00009825 equilibrio

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1. 11. %323 March19, 1981. EMPIRICALFOMULA TODETERMINEEQUILIBRIUMRATIOS FOR =ANES PLUSFROMEQUILIBRIUMRATIOS FCR HEPTANE INTRODUCTION UNSOLICITED In 19’77(1)*I was askedto determinetheoptimumseparator conditions for a gas condensatereservoir. Havingno specificbackgroundonthesubject,I comencedin gatheringinfonuationon themethodstotacklethisproblem. Thisledme to severalcorrelationsandexperimental. work from whichtheequilibriumratios(K-values)forsinglecomponents couldbe derived. TheK-valuesarerequiredto predict recovery levels. SoonI realisedthat I had to becomea highlycompetent mathematiciansnda skilledcomputerengineerifIwantedto makeuaeof themanyformulaepublishedin technicalmagazines andbooks. SinceI couldnot sparew timeto do this,I rejectedthissolution.The remainingchoicewas to usethe K-chartspublishedby theI?GPA(ref.1),but stillaimingto comeupwithreliableseparatorresultsforhighlyvolatileoils and gas condensates. In1957,NaturalGasProcessorsA~sociation(NGpA)haveco~iled all experimentieally deriveddataforequilibriumratios(X)of singlecomponentsinconvergencepressurecharts. Ithasbeen fomd thatat a giventemperature,theK-valuesof allcomponents inthemixtureconvergeto unityat a “certain@ressure”. This pressurehasbeencalled(apparent)convergencepressure,pk. The K-chartsareisothermallog K versuslog P curves. NGPAhave regularlyrevisedandupdatedthegraphsasmoreexperimentaldab becameavailable.Theyare presentedin section18 of the M- gineeringDataBook(ref.1). AlthoughNGPA recognize thatthereare indicationsthatcoruposi- tioneffectsinhydrocarbonmixturesarenotfullyrepresentedby convergencepressurealone9theconvergencepressurecorrelation has been retainedforthe following reasons: 1) The chartsin useprovidea usefuland rapidgraphicalapproach forengineers. Note (1) : At that the employedwithMaraven,Lagunillas,Venezuela.

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EMPIRICALFOMULA TO DETERMINEEQUILIBRIUMRATIOSFOR =ANES PLUSFROM EQUILIBRIUMRATIOSFCR HEPTANE

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  • 1.

    11.

    %323

    March19, 1981.

    EMPIRICALFOMULA TO DETERMINEEQUILIBRIUMRATIOSFOR =ANES PLUSFROM EQUILIBRIUMRATIOS

    FCR HEPTANE

    INTRODUCTION UNSOLICITEDIn 1977(1)*I was askedto determinethe optimumseparatorconditionsfor a gas condensatereservoir.

    Havingno specificbackgroundon the subject,I comenced ingatheringinfonuationon the methodsto tacklethisproblem.Thisled me to severalcorrelationsand experimental.work fromwhichthe equilibriumratios(K-values)for singlecomponentscouldbe derived. The K-valuesare requiredto predictrecoverylevels. SoonI realisedthat I had to becomea highlycompetentmathematiciansnd a skilledcomputerengineerif I wantedtomake uae of the many formulaepublishedin technicalmagazinesand books. SinceI couldnot sparew time to do this,Irejectedthis solution.The remainingchoicewas to use theK-chartspublishedby the I?GPA(ref.1), but stillaimingtocomeup with reliableseparatorresultsforhighlyvolatileoilsand gas condensates.

    In 1957,NaturalGas ProcessorsA~sociation(NGpA)have co~iledall experimentieallyderiveddata for equilibriumratios(X)ofsinglecomponentsin convergencepressurecharts. It has beenfomd that at a giventemperature,the K-valuesof all componentsin the mixtureconvergeto unityat a certain@ressure. Thispressurehas been called(apparent)convergencepressure,pk.

    The K-chartsare isothermallog K versuslog P curves. NGPAhaveregularlyrevisedand updatedthe graphsas more experimentaldabbecameavailable.Theyare presentedin section18 of the M-gineeringDataBook (ref.1).

    AlthoughNGPA recognize that thereare indicationsthatcoruposi-tion effectsin hydrocarbonmixturesare not fullyrepresentedbyconvergencepressurealone9the convergencepressurecorrelationhas been retainedforthe following reasons:1) The chartsin use providea usefuland rapidgraphicalapproach

    for engineers.

    Note (1) : At that the employedwith Maraven,Lagunillas,Venezuela.

  • .-1i

    i

    11

    i

    . .

    ..

    #

    2) The valuesare sufficientlyaccurateto satisfymanycalculations.

    3) The graphsare tidel.yusedin the industry.

    113.LIMITATIONSOF THE K-CHARTS

    In thepastspredictions,usingthe K-valuesof the graphspublishedby NGPAhave semethes failed. Ofthenthe K-valueswere suspectedfor this failure. The main fieldsofuncer-tain~ are however:

    1. K-valueformethane

    2.

    M the caseof meth=e, interpretationbetweenpk chartsisa must to obtainaccurateK-values. M.B. standingpointedoutin Ref. 2 that the K-valueformethaneinfluencesin a largemeasurethe liquidrecove~.

    2. The equilibriumratioforheptanesplus

    h the EhgiaeeringDaL.:?-nknO K-chartsare givenfortheheptsnesplus fraction. In factno suchgraphscan beconstmcted. The K-valuesforheptanesplushave alwaysto beestimated.

