Immediate Settlement Settle3D

  • Upload
    geoteco

  • View
    26

  • Download
    0

Embed Size (px)

Citation preview

  • WhentoUseImmediateSettlementinSettle3D

    Mostengineersagreethatsettlementismadeupofthreecomponents:immediate,primaryconsolidationandsecondaryconsolidation(orcreep).Mostengineersalsoagreethatforspecificscenarios,oneortwoofthesecomponentsmaybemissingornegligible.InSettle3D,youhavetheabilitytoturnonoroffeachofthesetypesofsettlement.Usersgenerallyknowwhetherornottheirmaterialiscreeping,butthequestionremains,whenshouldyouturnonimmediatesettlement,whenshouldyouturnonprimaryconsolidationandwhenshouldyouturnonboth?Thisarticleattemptstoanswerthisquestionthroughconsultationofcommontexts(seeBibliography)alongwithuserscommentsandsomeofourowninsights.Wehopethatthisarticlewillhelptosettlethismatter.

  • ComponentsofSettlementVirtuallyallreferencesagreethatthetotalsettlementofafoundationiscomposedofthreecomponents: ST=Si+Sc+Sswhere: STisthetotalsettlement Siistheimmediatesettlement Scistheconsolidationorprimarysettlement SsisthesecondarysettlementorcreepSomeofthesecomponentsmaynotbepresent,ortheeffectsmaybenegligibledependingonthesoiltype.Hence,theabilitytoturneachcomponentonandoffinSettle3D.Butthequestionremains,whendoIuseeachtypeofsettlement?Letsmaketwoassumptions:

    Thesoilgrainsareincompressible Waterisincompressible

    Neitheroftheseistrueofcoursebutthestiffnessofthesoilgrainsandthewaterisgenerallysolargethatwecanignoretheeffectsoftheircompressibility.Withthesetwoassumptionsinmind,theonlywaythatsettlementcanoccuristhroughrearrangementofthesoilgrainsand/orcollapseofporespace.Thebasicmechanismforsettlementisthereforeessentiallythesameforallthreetypesofsettlement,andthedivisionintothreecomponentsisbasedonotherfactors.

    SecondaryConsolidationLetsfirstconsidersecondaryconsolidation.Thesecondarysettlement,Ssrepresentstimedependentsettlement,orcreep,thatoccursunderaconstanteffectivestress.Thiscomponentofsettlementisimportantinorganicsoilssuchaspeat,butcanoftenbeomittedforothersoiltypes.Itisfairlyeasytoseparatethiscomponentofsettlementfromtheothertwosinceitoccurswheneffectivestressdoesnotchange1.Thereforewewillnotdiscussthiscomponentfurther.

    1 There is research that suggests that creep occurs simultaneously with consolidation settlement, but traditionally, engineers adopt the definition of creep occurring after consolidation settlement. This is the approach adopted by Settle3D.

  • ImmediateSettlementTheimmediatesettlementisalsosometimescalledvolumedistortionsettlement.Essentially,thisistherearrangementofgrainsduetochangingstress,resultinginareductioninvoidratioandinstantsettlement.Inmosttexts,immediatesettlementisconsideredtobeanelasticprocess.Thereforethesettlementcanbecalculatedfromelastictheory(seeforexample,Day2005,equation8.9).Settle3Dalsouseselastictheorytocalculateimmediatesettlement.So,byturningonimmediatesettlementinSettle3D,youareessentiallycalculatingthevolumedistortionduetostresschanges.Oneimportantconsiderationisthattheremaybeinelasticprocessesatwork(plasticflow),meaningthatthisimmediatesettlementcalculationwillunderestimatetheactualsettlement.HoltzandKovaks(1981)state,Theimmediate,ordistortion,settlement,althoughnotactuallyelasticisusuallyestimatedbyusingelastictheory.ItisrecommendedthatalowervalueofEbeusedtoaccountfortheplasticflow.Therearemanyothermethodsthattrytosimplifytheelasticcalculation,especiallyintheestimationofEfromlaboratoryorfieldtests.Someofthesemethodstakeintoaccounttheplasticflow,loadrigidityandloadshape.AllarebasedonempiricalsettlementdataandarethereforegroupedunderempiricalmethodsinSettle3D(e.g.Schmertmannmethod).Thesecanalsobeusedtocalculateimmediatesettlement.Notehoweverthatthesemethodsaregenerallynotasrobustinthattheycanonlyconsidersimpleloadinggeometries.Also,whenplottingtotalsettlement,theempiricalsettlementsarenotincluded.Youmustaddthemmanually.

