Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/117979
DC FieldValueLanguage
dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorWang, Ten_US
dc.creatorWu, Men_US
dc.creatorYin, ZYen_US
dc.creatorChen, XGen_US
dc.date.accessioned2026-03-10T05:45:15Z-
dc.date.available2026-03-10T05:45:15Z-
dc.identifier.issn0266-352Xen_US
dc.identifier.urihttp://hdl.handle.net/10397/117979-
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectCarbon dioxideen_US
dc.subjectDiscrete element methoden_US
dc.subjectPhase transitionen_US
dc.subjectPore cloggingen_US
dc.subjectVolume of fluiden_US
dc.titleNumerical analysis of liquid-gas phase transition effects on pore clogging and particle transporten_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume192en_US
dc.identifier.doi10.1016/j.compgeo.2025.107863en_US
dcterms.abstractThis study investigates the impact of liquid–gas phase transition on pore clogging during supercritical carbon dioxide (SC-CO<inf>2</inf>) geological storage. To address this, we developed a pore-scale CFD-DEM-VOF model incorporating phase transition. It is capable of simulating phase transition processes in multiphase flows and their subsequent effects on particle behavior, as well as the resulting coupled dynamics of particle transport, pore clogging, and unclogging. Throughout these simulations, drag forces, contact forces on particles, and the evolution of the flow field were meticulously tracked and analyzed. Crucially, the research employed both constant-velocity and constant-pressure inlet boundary conditions, using non-phase-transition models as controls for comparison. Analysis of the results revealed that phase transition influences particle behavior through two distinct mechanisms. Firstly, volume expansion accelerates particle transport towards pore outlets. Conversely, and simultaneously, phase transition enhances turbulence and vortex formation within the flow field. This secondary effect loosens particle clusters, slows their movement, and traps particles within swirling flow structures that impede passage. Under constant-velocity boundary conditions, higher phase transition rates generally promote faster particle transport through pores. In contrast, under constant-pressure conditions, phase transition reduces the inlet flow velocity at higher rates. Due to the low viscosity and density of gas, it is less effective at carrying particles through pores under these conditions. As a result, moderate phase transition rates yield the highest particle transport rates in the constant-pressure inlet model.en_US
dcterms.accessRightsembargoed accessen_US
dcterms.bibliographicCitationComputers and geotechnics, Apr. 2026, v. 192, 107863en_US
dcterms.isPartOfComputers and geotechnicsen_US
dcterms.issued2026-04-
dc.identifier.scopus2-s2.0-105025397499-
dc.identifier.eissn1873-7633en_US
dc.identifier.artn107863en_US
dc.description.validate202603 bchyen_US
dc.description.oaNot applicableen_US
dc.identifier.SubFormIDG001153/2026-01-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThis study was supported by National Natural Science Foundation of China (Grant No.: 52408394), General Research Fund Grant No. PolyU 15227624 from the Research Grants Council of the Hong Kong SAR, and State Key Laboratory of Intelligent Construction and Healthy Operation and Maintenance of Deep Underground Engineering (Grant No.: SDGZ2504). The authors are grateful to the anonymous reviewers and the editor for their valuable suggestions to improve the manuscript.en_US
dc.description.pubStatusPublisheden_US
dc.date.embargo2028-04-30en_US
dc.description.oaCategoryGreen (AAM)en_US
Appears in Collections:Journal/Magazine Article
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Embargo End Date 2028-04-30
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