the science of foaming - université paris-sud · the science of foaming ... surfactants, polymers,...
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Historicalperspective
Thescience
offoaming
Wiebke
Drenckhan
a,⁎,Arnaud
Saint-Jalmes
b
aLaboratoire
dePhysique
desSolides,U
niversitéParis-Sud,U
MR8502,O
rsay,FrancebInstitutde
Physiquede
Rennes,CNRS
UMR6251,U
niversitéRennes-1,Rennes,France
abstract
article
in
fo
Available
onlinexxxx
Keywords:
Foaming
Liquidfoam
Bubblegeneration
Gas/liquid
interfaceFoam
ingtechniques
Bubblesize
distribution
Thegeneration
ofliquidfoam
sisatthe
heartofnumerous
natural,technicalorscientific
processes.Eventhough
thesubject
offoam
generation
has
along-standin
ghistory,m
anyrecent
progresseshave
beenmade
inan
attempt
toelucidate
thefundam
entalprocesses
atplay.W
ereview
thesubject
byprovidin
gan
overviewof
therelevantkey
mechanism
sofbubble
generationwithin
acoherenthydrodynam
iccontext;and
wediscuss
dif-ferentfoam
ingtechniques
which
exploitthesemechanism
s.©
2015Elsevier
B.V.A
llrightsreserved.
Conten
ts
1.Introduction
...............................................................
02.
Fundamentals
offoamform
ation.....................................................
02.1.
Introduction...........................................................
02.2.
Thephysics
ofdeforming
interfaces.................................................
02.3.
Thephysics
ofrupturinggas
ligaments
...............................................
02.4.
Bubblegeneration
requiringtopologicalchanges
...........................................
02.4.1.
Bubblinginto
astationary
liquid..............................................
02.4.2.
Bubblinginto
aflow
ingliquid
...............................................
02.4.3.
Breakupofbubbles
undershear
..............................................
02.4.4.
Gas
entrainment
atfreesurfaces
..............................................
02.5.
Bubblegeneration
without
topologicalchanges—
phasetransitions
..................................
03.
Techniquesoffoam
formation
.......................................................
03.1.
Introduction...........................................................
03.2.
Mechanicalfoam
ingtechniques
..................................................
03.2.1.
Foaming
bybubbling
intoastationary
liquid.........................................
03.2.2.
Foaming
viaco-injection
ofgasand
liquid..........................................
03.2.3.
Gas
entrainment
atfreesurfaces
andbubble
break-upunder
shear..............................
03.3.
Foaming
throughphase
transitionsand
byelectro-chem
istry.....................................
03.3.1.
Nucleation
andgrow
thofbubbles
insupersaturated
liquids..................................
03.3.2.
Cavitationand
boiling...................................................
03.3.3.
Foaming
byelectrolysis
..................................................
03.4.
Conclusionsand
outlook......................................................
0Acknow
ledgements
..............................................................
0References
..................................................................
0
1.Introduction
Liquidfoam
sconsistofgas
bubbleswhich
areclosely
packedwithin
aliquid
carriermatrix
[1–4].Coalescenceofthe
bubblesishindered
by
theaddition
ofstabilisingagents,w
hichmay
below
molecular
weight
surfactants,polymers,proteins,nano-particles,or
theirmixtures
[5].The
resultingnetw
orkof
gas/liquidinterfaces
providesliquid
foams
with
numerous
complex
anduseful
properties.Amongst
these
aretherm
alandacoustic
properties,orthe
factthat
theystrongly
scatterlight.M
ostexploited
aretheir
rheologicalproperties,sincethey
havethe
uniquefeature
thatthesam
efoam
may
behavelike
anelastic/plastic
Advances
inColloid
andInterface
Sciencexxx
(2015)xxx–xxx
⁎Corresponding
author.E-m
ailaddress:Wiebke.D
(W.D
renckhan).
CIS-01529;NoofPages
32
http://dx.doi.org/10.1016/j.cis.2015.04.0010001-8686/©
2015Elsevier
B.V.A
llrightsreserved.