    OR

    Sowhendoyouneedtoconsiderimmediatesettlement?Immediatesettlementisgenerallyassumedtobethesettlementthatoccursquicklyaftertheconstructionofyourfoundationorembankment.Howquickly?Bowles(1996)suggeststhatimmediatesettlementsarethosethattakeplacewithin7daysof

  • loading.Adoptingthisdefinitionallowsustoconsidermanypossiblescenariosthatcouldleadtoimmediatesettlement.Thesewillbediscussedinthenextsection.

    PrimaryConsolidationTheprimaryconsolidationsettlement,Scisthegradualrearrangementofgrainsaswaterisexpelled.Thiscomponentofsettlementisusuallydominantinfinegrainedsaturatedclays.Butconsolidationalsooccursinothersoiltypes.Hence,thereissomegrayareaastowhentouseimmediatesettlement,whentouseprimaryconsolidationsettlementandwhentouseboth.ThefollowingsectionoutlinesdifferentpossiblescenariosandhowtosimulatetheminSettle3D.

    SettlementScenariosInthissection,weconsiderdifferentsettlementscenariosandhowtodealwiththeminSettle3D.Firstwewilldescribeasimpletestmodelusedtoillustrateeachsituation.

    TestModelConsideraflexiblecircularloadofmagnitudeq=10kPaandradiusa=1montopofasoillayerwiththicknessh=10m.Wewillusethismodeltoexaminedifferentscenarios.Lookingatthescreencapturebelow,aquerypointisplacedatthecentreofthecircleforcalculationofsettlements.

  • Scenario1:UnsaturatedMaterialInthiscase,thereisnoconsolidationandallofthesettlementisimmediate.However,thisdoesntnecessarilymeanthatyoushouldturnonimmediatesettlementandturnoffconsolidationsettlement.Ifyouturnonconsolidationsettlementforanunsaturatedmaterial,thenthesettlementwilloccurimmediatelysincethereisnotimedependentdissipationofporepressures.Thistechniquewouldbeusefulintwopossiblescenarios:

    Yourmateriallayerispartiallybelowthewatertable.Inthiscase,youcanturnonconsolidationsettlementandturnoffimmediatesettlement.Thesoilthatisabovethewatertablewillcompactimmediatelyandthesoilbelowthewatertablewillcompactgradually.

    YourmaterialisnonlinearandyouwishtousethenonlinearparametersCcandCr.Inthiscase,youmustuseconsolidationsettlementandnotimmediatesettlement.

    Fortheunsaturatedmaterial,itdoesntreallymatterifyouchooseimmediateorconsolidationsettlement,aslongasyoudontchooseboth.

    Infact,ifyouchooseconsolidationsettlementwithalinearmaterial,mvisjusttheinverseofEthatisusedforimmediatesettlement.Soamodelwithmv=0.001m2/kNwillgiveexactlythesamesettlementasamodelwithE=1000kPa.

  • Scenario2:PartiallySaturatedMaterialInthiscasetherewillbesomeimmediatesettlementasairisquicklypushedoutoftheporespaces.However,aswiththeunsaturatedcase,itisnotnecessarytoturnonimmediatesettlement.InSettle3D,youcanaccountforthiseffectbysettingtheBbarlessthan1(Bbarrangesfrom0foranunsaturatedmaterialto1forasaturatedmaterialseetheTheorymanualformoredetails).Whenyoudothis,aproportionoftheappliedstressistransferredimmediatelytothesoilsothatyouseesomeimmediatedeformation.

    Scenario3:FullySaturatedSandIfyouaredealingwithsand,orsomeothercoarsegrainedmaterialthathasahighpermeability,thenporepressuresdissipatequicklyandsettlementisessentiallyimmediate.InSettle3D,youcansimulatethisinseveralways:

    TurnonImmediateSettlementandturnoffPrimaryConsolidation TurnoffImmediateSettlement,turnonPrimaryConsolidationandseta

    largevalueforcvork. TurnoffbothImmediateSettlementandPrimaryConsolidationanduse

    oneoftheEmpiricalMethods.Thefigureonthefollowingpageshowsacomparisonofresultsforthefirstmethodandthesecondmethod.

