Please use this identifier to cite or link to this item: http://bura.brunel.ac.uk/handle/2438/7418
Full metadata record
DC FieldValueLanguage
dc.contributor.authorRohan, E-
dc.contributor.authorShaw, S-
dc.contributor.authorWheeler, MF-
dc.contributor.authorWhiteman, JR-
dc.date.accessioned2013-05-07T08:47:55Z-
dc.date.available2013-05-07T08:47:55Z-
dc.date.issued2013-
dc.identifier.citationComputer Methods in Applied Mechanics and Engineering, 260: 78-91, Jun 2013en_US
dc.identifier.issn0045-7825-
dc.identifier.issn1879-2138-
dc.identifier.urihttp://www.sciencedirect.com/science/article/pii/S0045782513000546en
dc.identifier.urihttp://bura.brunel.ac.uk/handle/2438/7418-
dc.descriptionThis is the post-print version of the Article. The official published version can be accessed from the link below - Copyright @ 2013 Elsevieren_US
dc.descriptionThis article has been made available through the Brunel Open Access Publishing Fund.-
dc.description.abstractWe propose two fully discrete mixed and Galerkin finite element approximations to a system of equations describing the slow flow of a slightly compressible single phase fluid in a viscoelastic porous medium. One of our schemes is the natural one for the backward Euler time discretization but, due to the viscoelasticity, seems to be stable only for small enough time steps. The other scheme contains a lagged term in the viscous stress and pressure evolution equations and this is enough to prove unconditional stability. For this lagged scheme we prove an optimal order a priori error estimate under ideal regularity assumptions and demonstrate the convergence rates by using a model problem with a manufactured solution. The model and numerical scheme that we present are a natural extension to ‘poroviscoelasticity’ of the poroelasticity equations and scheme studied by Philips and Wheeler in (for example) [Philip Joseph Philips, Mary F.Wheeler, Comput. Geosci. 11 (2007) 145–158] although — importantly — their algorithms and codes would need only minor modifications in order to include the viscous effects. The equations and algorithms presented here have application to oil reservoir simulations and also to the condition of hydrocephalus — ‘water on the brain’. An illustrative example is given demonstrating that even small viscoelastic effects can produce noticeable differences in long-time response. To the best of our knowledge this is the first time a mixed and Galerkin scheme has been analysed and implemented for viscoelastic porous media.en_US
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectPorous mediaen_US
dc.subjectViscoelasticityen_US
dc.subjectFinite element methoden_US
dc.subjectError estimatesen_US
dc.subjectTime steppingen_US
dc.subjectGeoengineeringen_US
dc.titleMixed and galerkin finite element approximation of flow in a linear viscoelastic porous mediumen_US
dc.typeArticleen_US
dc.identifier.doihttp://dx.doi.org/10.1016/j.cma.2013.03.003-
pubs.organisational-data/Brunel-
pubs.organisational-data/Brunel/Brunel Active Staff-
pubs.organisational-data/Brunel/Brunel Active Staff/School of Info. Systems, Comp & Maths-
pubs.organisational-data/Brunel/Brunel Active Staff/School of Info. Systems, Comp & Maths/Maths-
pubs.organisational-data/Brunel/University Research Centres and Groups-
pubs.organisational-data/Brunel/University Research Centres and Groups/School of Information Systems, Computing and Mathematics - URCs and Groups-
pubs.organisational-data/Brunel/University Research Centres and Groups/School of Information Systems, Computing and Mathematics - URCs and Groups/Brunel Institute of Computational Mathematics-
Appears in Collections:Publications
Brunel OA Publishing Fund
Dept of Mathematics Research Papers
Mathematical Sciences

Files in This Item:
File Description SizeFormat 
Fulltext.pdf484.12 kBAdobe PDFView/Open


Items in BURA are protected by copyright, with all rights reserved, unless otherwise indicated.