Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/116206
DC FieldValueLanguage
dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorPeng, Men_US
dc.creatorYin, ZYen_US
dc.date.accessioned2025-12-02T02:25:05Z-
dc.date.available2025-12-02T02:25:05Z-
dc.identifier.issn0266-352Xen_US
dc.identifier.urihttp://hdl.handle.net/10397/116206-
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectDrainage effecten_US
dc.subjectModified cam-clayen_US
dc.subjectOffshore foundationsen_US
dc.subjectPlate anchorsen_US
dc.subjectRate effecten_US
dc.titleNumerical investigations into the drainage effects on the behaviors of plate anchors under unidirectional and combined loadingsen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume188en_US
dc.identifier.doi10.1016/j.compgeo.2025.107624en_US
dcterms.abstractThis study presents one of the first systematic investigations into the drainage-dependent behaviors of a deeply embedded plate anchor under unidirectional and combined loadings using finite element analysis. The hydro-mechanical soil response is modeled via Biot's consolidation theory coupled with the Modified Cam-Clay model, incorporating a regularization scheme to address numerical instability near the drained regime and to robustly capture anchor–soil detachment. Results show that anchor capacities are strongly dependent on drainage conditions and are predominantly governed by the normal component under combined loading. Failure mechanisms vary significantly with drainage and are generally localized around the anchor, except in drained penetration, which induces notable mudline settlement. Detachment at the anchor–soil interface arises under near-drained conditions across all loading paths and progressively vanishes with increasing loading rate due to the mobilization of interfacial suction. A typical transition from detachment to attachment is observed near a dimensionless velocity of V = 1. A quantitative method is proposed to identify threshold velocities separating drained, partially drained, and undrained regimes. Both thresholds are identified for various unidirectional and combined loading paths and exhibit strong path dependency, attributed to differences in pore pressure generation and dissipation mechanisms across loading scenarios.en_US
dcterms.accessRightsembargoed accessen_US
dcterms.bibliographicCitationComputers and geotechnics, Dec. 2025, v. 188, 107624en_US
dcterms.isPartOfComputers and geotechnicsen_US
dcterms.issued2025-12-
dc.identifier.scopus2-s2.0-105014805457-
dc.identifier.eissn1873-7633en_US
dc.identifier.artn107624en_US
dc.description.validate202512 bcjzen_US
dc.description.oaNot applicableen_US
dc.identifier.SubFormIDG000375/2025-10-
dc.description.fundingSourceRGCen_US
dc.description.fundingTextThis research was financially supported by the Research Grants Council (RGC) of Hong Kong Special Administrative Region Government (HKSARG) of China (Grant No. 15217220, 15232224).en_US
dc.description.pubStatusPublisheden_US
dc.date.embargo2027-12-31en_US
dc.description.oaCategoryGreen (AAM)en_US
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