A coupled cryogenic thermo-hydro-mechanical model for frozen medium: Theory and implementation in FDEM
被引:16
作者:
Sun, Lei
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Univ Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, Canada
Wuhan Univ, Sch Civil Engn, Wuhan 430072, Peoples R ChinaUniv Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, Canada
Sun, Lei
[1
,2
]
Tang, Xuhai
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机构:
Wuhan Univ, Sch Civil Engn, Wuhan 430072, Peoples R ChinaUniv Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, Canada
Tang, Xuhai
[2
]
Aboayanah, Kareem Ramzy
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Univ Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, CanadaUniv Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, Canada
Aboayanah, Kareem Ramzy
[1
]
Zhao, Qi
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机构:
Hong Kong Polytech Univ, Dept Civil & Environm Engn, Hung Hom, Hong Kong, Peoples R ChinaUniv Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, Canada
Zhao, Qi
[3
]
Liu, Quansheng
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Wuhan Univ, Sch Civil Engn, Wuhan 430072, Peoples R ChinaUniv Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, Canada
Liu, Quansheng
[2
]
Grasselli, Giovanni
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Univ Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, CanadaUniv Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, Canada
Grasselli, Giovanni
[1
]
机构:
[1] Univ Toronto, Dept Civil & Mineral Engn, Toronto, ON M5S 1A4, Canada
[2] Wuhan Univ, Sch Civil Engn, Wuhan 430072, Peoples R China
[3] Hong Kong Polytech Univ, Dept Civil & Environm Engn, Hung Hom, Hong Kong, Peoples R China
This paper presents the development of a coupled modeling approach to simulate cryogenic thermohydro-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. (c) 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/).
机构:
Delft Univ Technol, Fac Civil Engn & Geosci, POB 5048, NL-2600 GA Delft, NetherlandsDelft Univ Technol, Fac Civil Engn & Geosci, POB 5048, NL-2600 GA Delft, Netherlands
机构:
Delft Univ Technol, Fac Civil Engn & Geosci, POB 5048, NL-2600 GA Delft, NetherlandsDelft Univ Technol, Fac Civil Engn & Geosci, POB 5048, NL-2600 GA Delft, Netherlands