Contents
listsavailable
atScienceD
irect
Advances
inColloid
andInterface
Science
journ
alhomepage:www.e
lsevie
r.com/lo
cate
/cis
Pleasecite
thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
solidor
likeaviscous
liquiddepending
onhow
itismanipulated.The
resultisthatliquid
foamshave
foundtheir
way
intonum
erousapplica-
tionsof
verydifferen
tkind,including
cosmetic
andlaundry
applica-tions,fire
fighting,oilrecovery,soilremidation
orfoam
fractionation.Liquid
foamsare
alsovery
important
astem
platesfor
thegeneration
ofsolidfoam
s.Lastbut
notat
alltheleast,foam
smay
alsooccur
asa
byproductin
man
ynaturalor
industrialprocesses.Inthe
lattercase,
their
presence
may
interferewith
productionin
aharm
fulmanner;
paperor
paintindustrybeing
themost
prominentexam
ples.The
physicalpropertiesofa
foamdepend
cruciallyon
itsstructural
properties—
suchas
thegas
fractionΦ
(=gas
volume/foam
volume)
orthe
bubblesize
distribution.Alarge
number
offoaming
techniqueshas
beendeveloped
inthe
pastinorder
toobtain
controloverthese
pa-ram
eters.Depen
dingon
thetechnique,bubble
sizesmay
rangefrom
microm
etresto
centimetres,bubbles
canbe
extremely
monodisperse
orhighly
polydisperse,andgas
fractionscan
bevaried
overthe
entirerange.U
nfortunately,tomost
users'despair,eachindividualtechnique
typicallycovers
onlyarelatively
smallrange
oftheseparam
eters.More-
over,thechoice
ofafoam
ingtechnique
isnotonly
guidedby
theprop-
ertiesofthe
obtainedfoam
,butalsoby
howrapidly
itcanbe
generated.Hence,any
academic
orindustrialfoam
ingapplication
needsto
startwith
awise
choiceofthe
appropriatefoam
ingtechnique(s)
—which
canbe
adaunting
task.Allfoam
ingtechniques
haveone
aspectincom
mon:the
generationofbubbles
within
aliquid.This
implies
thecreation
ofgas/liquidinter-
facesofinterfacialtension
γwhich,in
turn,implies
anenergy
inputof
atleastU=
4γrB 2
perbubble.For
typicalinterfacialtensionsand
bubblesizes,this
isman
yorders
ofmagnitude
largerthan
thermalenergies
(kT),which
means
thatbubbleform
ationisnot
aspontaneous
processand
thatoneneeds
toputa
lotofenergyinto
aliquid
inorder
tocreate
afoam
.Whatdistinguishes
thedifferentfoam
ingtechniques
ishow
ex-actly
onechooses
toputthis
energyinto
theliquid.This
may
bedone
byph
ysical,chemical
oreven
biologicalmeans
(seeTable
1).Physicalmeans
include
mechanical
action(gas
sparging,whipping,sh
aking,etc.)
orphasetransitions(boiling,cavitation,effervescence,etc.).Chem
-ical
techniquescreate
bubbleseith
erby
agas-releasing
chemicalor
electro-chemicalreaction
(electrolysis),while
themost
common
bio-logicalapproach
relieson
gas-generatingspecies
suchas
yeast.These
differenttechniqueslead
tothe
finalfoamin
aone-step
orina
two-step
process.Inaone-step
process,themechanism
which
gener-ates
thebubbles
leadsdirectly
tothefinalfoam
with
awell-defi
nedgas
fraction.O
nly
fewfoam
ingtechniques
allowfor
this.M
osttech-
niquesrely
ontw
otypes
oftwo-step
processes.Inthe
firstcase,loose
bubblesare
generatedin
theliquid
which
arethen
compacted
togive
thefinalfoam
—for
example
throughgravity
orpressure-driven
drain-age
oftheliquid.In
thesecond
case,theinitialbubbling
mechanism
cre-ates
acoarse
foamcontaining
largebubbles,w
hichare
thenbroken
intosm
allerbubbles
tocreate
thefinalfoam
.
