Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/105895
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorZhan, Z-
dc.creatorZhou, C-
dc.date.accessioned2024-04-23T04:32:05Z-
dc.date.available2024-04-23T04:32:05Z-
dc.identifier.urihttp://hdl.handle.net/10397/105895-
dc.description8th International Conference on Unsaturated Soils (UNSAT 2023), Milos, Greece, May 2-5, 2023en_US
dc.language.isoenen_US
dc.publisherEDP Sciencesen_US
dc.rights© The Authors, published by EDP Sciences. This is an open access article distributed under the terms of the Creative Commons Attribution License 4.0 (http://creativecommons.org/licenses/by/4.0/).en_US
dc.rightsThe following publication Zhan, Z., & Zhou, C. (2023). SimuIating landsIides using two-phase two-point material point method. E3S Web of Conf., 382, 13009 is available at https://doi.org/10.1051/e3sconf/202338213009.en_US
dc.titleSimuIating landsIides using two-phase two-point material point methoden_US
dc.typeConference Paperen_US
dc.identifier.volume382-
dc.identifier.doi10.1051/e3sconf/202338213009-
dcterms.abstractMaterial point method (MPM) is an effective numerical method for large-deformation analysis under unsaturated conditions. In the previous studies, water retention ability and permeability function were assumed to be Independent of soil deformation. Besides, most studies used a single set of material points, so some processes (e.g., the infiltration of free water into unsaturated soil) cannot be modelled. Thereby, a two-point MPM approach has been extended from saturated to unsaturated soils. The required information of soild and liquid phases is carried by two individual sets of material points, with the assumption of zero pore air pressure. GIMP is applied for space discretisation. In the modelling of hydraulic behaviour, the porosity-dependent water retention curve and permeability function are incorporated. A centrifuge test about rainfall-induced unsaturated soil slope failure is simulated to investigate the influence of the porosity-dependent water retention curve and permeability function. Parametric studies demonstrate soil parameters for water retention behaviour and shear strength play significant roles in the slope failure mechanisms.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationE3S Web of conferencesk, 2023, v. 382, 13009-
dcterms.isPartOfE3S Web of conferences-
dcterms.issued2023-
dc.identifier.scopus2-s2.0-85159272440-
dc.relation.conferenceInternational Conference on Unsaturated Soils [UNSAT]-
dc.identifier.eissn2267-1242-
dc.identifier.artn13009-
dc.description.validate202404 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.fundingSourceRGCen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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