction, ice expansion and distinct three-zone distribution) caused by water/ice phase change at laboratory and field scales, which are difficult to be all revealed by existing THM models. The novel modeling framework presents a gateway to further understanding and predicting the multi-physical coupling behavior of frozen media in cold regions.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of rock mechanics and geotechnical engineering, Nov. 2024, v. 16, no. 11, p. 4335-4353-
dcterms.isPartOfJournal of rock mechanics and geotechnical engineering-
dcterms.issued2024-11-
dc.identifier.scopus2-s2.0-85199071343-
dc.identifier.eissn2589-0417-
dc.description.validate202503 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNatural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grants; NSERC/Energi Simulation Industrial Research Chair program; Lassonde International Graduate Scholarship in Mining at the University of Toronto; FCE Start-up Fund for New Recruits at the Hong Kong Polytechnic Universityen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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