Inorder
todescribe
thescience
offoaming
wehave
decidedto
takethe
following
approach:Firstofall,weconcentrate
onthe
descriptionof
physicalfoam
ingtechniques,leavin
gout
considerationsof
chemical
andbiological
foaming
(with
the
exceptionof
electro-chem
icalfoam
ing).Weprovide
firstadetailed
descriptionofthe
differentfunda-mentalm
echanismswhich
leadto
thecreation
ofisolatedbubbles
ina
liquid(Section
2).Wethen
continuewith
thedescription
ofcommonly
usedfoam
ingtech
niques(Section
3).Consideringthelarge
number
ofavailablefoam
ingtechniques,w
ehave
decidedto
stayon
thelevel
ofageneral
overview,providin
gthereader
mostly
with
themain
ideasofthe
differentconcepts
ortechniques,rather
thanwith
anin-
depthanalysis.W
ehope
that
this
canhelp
thereader
toorient
hisgeneralrefl
exionsbefore
goinginto
detailbyfollow
ingthe
providedreferences.
Beforeentering
intothe
analysis,somecom
ments
onthe
physico-chem
icalaspectsoffoam
ingare
required.Any
foaming
solutionneeds
tocontain
stabilisingagents
inorder
tocontrolthe
stabilityofthe
ob-tained
foam.It
isevident
thatthe
propertiesofthe
obtainedfoam
de-pend
sensitivelyon
thefactw
hetherbubble
coalescenceoccurs
duringthe
foaming
process.Infact,in
many
ofthemore
complex
foaming
tech-niques,the
finalfoamproperties
aregiven
byasubtle
equilibriumbe-
tween
bubblegeneration
andbubble
coalescence.
Moreover,
the
stabilisingagents
may
havecharacteristic
adsorptiontim
esor
energybarriers,w
hichneed
tobe
compared
with
thecharacteristic
generationtim
esand
energyinputofthe
foaming
process.Forexample,adsorption
times
playan
important
rolein
settingthe
interfacialtensionduring
bubblegeneration.Ifthe
bubblingprocess
isfaster
thanthe
equilibra-tion
timeofthe
interface,thesurface
tensionwillbe
between
thatof
thepure
solventand
theequilibrium
surfacetension,its
precisevalue
dependingon
thebubbling
speed[6].Last
butnot
least,thestabilising
agentsoften
confervisco-elastic
propertiesto
thegas/liquid
interfaces[7].This
may
addim
portantinterfacialstresses
duringthe
processof
bubblecreation
,which
may
altersign
ificantly
thefinally
obtained
foam.For
thesake
ofsimplicity,w
eshallneglect
allthesedifferent
ef-fects
inmostofourargum
entationsby
assuming
thatbubblesare
indef-initely
stableand
thattheirinterfaces
haveone
constantvalueγfor
theinterfacial
tensionwhich
isobtained
instantaneously
uponbubble
creation.The
formulation
ofthebulk
liquidcan
alsomodify
significantlythe
rheology
oftheliquid
phase,leading
eventuallyto
non-N
ewtonian
behaviourand
verydifferentconditions
forbubble
formation
[8,9].Fort he
sakeofclarity
wewilllim
itourdescriptionto
thefoam
ingofsim
ple,i.e.N
ewtonian
fluids.
2.Fundam
entals
offoamform
ation
2.1.Introduction
Inthis
sectionweshallconcentrate
onthe
descriptionofthe
funda-mentalm
echanismswhich
leadto
thegeneration
ofindividualbubbles.W
ehave
chosento
groupthem
intotw
oconceptually
differentcatego-ries.In
thefirstcategory,the
gas/liquidinterface
needsto
undergoato-
pologicalchangein
orderto
createthefinalbubble.This
topologicalchange
canoccur
inmany
differentways.The
most
common
onesare
sketchedin
Fig.1.Forexam
ple,abubble
may
detachfrom
anozzle
orfrom
adeform
edfree
surface;oralarge
bubblemay
breakinto
smaller
ones.Whatdifferentiates
thesemechanism
siswhich
ofthetw
ophases
isflow
ingand
underwhich
conditions.Thedifferent
mechanism
sare
discussedin
more
detailinSection
2.4.Evenifthe
initialmechanism
ofcreatingapocket-like
gas/liquidinterface
may
bevery
different,thefinalbreak-up
mechanism
which
leadsto
thetopologicalchange
isthe
same:
thegas/liquid
interfacehas
tobe
deformed
intoaslen
derfila-
ment
which
isphysically
unstableand
breaksto
make
thetopological
transition.Thephysics
ofthisinstability
isdescribed
inmore
detailinSection
2.3.
