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1RobustSolutionofRichards’EquationforNon-UniformPorousMediaCassT.MillerandGlennA.WilliamsDepartmentofEnvironmentalSciencesandEngineering,UniversityofNorthCarolina,ChapelHill,NCC.T.KelleyandMichaelD.TocciDepartmentofMathematics,NorthCarolinaStateUniversity,Raleigh,NCShorttitle:ROBUSTSOLUTIONOFRICHARDS’EQUATION2Abstract.Capillarypressure-saturation-relativepermeabilityrelationsdescribedusingthevanGenuchtenandMualemmodelsfornon-uniformporousmedialeadtonumericalconvergencedi cultieswhenusedwithRichards’equationforcertainauxiliaryconditions.Thesedi cultiesarisebecauseofdiscontinuitiesinthederivativeofspeci cmoisturecapacityandrelativepermeabilityasafunctionofcapillarypressure.Convergencedi cultiesareillustratedusingstandardnumericalapproachestosimulatesuchproblems.Constitutiverelations,interblockpermeability,andnonlinearalgebraicsystemapproximationmethods,andtwotimeintegrationapproachesareinvestigated.AnintegralpermeabilityapproachapproximatedbyHermitepolynomialsisrecommendedandshowntoberobustandeconomicalforasetoftestproblems,whichcorrespondtoasand,aloam,andaclayloammedia.31.IntroductionFluid owinunsaturatedporousmediaisoftenmodeledusingRichards’equation(RE)[Richards,1931]andclosedbyconstitutiverelationstodescribetherelationshipamong uidpressures,saturations,andrelativepermeabilities[BrooksandCorey,1966;vanGenuchten,1980].Becauseofthenonlinearitiesinvolved,REisoftensolvedusinglow-ordernumericalapproximationmethods,suchas nitedi erenceor niteelementmethods.Thesetypesofsolutionmethodsareusedinmanyoftheexistingunsaturated owcodes.Theapplicationofthesecodestoawidevarietyofproblemsisconsideredcommonplace[vanderHeidje,1996].Thestandarduseofsuchsimulationmethodsnotwithstanding,problemsexistwithboththerobustnessande ciencyofnumericalsolutionstoRE;advancementsinthesolutionoftheseproblemsisanimportantandactivetopicofresearchinthewaterresourcescommunity.AcommonsetofconstitutiverelationsusedtocloseREisthevanGenuchtenrelationtodescribetheinterdependenceof uidpressuresandsaturationsandtheMualemrelationtodescribetheinterdependencebetween uidsaturationandrelativepermeability.Theexponent,ornv,inthevanGenuchtenrelationisameasureofpore-sizeuniformity.Formanynaturalporousmedia,typicalvaluesofnvrangebetween1.0to2.0,whendeterminedusingstandardlaboratoryapproachesand ttedusingstandardinversetechniques[Kooletal.,1985;vanGenuchtenetal.,1991].UsingthevanGenuchtenandMualem(VGM)constitutiverelationsinexistingREcodes,weexperiencedsigni cantproblemsinattainingaconvergentsolutionforcasesinwhichnv2forcertainsetsofauxiliaryconditions.Anexampleofsuchacasewasforin ltrationfromapondedsurfaceboundaryconditionintoasystemoriginallydrainedtoequilibrium.Theseexperiencesmotivatedthiswork,whichhadseveralobjectives:(1)todocumentacommonclassofvariably-saturated owproblemsthatlackrobustnesswhensolvedusingstandardsolutionapproaches;(2)todeterminethereasonwhytraditional4approacheslackrobustnessforthisclassofproblems;(3)toinvestigateavarietyofalternativeapproaches;and(4)tocompareasetofalternativeapproachesforarangeofmediaconditionstotestrobustnessande ciency.2.BackgroundFouraspectsoftheliteratureonunsaturated owwarrantatleastabriefconsideration:(1)constitutiverelationsusedtodescribepressure-saturation-conductivityrelationsandtypicalparametervaluesfornatural,unconsolidatedmedia;(2)approachestypicallyusedtoapproximateRE;(3)methodsforapproximatingrelativepermeabilitiesinadiscreteapproximationofRE;and(4)strategiesusedtoestimatetherelativelycomplexconstitutiverelationsthatareapartoftheformulationsofconcern.Wediscusseachoftheseaspectsinturn.2.1.Pressure-Saturation-ConductivityRelationsAwell-posedformulationofRErequiresthatconstitutiverelationsbespeci edtodescribetheinterdependenceamong uidpressures,saturations,andrelativepermeabilities,whichwillbereferredtoasp-s-krelations.Severalapproacheshavebeenadvancedtodescribep-s-krelations[BrooksandCorey,1966;Mualem,1976;vanGenuchten,1980],butdeterminingthemostappropriateconstitutiverelationformulationisstillanopenissue.WeusethevanGenuchtenrelationtodescribetherelationshipbetween uidpressuresandsaturations[vanGenuchten,1980]andtheMualemrelationforthatbetween uidsaturationsandrelativepermeabilities[Mualem,1976].SeveralcodesdocumentedintheliteratureusetheserelationstocloseRE(e.g.,[Yeh,1987;SimunekandvanGenuchten,1994]).WewillrefertotheserelationscollectivelyasthevanGenuchten/Mualem(VGM)relations.BecauseofthewidespreaduseofthevanGenuchtenrelation,manyexperimentaldatasetshavebeendescribedusingthisapproach,andmanysetsofparametervalues5areavailableintheliterature[vanGenuchtenetal.,1991].Inaddition,aparameterestimationcodeisavailableandhasbeenwidelyusedtodeterminetheseparametervaluesfromexperimentaldata[vanGenuchtenetal.,1991].Theseparametervaluesarerelatedtothemeanporessize( v)andtheuniformityofthepore-sizedistribution(nv).Thestandardrangeofvaluesofnvisofparticularinterest;itcanvaryfromnear1.0[vanGenuchtenetal.,1991]tonearorevengreaterthan10.0[KoolandParker,1987;MayerandMiller,1992],withtheporesizedistributionbeingincreasinglyuni
本文标题:Short-title-ROBUST-SOLUTION-OF-RICHARDS--EQUATION
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