    As a firstapproximationit was assumedthatthe K-valueforheptanespluswouldbe 15% of the K-valueof heptane. Thiseasysolutionwas basedon a papermadeby D. ~tz and .K. Hachmuch(ref.3) and on informationfromref.2. Appli-cationof the 0.15correlationforthe gas condensatereser-voir fluidsgaveresultswhichwere oftennot satisfactory.Thereforaa methodfor determiningK-valuesforheptanespluswas workedout. The finalformulahas yieldedgoodresultsand has been in closeagreementwith laborato~test data.

    IV. DETERMnW?IONOF THE RATIOKc47+/~7: K-m

    me idea of a relationshipbetweenthe equilibriumratiosforheptsnesplus and heptanes,set fowardby ~tz and Hachmuchwasmaintained.Aftermany experimentsit was foundthattheformula;!expressingthis relationshiphad to includethe follo-wingparameters:

    ./.

    .

  • 3.

    a) The molecularweightof the heptanesplus,b) The specificgravityof the heptanesplus.c) The separatorand convergencepressure.

    Discussion

    1. Themledularwe~ghtof the heptanesplus givesthe first~dicatiOn Of howvolatilethis &action is. The higherthemolecularweightthemore longand littlevolatileh@rocarbonmoleculesare present. The ratio~ is proportionaltwiththe ratiomolecul~ weightof heptane/molecul~weightofheptanesplus.

    2. The specifiegratityof the heptanesplusis alsolinkedtoa certaindegreewiththe K-value. SomearomaticshavingaZow bubblepoint end low molecularweightare in factheavycomponents.This distortiveeffectis takeninto accountby calculatingthe expectedmolecularweightbasedon thespecificgravityof the heptanesplus. For thisexclusivepurposethe averagerelationshipbetweenmolecularweightand specificgratityhas been definedby a straightlineona semi-logaritticscale,accordingto the formula:

    ~0/3M (c?+, C) = 5.8 X G (CT+) - 2.585Note : seenomenclatureat the end of thisnote.

    Again,the ratioKr is proportionalwiththe ratiomolecularweightof Mptsne/calculatedmolecularweightof heptanesplus.

    Whenthe separatorpressureis approachingthe convergencepressurethe rationKr comescloser to one. At the conver-gencepressureitselfK-valuesof all componentsare equalto one. This shouldalsobe the case forthe multi-componentC7+.

    Fomu,laforKr&lcti-8tion

    The followingempiricalformulawhichis reflectingthe abovementionedeffects,has been in~ose.agreementwith reel labo-ratoryteatg.:

  • ,.

    ,.

    4,

    i

    1%7+/%7 = KJ

    ( @&/P~ep)M(C7) M(C7+,C)fi= xM@7+,m M(C7+,m))v. RESULTS

    In tabulations1 and 2 the calculateddataand laboratorydataare given. The resemoir fluidis a gas-condensate.As can beseen fromthe tabulationsagreementat all pressurestepsisexcellent.

    J.A.Follet.

    I

  • i.:

    IIiL

    $

    I

    K(C7)

    K(C7+ )

    %

    M(C7)

    M(C7+,=)

    M(C7+,m)

    Pk

    %p

    :

    :

    :

    .

    .

    l.

    :

    :

    :

    l.

    Specificgravityof the heptanesplusfraction,in g/cc and 60/600 F

    (- repofiedinthe WT study).

    Ik@libriumratioforheptane.

    Equilibriumratioforheptanesplus

    Ratio K(C7+)~(~).

    Molecularweightof heptane.

    Calculatedmolecularweightofheptanesplue(fr~the specificgratity)

    Measuredmolecularweightof heptanesplus(as reportedin the PVT study).

    Convergencepressuxe.

    Separatorpressure.

    .i

  • I,.i .

    Ij

    I

    REFERENms

    i

    I 1. EngineeringDataBook,publishedby the NaturalGas ProcessorsSuppliersAssociation,Section18 : EquilibriumRatios(1976).1 2. Volumetricand phasebehaviorof oil fieldhydrocarbonsystems,i by M.P.. Standing(1952) l..i

    J1I 3. Vaporizationequilibriumconstantsin a crudeoil-naturalgas\ system,by D. Katz and K. Hachmuch,Ind.Eng.Chem.29, 1072(1937)l!

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    1S? sTAGE 2ND STA6E 3RD STAGE QTM sTsSE .--------..0---- --------------- --------------- ---------------

    HMC7XON OF LIOUID = 0.3834 O.aE$ls 0.2265fJl 3a3u

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    ,TOR CONL)I 7X(WW / CALCUL.A710NS------------------------------

    ;uREo IN PSIA / TCMPcRATUREQ IN FWR =RGENCE PRESSURE, IN PSIA =CAL PKSWTE?4P (PSI WFAHRJ OF c2+Q =

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    Separator

    Separator

    Analyoea of Separator Gas~sFrom IL4uM -SQige Separation Teat

    .

    Reasure, PSIG: 1500

    Temperature, F. - 160

    Component

    Hydrogen SulfideCarbon DioxideNitrogenMethaneEthanePropane ,iso-13utanen-Butaneiso-Pentane

    .

    n-PentaneHexanesHeptanes plus

    MolPercent .

    Nil3.350.74

    77.31, 10.24

    4.080.751.100.370.350.5?1.14

    100.00

    GPM

    2.5791.1200.2450.3460.1350.1260.2320.517

    200

    100 l

    MolPercent GPM

    Nil4.400.30

    67.4716.837.121.141.530.400.320.230.26

    4.2391.9540.3720.4820.1460.1150.093

    0.1175.300 100.00

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    41.2527.5616.192.853.931.010.840.620.67

    7.518 100.00

    GPM

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    14.782

    100

    MolPercent

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    100

    MolPercent GPM

    Nil2.140.038.00

    23.5732.22

    8.4413.054.123.372.872.19

    5.9388.8432.7544.1031.5041.2181.1680.992

    100.00 26.520