Table1
Classificationofdifferent
foaming
techniques.
Global
mechanism
Sub-mechanism
Examples
Physicalfoam
ingMechanical
foaming
Bubbling,sparging,foamgeneration
inporous
media,w
avebreaking,shaking,rotor–stator
mixers,kitchen
blender,doublesyringe
techniquePhase
transitionCham
pagne,beer,extrusion,cream
dispenser,shavingfoam
Chemical
foaming
Chemical
reactionFizzy
drinktablets,baking
powder,polyurethane
foaming
Electro-chemical
reactionMicroflotation
Biologicalfoam
ingYeast
Baking
2W.D
renckhan,A.Saint-Jalm
es/A
dvancesin
Colloidand
InterfaceScience
xxx(2015)
xxx–xxx
Pleasecite
thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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Inthe
secondcategory,no
topologicalchangeofthe
gas/liquidinter-
faceisrequired,as
afreely
floatingbubble
isdirectly
createdwithin
theliquid
byaph
asetransition
orby
achem
icalreaction
(Table1and
Fig.2).Thedifferent
physicalmechanism
softhis
kindofbubble
crea-tion
arediscussed
inmore
detailin
Section2.5.Som
emechanism
smay
belongto
bothclasses.For
example,phase
transitionsare
oftenfavoured
bythe
presenceofw
allsor
impurities
fromwhich
thebubbles
needto
detachvia
atopologicalchange.
Inboth
categories,anum
berofdifferentstresses
areinvolved
inthe
processofbubble
creation.Webriefly
reviewthese
inSection
2.2and
discusshow
theymay
begrouped
intonon-dim
ensionalnumbers
foracoherentdescription
ofdifferentbubblingprocesses.
2.2.Thephysics
ofdeforming
interfaces
Any
processofbubble
formation
involvesthe
creationand
deforma-
tionofa
gas/liquidinterface.Even
ifthefundam
entalmechanism
may
benon-m
echanicalinnature
(likechem
icalreactions),theactualcreation
processinvolves
anum
berofm
echanicalstresses(=
forceper
area)which
needto
beconsidered.O
neofthe
most
importantcontributions
isthat
ofthesurface
tensionγ,w
hichleads
toanorm
alstressσγand
thereforeto
apressure
dropΔpacross
acurved
surfaceofm
eancurva-
tureκdescribed
bythe
Young–Laplacelaw
[15]
σγ ¼
Δp¼
2γκ:
ð1Þ
Ofsim
ilarim
portanceisthe
influenceofa
hydrostaticpressure
dif-ference,w
hichleads
tothe
well-know
nbuoyancy
forceFBon
abubble
ofvolumeVB ,w
hichplays
amajor
rolein
bubbledetachm
entandcom
-paction.The
buoyancyforce
isgiven
by
FB ¼
ΔρgV
B :ð2Þ
Surfacetension
andgravitationalstresses
are“static”
stressessince
they
donot
requirefluid
motion
.In
adynam
iccon
textim
portant“dynam
icstresses”
may
arise.Thefirstone
isatangentialviscous
stressσV ,w
hichresults
fromaviscous
shearflow
attheinterface.Itdepends
onthefluid
viscosityηLand
thedeform
ationrate
dU/dLof
thefluid
andiscom
monly
approximated
as
σV ¼
ηL UL
;ð3Þ
where
Uisthe
characteristicflow
velocityand
Lacharacteristic
lengthscale
oftheflow
.Generally
onehas
twoviscous
contributions,on
efrom
thegas
andone
fromthe
liquidphase.V
iscousflow
canalso
leadto
theoccurrence
ofadynam
icpressure,hen
ceexerting
additional
Fig.1.Differentroutes
ofbubblegeneration
which
requireatopologicalchange
to“pinch-off”
oneor
more
bubblesfrom
amain
gasbody
(bubblingfrom
nozzlefrom
[10],effervescencefrom
[11],co-flowfrom
PhDthesis
Jan-PaulRaven,cross-flowfrom
[12],air-entrainmentinspired
by[13],breakup
undershear
from[14]).“A
ctive”or
“Passive”refers
towhether
ornot
thecorresponding
phaseisflow
ingactively
inthe
process.
