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dc.contributor.authorKlemetsdal, Øystein
dc.contributor.authorMøyner, Olav
dc.contributor.authorLie, Knut-Andreas
dc.date.accessioned2018-02-22T07:12:24Z
dc.date.available2018-02-22T07:12:24Z
dc.date.created2017-06-28T12:52:52Z
dc.date.issued2017
dc.identifier.isbn978-94-6282-209-2
dc.identifier.urihttp://hdl.handle.net/11250/2486279
dc.description.abstractModels of polymer flooding account for several processes such as concentration dependent viscosity, adsorption, incomplete mixing, inaccessible pore space, and reduced permeability effects, which altogether gives strongly coupled nonlinear systems that are challenging to solve numerically. Herein, we use a sequentially implicit solution strategy that splits the equation system into a pressure and a transport part. Our objective is to improve convergence rates for the transport subproblem, which contains many of the essential nonlinearities caused by the addition of polymer. Convergence failure for the Newton solver is usually caused by steps that pass inflection points and discontinuities in the fractional flow functions. The industry-standard approach is to heuristically chop time steps and/or dampen saturation updates suggested by the Newton solver if these exceed a predefined limit. An improved strategy is to use trust regions to determine safe saturation updates that stay within regions having the same curvature for the numerical flux. This approach has previously been used to obtain unconditional convergence for waterflooding scenarios and multicomponent problems with realistic property curves. Herein, we extend the method to polymer flooding, and study the performance of the method for a wide range of polymer parameters and reservoir configurations.nb_NO
dc.language.isoengnb_NO
dc.publisherEuropean Association of Geoscientists and Engineersnb_NO
dc.relation.ispartof19th European Symposium on Improved Oil Recovery/IOR Norway 2017
dc.titleNon-linear Newton Solver for a Polymer Two-phase System Using Interface-localized Trust Regionsnb_NO
dc.typeChapternb_NO
dc.description.versionacceptedVersionnb_NO
dc.identifier.doi10.3997/2214-4609.201700356
dc.identifier.cristin1479526
dc.relation.projectNorges forskningsråd: 244361nb_NO
dc.description.localcodeThis chapter will not be available due to copyright restrictions (c) 2017 by European Association of Geoscientists and Engineersnb_NO
cristin.unitcode194,63,15,0
cristin.unitnameInstitutt for matematiske fag
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1


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