  • 05

    10

    15

    20

    25

    0 5 10 15 20Time (d)

    Tota

    l Set

    tlem

    ent (

    mm

    )

    Primary Consolidation: m v = 0.001 m

    2/kN k = 0.1 m/day

    Immediate Settlement: E = 1000 kN/m2

    Comparisonofsettlementresultsforthecircularloadmodelusingdifferentmethodstoaccountforrapidporepressuredissipation.

    Scenario4:FullySaturatedClayThisisprobablytheonlysituationinwhichyoumaywanttousebothImmediateSettlementandPrimaryConsolidation.Settle3DusesonedimensionalconsolidationtheorytocalculatethePrimaryConsolidationsettlement.However,mostloadingscenariosareactuallythreedimensional.Thereforeevenwithanincompressiblefluid,somevolumedistortionsettlementwilloccurimmediatelyinasaturatedclay.Elastictheorycanbeusedtoestimatethissettlementwithoneimportantconsideration:youshouldusetheundrainedYoungsmodulusandPoissonsratio.TheundrainedPoissonsratiois0.5(alowernumbercanbeusedifnot100%saturated).TheundrainedYoungsmoduluscanbecalculatedby:

    draineddrained

    undrainedEE 12

    3

    so,foramaterialwithaPoissonsratioof0.2,Eundrained=1.25Edrained.However,LambeandWhitman(1979)statethatWithactualsoils,theratioofEundrained/Edrainedistypicallymuchlargerthanthistheoreticalvalue.Valuesof3or4arenotuncommonfornormallyconsolidatedclays.Itisalsoimportanttonotethatthisisathreedimensionaleffect,sotheamountofimmediatesettlementdependsonthegeometryofthesituationandthedrainedPoissonsratio.Foraloadwithverylargearealextent,orlowdrainedthesituationisclosetoaonedimensionalloadingscenario,sotheimmediatesettlementwillbenegligible.Poulos(2000)presentsgraphsshowingtheimportanceoftheseparametersincalculationofimmediatesettlement.

  • Theoreticalabilityofonedimensional(PrimaryConsolidation)analysistopredicttotalfinalsettlement.FromPoulos(2000). Forsoft,normallyconsolidatedmaterials,ImmediateSettlementshouldbeaddedtothePrimaryConsolidationsettlement.Therefore,thefollowingequationapplies:ST=Si+SC Soft,normallyconsolidatedclaysHoweverPoulos(andothers)suggestthatfornormallyconsolidatedclays,theimmediatesettlementasaproportionofthetotalsettlementisoftennegligible.Thisisillustratedonthefollowingpage.

  • Normally consolidated clay: Eundrained ~ 3Edrained Si is small

    Forstiffoverconsolidatedmaterial,PouloswarnsthattheimmediatesettlementshouldnotnecessarilybeaddedtothePrimaryConsolidationsettlement.InsteadtheimmediatesettlementaccountsforpartofthePrimaryConsolidationSettlementandthatifyouaddthemtogether,youwillbedoublecounting. InSettle3Dtherefore,youwouldhavetosomehowreducethecalculatedconsolidationsettlementtobalancetheimmediatesettlement. InSettle3D,thesethreedimensionaleffectscanbemoreeasilyaccountedforinanotherway.GotoProjectSettings,choosetheAdvancedtabandselectUseMean3DStressasshownonthenextpage:

  • Settle3Dwillnowsettheinitialexcessporepressuretobeequaltotheundrainedmeanstressratherthantheverticalstress,wheretheundrainedmeanstressis:

    5.032131

    undrainedM SeetheTheoryManual,section4.2andDas(2007)fordetails.Usingthemeanstressinsteadoftheverticalstressmeansthatwhenaloadisapplied,partoftheloadisinstantlycarriedbythegrainskeleton.Thisresultsinsomeimmediatesettlement.Sincethecalculatedmeanstressisafunctionoftheloadgeometry,thereisnoneedtoapplyafudgefactortoaccountforthesizeoftheload.Theplotbelowshowshowimmediatesettlementissignificantforasmallloadonathicklayer,yetinsignificantforalargeloadonathinlayer.Thesubsequentplotalsoshowshowamodelthatdoesnothavemeanstressturnedonproducesthesamelongtermsettlementasthemodelwithmeanstressturnedon.Thisshowshowtheimmediatesettlementisnotbeingdoublecountedwhenmeanstressisturnedon.