Fig.2.Sketchofthe
twomain
routesofbubble
generationby
physicalmeansw
hichdo
notrequire
atopologicalchange
oftheinterface.The
firstcreatesbubbles
viacavitation,boil-
ingor
effervescence.Inthe
second,thedrops
ofanem
ulsionturn
intoagas,generally
uponpressure
release.
3W.D
renckhan,A.Saint-Jalm
es/A
dvancesin
Colloidand
InterfaceScience
xxx(2015)
xxx–xxx
Pleasecite
thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
normalstresses
onan
interface.Gases
orliquids
inmotion
alsoexert
normalin
ertialstressesσI on
aninterface
dueto
themom
entum
ofthe
flow.These
stressesmay
beapproxim
atedas
σI ¼
ρU2:
ð4Þ
Asdiscussed
inSection
2.1,thepresen
ceof
stabilisingagents
cangive
riseto
important
interfacialstresses[16]
which
caninterfere
with
bubblegeneration
innon
-negligible
manner
[17,18].Other
stressesmay
actin
specificallydesigned
systemswhich
make
useofacoustic,
electricorm
agneticforces.Forsim
plicity,wewillnotconsiderexplicitly
anyofthese
latterstresses
here.Generally,allthe
above-mentioned
stressesactsim
ultaneouslyduring
theprocess
ofbubblegeneration.H
owever,in
most
cases,someofthe
contributionsdom
inatewhile
otherscan
beneglected.O
necom
monly
distinguishesbetw
eena“quasi-static”
anda“dynam
ic”regim
e.Inthe
quasi-staticregim
e,theflow
velocitiesare
sufficientlysm
allsothatthe
systemcan
beassum
edto
progressvia
asequence
ofstaticstates.Such
processesare
thereforeindependentofthe
flowvelocities.In
thedynam
icregim
e,viscousand/orinertialforcesneedto
betaken
intoaccount.In
thisregim
ethe
bubbleform
ationisoften
dominated
byone
ofthetw
ocontri-
butions,which
iswhy
onecom
monly
distinguishesbetw
eena“viscosity-
dominated”
andan
“inertia-dominated”
regime.
One
way
tonavigate
thecom
plexityof
thedifferent
stressesis
towork
with
non-dim
ensionalnumbers
which
allowsto
measure
ina
(somew
hat)more
quantitativeway
therelative
importance
ofeachof
theacting
stresses.Table
2sum
marises
themost
important
non-
dimensionalnum
berswhich
areused
inthe
descriptionofbubble
for-mation
.Theuse
ofthese
numbers
canbe
extremely
powerful
sincethey
providean
important
degreeofabstraction
bygrouping
togetherdifferent
parameters
usingsim
ple“scaling
arguments”.M
ostofthese
numbersare
usedthroughoutthisarticle
inorderto
classifydifferentre-
gimes
offoaming
techniques.The
definitionofthe
dimensionless
numbers
involvesthe
following
parameters:surface
tensionγ,density
ρ,viscosityηand
thegravitation-
alaccelerationg.M
oreover,itrelies
onacharacteristic
velocityUand
acharacteristic
lengthscale
L.Thelatter
twoparam
etersneed
tobe
cho-sen
with
care,asmost
flowproblem
sinvolve
complex
flowfields
andflow
geometries,hen
ceawide
rangeof
velocitiesand
lengthscales.
Moreover,
theproblem
sdeal
with
two-ph
aseflow
s;on
etherefore
needsto
choosewisely,ifthe
stressesofone
ofthephases
dominate
thebehaviour,or
ifbothneed
tobe
takeninto
account.Good
choicesofthese
parameters
arediscussed
inmore
detailthroughoutthisarticle.
