00009825 equilibrio
DESCRIPTION
EMPIRICALFOMULA TO DETERMINEEQUILIBRIUMRATIOSFOR =ANES PLUSFROM EQUILIBRIUMRATIOSFCR HEPTANETRANSCRIPT
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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.
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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:
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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.:
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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.
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IIiL
$
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K(C7)
K(C7+ )
%
M(C7)
M(C7+,=)
M(C7+,m)
Pk
%p
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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.
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REFERENms
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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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LPORATOR CALCULATION USXN~ WSEWOIR FLUIfl CO~f0S2TIW.- . .
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. . . . .O-.. ------- *-9--- 09--.. -O.-. --------------------------
L6TCD COWOSJTIONS IMMOL PERCENT {NO* OF c~@!pl&NTti m 311.-.------..-- . . . . ..------..*.-.
1S? sTAGE 2ND STA6E 3RD STAGE QTM sTsSE .--------..0---- --------------- --------------- ---------------
HMC7XON OF LIOUID = 0.3834 O.aE$ls 0.2265fJl 3a3u
0.19760.65S8. 0.90a3 0.a63U
.0-m--*-.-----*-----------------------e----..-----*-----.-..--.--------.-----m------------------Wtl FEED uAt?OR LIQuID VAPOR LlOUIO VAPoR LIOUXi) VAPOR LIQUID..----* --.. .-------- .----- .-. -------- m---------------------------------------------------------
2.990.9S
s?, 18Soe?b5*Q91.252.230.96a.os1.79
1s.85--...-
100.00
3.990.64
76.8210.9Qe.160.721.150.350.320.311.03
100.00
2.030.14
25.6110.427.662.113.971.992.23*.1739.6@
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100.00
4.54O.*O
6?5.7S18.347.251.081.570.37O.mb0.220.34
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100.00
0.71O*O14.536.377*882.665.232.653.224.2460.33------
10*O.OO
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2.64ZJ.76O.aa0.030.5s0.63
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100*O1
o*2th0.001.003*997.042.64S*373.043.+66.61
66.34-----.
100.00
x.960.007.2025.3~32.968.19s2.693.803.522.471.92
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100.00
0.020.000.040.673.001.7434.232.933.457.49
76.40--0---
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STOCUT6Wt.IOLtiO
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t 0.U30.130.590.35o.e40.580.68?J.4B15.10
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19.76
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,TOR CONL)I 7X(WW / CALCUL.A710NS------------------------------
;uREo IN PSIA / TCMPcRATUREQ IN FWR =RGENCE PRESSURE, IN PSIA =CAL PKSWTE?4P (PSI WFAHRJ OF c2+Q =
SfP-$ SEP-2 SEP-3 ST.TK----- ----- ..--* -----
1S00/$60 21s/ 100 75/ 100 15/ 100S2S0 6000 6500 7000
374/ 6Q6 355/ 672 350/ 6al 338/ 701
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Separator
Separator
Analyoea of Separator Gas~sFrom IL4uM -SQige Separation Teat
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Reasure, PSIG: 1500
Temperature, F. - 160
Component
Hydrogen SulfideCarbon DioxideNitrogenMethaneEthanePropane ,iso-13utanen-Butaneiso-Pentane
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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
60
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Nil4.990.09
41.2527.5616.192.853.931.010.840.620.67
7.518 100.00
GPM
6.9424.4440.9301.2360.3690.3040.2530.304
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