  • 05

    10

    15

    20

    25

    30

    35

    40

    45

    0 5 10 15 20 25 30 35 40 45 50

    Time (d)To

    tal S

    ettle

    men

    t (m

    m)

    Load radius = 10 mSoil layer thickness = 1m

    Load radius = 1 mSoil layer thickness = 10m

    Settlementcalculatedforoverconsolidatedclaywithmeanstressoptionturnedon.

    0

    5

    10

    15

    20

    25

    30

    35

    40

    45

    50

    0.1 1 10 100 1000Time (days)

    Set

    tlem

    ent (

    mm

    )

    Vertical stress on

    Mean stress on

    Settlementcalculatedforthe10mloadwithmeanstressturnedoncomparedtothesettlementcalculatedwithverticalstressonly.

  • SummaryThetablebelowsummarizeshowtomodeldifferentscenariosinSettle3D.Thisisonlyaguidelineandspecificsites,loadingscenariosandacquireddatamaydemandadifferentapproachforyoursettlementproblem.Asalways,youshoulduseyourengineeringjudgmentwhencreatingandanalyzingthesenumericalmodels.

    Material Possible Methods

    Unsaturated 1. Immediate on*, primary off or 2. Immediate off, primary on

    Partially saturated 1. Immediate off, primary on with B-bar < 1

    Sand 1. Immediate on*, primary off or 2. Immediate off, primary on, cv or k is large or 3. Immediate and primary off, use empirical method

    Saturated normally consolidated clay

    1. Primary on +

    (optional) immediate on* with undrained parameters**

    Saturated overconsolidated clay

    1. Primary on, immediate off, mean stress on or 2. Immediate on* with undrained parameters** +

    primary on + correction to account for double-counting

    *Elasticsolutionsdonotaccountforplasticflowandmaythereforeunderestimatetheactualsettlement**Undrainedstiffnessparameterscalculatedfromtheorymaybetoosoft,thereforetheimmediatesettlementmaybeoverestimated

  • Bibliography Bowles,J.E.(1996).FoundationAnalysisandDesign5thed.,McGrawHill,1175pp.CanadianGeotechnicalSociety(2007).CanadianFoundationEngineeringManual4thed.,CanadianGeotechnicalSociety,488pp.Das,B.M.(2007).PrinciplesofFoundationEngineering6thed.,Thomson,750pp.Day,R.W.(2005).FoundationEngineeringHandbook:DesignandConstructionwiththe2006InternationalBuildingCode,McGrawHill.DepartmentoftheNavy(1982).SoilMechanicsNAVFACDesignManual7.1,DepartmentoftheNavy,Alexandria,VA.,378pp.Holtz,R.D.andW.D.Kovacs(1981).AnIntroductiontoGeotechnicalEngineering,PrenticeHallInc.,733pp.Lambe,T.W.andWhitman,R.V.(1979).SoilMechanics,SIVersion,JohnWiley&Sons,553pp.McCarthy,D.F.(2007).EssentialsofSoilMechanicsandFoundations7thed.,PrenticeHall,850pp.Peck,R.B.,Hanson,W.E.andT.H.Thornburn(1974).FoundationEngineering2nded.,JohnWiley&Sons,514pp.Poulos,H.G.(2000).FoundationSettlementAnalysisPracticeVersusResearch,TheEighthSpencerJ.BuchananLecture,https://ceprofs.civil.tamu.edu/briaud/buchanan%20web/lecture_series.htm

    Components of SettlementSecondary ConsolidationImmediate SettlementPrimary Consolidation

    Settlement ScenariosTest ModelScenario 1: Unsaturated MaterialScenario 2: Partially Saturated MaterialScenario 3: Fully Saturated SandScenario 4: Fully Saturated Clay

    SummaryBibliography