Another
frequentlyused
parameter
isthe
capillarylength
lc ¼ffiffiffiffiffiffiffiffiffiffiffiγΔρg
r;
ð12Þ
which
isadim
ensionalexpressionofthe
Bondnum
ber.Itprovidesachar-
acteristiclength
beyondwhich
gravitationaleffectsneed
tobe
takeninto
accountin
comparison
tosurface
tensioneffects.Last
butnot
least,theviscosity,density
andflow
rateratio
ofthegas
(“G”)
andthe
liquid(“L”)
phase
λV ¼
ηG
ηL;λD ¼
ρG
ρL;and
λQ¼
QG
QL;
ð13Þ
areoften
takeninto
accountinthe
descriptionofbubble
formation.
Num
erousothernon-dim
ensionalnumbers
exist,forexam
ple,ifthevisco-elasticity
ofthe
interfaceswas
tobe
takeninto
account.The
interfacialmobility
may
beused
toas
ameasure
oftheinterfacialviscos-
ity,while
theMarangoninum
bercaptures
theim
portanceofan
interfa-cialelasticity
[3,7].
2.3.Thephysics
ofrupturinggas
ligaments
Here
weshalldiscuss
indetailthe
physicsofhow
thebubble
undercreation
undergoesthe
topologicalchangeto
detachfrom
anobject,a
freesurface
ora“m
other”bubble.M
anydifferent
configuration
scan
leadto
this
final
stageand
aselection
isdiscussed
indetail
inSection
2.4.How
ever,inallcases,the
physicsofthe
finalstepleading
tothe
topologicalchangeisthe
same(Fig.3):the
bubblehas
tobe
de-form
edinto
anelon
gatedcylinder
(or“gas
thread”,or
“ligament”),
which
becomes
physicallyunstable
andbreaks.Ifthe
cylinderis
rela-tively
shortwith
respectto
itswidth,it
breaksin
onepoint
toliberate
onebubble
(Fig.3a).Ifitis
verylong,it
canbreak
intomany
bubbles(Fig.3b).
Tounderstand
thisbreak-up
letusconsider
thephysics
ofalong
cy-lindricalligam
entofonefluid
within
another.Thiscan
beagas
ligament
inaliquid,a
liquidligam
entin
agas,or
aliquid
ligament
inasecond
immiscible
liquid.The
thinner
suchaligam
entis,
thehigher
isits
Table2
Summary
ofthemostim
portantdimensionless
numbers
usedto
classifydifferentregim
esofbubble
generationand
theircross-relations.
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renckhan,A.Saint-Jalm
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as:Drenckhan
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esA,The
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ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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surface-to-volumeratio.
Itwould
therefore
energeticallybe
more
favourableto
turnthe
cylinderinto
anum
berofsphericalobjects.But
thekey
questionis:how
doesthe
systemgetthere?
Thistransition
hap-pens
viaan
instabilitywhich
linksthe
ligamentcurvature
andpressure
viathe
Young–Laplaceequation
(Eq.(1)).Thisissue
hasbeen
widely
studied,andthe
understandingof
thekey
mechanism
sgoes
backto
the19th
centuryand
thepioneering
works
ofSavart,Plateauand
Ray-leigh
who
were
tryingto
understandthe
destabilisationofa
water
jetas
itfallsoutofa
faucet.Implem
entingthe
ideasofSavart[21]and
Pla-teau
[22],Rayleighdeveloped
afirst
basicmodel[23],w
hich
isnow
knownas
the“Rayleigh–Plateau
instability”.Rayleighconsidered
acy-
lindrical,infinite
thread
ofan
inviscid
fluid
inair,w
ithoutexternal
flow.Such
afluid
columnexperiences
spontaneousthickness
undula-tions
(called“varicosity”,Fig.4a)
which
aregenerally
damped.H
owev-
er,Rayleigh
couldshow
thatunder
certaincon
ditions,som
eof
the
undulationscan
actuallygrow
with
timerendering
acertain
rangeof
“varicose”modes
unstable.Thiscannot
