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dc.contributor.authorJiang, Mingjing
dc.contributor.authorShen, Zhifu
dc.contributor.authorZhou, Wei
dc.contributor.authorArroyo Alvarez de Toledo, Marcos
dc.contributor.authorZhang, Wangcheng
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria Civil i Ambiental
dc.date.accessioned2018-11-20T15:22:21Z
dc.date.available2019-12-01T01:25:53Z
dc.date.issued2018-11
dc.identifier.citationJiang, M., Shen, Z., Zhou, W., Arroyo, M., Zhang, W. Coupled CFD–DEM method for undrained biaxial shear test of methane hydrate bearing sediments. "Granular matter", Novembre 2018, vol. 20, núm. 4, p. 1-17.
dc.identifier.issn1434-7636
dc.identifier.otherhttps://www.researchgate.net/publication/327103114_Coupled_CFD-DEM_method_for_undrained_biaxial_shear_test_of_methane_hydrate_bearing_sediments
dc.identifier.urihttp://hdl.handle.net/2117/124782
dc.descriptionThe final publication is available at Springer via http://dx.doi.org/10.1007/s10035-018-0826-x
dc.description.abstractMethane hydrate (MH), a potential source of future energy, is extensively deposited in marine sediments. It is essential to understand the mechanical properties of methane hydrate bearing sediments (MHBS) for applications relevant to mining and geotechnical engineering. This study aims to investigate the undrained shear strength of MHBS through coupled computational fluid dynamics and discrete element method (CFD–DEM) numerical approach. The Tait’s fluid state equation is implemented into the Navier–Stokes equation-based CFD, while the DEM is used to model granular particle system of MHBS. The CFD–DEM tool is first verified by two typical geomechanics problems where analytical solutions are available. The simulations show that the stress–strain behavior of MHBS depends on temperature, back pressure and MH saturation, as observed in reported experimental results. The presence of MH alters the hardening response of clean sand into softening response due to the bonding effects of MH. The friction angles and cohesions described by total stress and effective stress both increase as the back pressure and MH saturation increase or the temperature drops. There is significant localization in MH bond breakage events but no localization effect is observed in fluid flow and excess pore pressure distribution. This is because fluid is mostly controlled by the boundary conditions instead of specific fluid–particle interactions locally in the simulated quasi-static loading.
dc.format.extent17 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de sòls
dc.subject.lcshSoil mechanics -- Mathematical models
dc.subject.otherMethane hydrate bearing sediments Undrained shear test Coupled CFD–DEM method Excess pore pressure
dc.titleCoupled CFD–DEM method for undrained biaxial shear test of methane hydrate bearing sediments
dc.typeArticle
dc.subject.lemacMecànica dels sòls -- Mètodes numèrics
dc.contributor.groupUniversitat Politècnica de Catalunya. MSR - Mecànica del Sòls i de les Roques
dc.identifier.doi10.1007/s10035-018-0826-x
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttps://link.springer.com/article/10.1007/s10035-018-0826-x
dc.rights.accessOpen Access
local.identifier.drac23516714
dc.description.versionPostprint (author's final draft)
dc.relation.projectidinfo:eu-repo/grantAgreement/EC/FP7/294976/EU/geohazards and geomechanics/GEO
local.citation.authorJiang, M.; Shen, Z.; Zhou, W.; Arroyo, M.; Zhang, W.
local.citation.publicationNameGranular matter
local.citation.volume20
local.citation.number4
local.citation.startingPage1
local.citation.endingPage17


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