
-
Introduction
Theory and Background
The Effect of Mesitylene on the Cold Flow Properties of Model Crude Oils
UgochukwuOkeibunorandMichaelSenra
Department of Chemical and Biomolecular Engineering, Lafayette College, Easton, PA 18042
Experimental Methods
Results and Analysis
Future Work
References
[1]Senra,M.,Scholand,T.,Maxey,C.,
&Fogler,H.S.Role of polydispersity
and cocrystallization on the gelation of
long-chained n-Alkanes in solution.
Energy & Fuels,235947-5957.Nov.
2009.
[2]NurFatmala.Wax in Subsea
Pipelines,February2016.WebAugust
7
th
2017.
Thecoldflowpropertiesofafluidrepresentits
movementandcharacteristicsatlowtemperatures.These
propertiesareoftendictatedbyhowtheprecipitated
solutesformcrystals.
Conclusions
v Microscopycanbeusedtoanalyze
thecrystalstructuresofthegels
formedinthisworktobetter
validatetheresultsandhypotheses.
v Increasinglycomplexn-alkane
systemscanbestudiedtodetermine
iftheeffectsseenformodelcrude
oilscanbeextendedtoactual
crudes.
Figure 2.Cross-polarizedmicroscopyimagesforslowlycooledn-alkane
solutions.Panela)for4%C36solutionsat33°C,panelb)for4%C36/5%
C28solutionat25°Candpanelc)for4%C36/6%C32solution[1]
Acknowledgements
ThankstotheLafayetteCollegeEXCEL
programandtheDepartmentof
ChemicalEngineeringforfacilitatingthe
completionofthisproject.
Thedepositionofwaxinsubseaoilpipelineshas
beenamajorprobleminflowassurance.Theseformed
geldepositscanreduceoilproductionandoncethey
occur,arecostlytoeliminate.
Figure 1.Waxformedin
pipeline[2]
Figure 4.TAInstrument
DiscoveryHR-2
rheometer
Figure 5. Storageandloss
moduliofafluidunder
stress
q Smallaromaticmoleculescan
influencethethermodynamicand
gelationcharacteristicsofmodel
crudeoils.
q Theireffectscanbeafunctionofthe
amountofaromaticpresentandthe
complexityofthecrudeoil.
q Themechanismsbywhichthe
aromaticinfluencesthesystemare
widelyvaried.
q Properpredictionofcrudeoil
gelationshouldrequireinformation
aboutthearomaticscontent.
Figure6showsthatthegelpointoftheC36
systemincreasedfrom33.5°Cto40°C,whilethegel
pointoftheC32systemhadaslightincreasefrom
28°Cto30°C.Ahypothesisforthisbehavioristhat
increasingmesityleneconcentrationsdecreasethe
solubilityofC32andC36indodecane,thuscausing
gelationtooccurathighertemperatures.
Figure8showsthatthecloudpointrange
wasabout2°Cforallsystems.However,
monodispersesystemsshowedaslightupward
trendwhilepolydispersesystemsshowedaslight
downwardtrend.Foreachmesitylene
concentration,thegelpointobtainedby
differentialscanningcalorimetrywasgenerally
about2°Clower,butsimilartrendswereobserved.
Figure 6.GelPointTrendforMonodisperseSystems.
Figure 8.CloudPointsforthen-alkaneSystemsObtainedbyCalorimetry
Figure7showsthatforbothsystems,aninitial
increaseinmesityleneconcentrationby1%-2%
causedasharpdecreaseinthegelpoints.Athigher
concentrations,thegelpointsrosesharplyand
remainedrelativelyconstant.Itishypothesizedthat
lowamountsofmesitylenedispersestheformed
crystals,whilehighamountsofmesitylenecanself-
aggregate,limitingtheirinfluenceonthecrystal
structure.
a)
b)
c)
Figure 7. GelPointTrendforPolydisperseSystems
Inthiswork,dodecane(C12),octacosane(C28),
dotriacontane(C32)andhexatriacontane(C36)served
asmodelcrudeoils.Theaimofthisworkwasto
investigatetheeffectsofmesitylene,asmallorganic,on
thecoldflowcharacteristicsofthesemodelcrudeoils.
PreviousworkhasshownthatC36(Figure2a)
formslargecrystals,producingavolume-spanning
networkthatisconducivetogelation.However,adding
anothern-alkanecaninfluencehowthesecrystalsform.
C28dispersesC36fromforminglargeanduniform
crystals(Figure2b),whileC32reducesthegelationof
C36byformingcocrystalswithC36(Figure2c).
Studieshaveshownthatn-
alkanes,theprimarycomponentsof
crudeoil,arelargelyresponsiblefor
thisdeposit[1].Thisphenomenon
occursbecauseoftheirlowsolubility.
Figure 3. Chemical
Structure of Mesitylene
Thisprojectaimstoanalyze
theeffectsofasmallaromatic
moleculeonthegelation
characteristicsofdifferentn-alkane
systems.Specifically,theeffectof
addingmesityleneonthegel
formationofthesemodeloil
systemswasstudiedbyrheology.
v Cold flow properties studied in this work were the gel point
and the cloud point.
v The gel point represents the temperature where initial gel
formation occurs and the cloud point represents the
temperature where crystals can first be seen.
v Rheology and differential scanning calorimetry were used to
analyze the pour points and cloud points respectively.
v Experimentation methods ensured elimination of thermal and
shear history by holding sample quiescently at a constant
temperature for a substantial period of time.
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