beunderstood
ifoneconsiders
onlythe
pressuregradientsarising
frommodulations
ofthecross-section
(ofradiusr)
oftheligam
ent.Infact,as
sketchedin
Fig.4a,theYoung–La-
placelaw
includesalso
theradius
r′,inthe
planeorthogonalto
thecross-
section,andassociated
with
thedeform
ationmode
(andwith
thedefor-
mation
wavelength
λ).Inparticular,w
henthe
cross-sectiongets
small,
thereis
asaddle
pointand
thetw
ocurvatures
havedifferent
signs.Thus,depending
onwhich
radius(r
orr′)
isthe
biggest,adifferent
behaviourwillbe
found.Qualitatively,m
odesassociated
with
larger′
(wavelength
longerthan
theligam
entsection)
willbe
unstable,andvice
versa.Performing
thedetailed
mathem
aticalanalysis
assuming
thatinertiaisbalancing
surfacetension,one
obtainsthatthe
modes
hav-ing
apositive
growth
rate(sketched
inFig.4b)
arethose
whose
wave
number
k(k
=2π
/λ)fulfils
krb1:
ð14Þ
Themaxim
umin
Fi g.4bcorresponds
tothe
most“dangerous”
mode
which
iscalled
the“Rayleigh
mode”.It
isgiven
by
kr¼0:697
andλ¼
9:02r:
ð15Þ
Anim
portantpointisthatalltheunstable
modesare
finiteand
oftheorderofthe
threadradius(butsom
ewhatlargerthan
thethread
radius).Since
thefinalbubble
ordropletsizeisofthe
orderofthewavelength
ofthe
mostunstable
mode,itis
generallyalinearfunction
ofthethread
ra-dius
atwhich
theinstability
occurs.Another
interestingoutput
isthe
capillarytim
escaleassociated
with
thesedeform
ations[24]
τcap ¼
ffiffiffiffiffiffiffiffir 3ργ
s;
ð16Þ
Fig.4.TheRayleigh–Plateau
instability:(a)Schem
eshow
ingthe
differentradiiofcurvature.(b)Grow
thrate
asafunction
oftheundulation
wave
number
k=
2π/λ
multiplied
bythe
threadradius
r.(c,d)Tim
eevolution
ofunstableligam
entsof(c)
twopolym
ericfluids
[27],ofa(d)
gasligam
entin
aviscous
liquidconfined
inatube
(from[28]).
Fig.3.Theinstability
ofthingas
ligaments
leadsto
thetopologicalchange
ofthegas/liquid
interfacerequired
tocreate
oneorm
oreseparate
bubbles.(a)Bubble
pinch-offinwater/glycerol
mixtures
ofincreasingliquid
viscosityηL (from
[19]).(b)Pinch-offofa
gasbubble
containinginsoluble
SF6forη
L =0.03
Pas,show
ingthe
generationofm
anytiny
satellitebubbles
duringthe
detachment
ofthemain
bubble(tim
ebetw
eenim
ages:5μs.Scale
bar50
μm)(from
[20]).
5W.D
renckhan,A.Saint-Jalm
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thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
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ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
which
providesan
approximation
asto
howrapidly
athread
willbe-
comeunstable.
Rayleigh'ssim
plemodelw
asexpanded
inmany
differentways
inorder
todescribe
more
realisticscenarios.W
eber[25]
was
oneofthe
firsttotake
intoaccountthe
viscosityofthe
fluidofthe
cylinder.Hisre-
sultscan
berationalised
usingthe
Ohnesorge
number
Oh(Eq.(10)
inTable
2)which
canalso
beconsidered
asthe
ratioofthe
viscoustim
e-scale
overthe
capillarytim
escale
([24,26]and
references
therein).
Thestability
ofthefluid
cylinder
decreaseswith
decreasingOh,and
thegrow
thrate
andthe
wavelength
ofthemost
unstablemode
canbe
calculatedusin
gthis
“viscous”Rayleigh–Plateau
instability([24,26]
andreferences
therein).Rem
ainingin
thesituation
ofstationaryliquids
(noflow
insideor
outsidethe
cylinder),theratio
λVof
theviscosities
ofthe
innerand
outerfluidcan
betaken
intoaccount[29].The
mostunstable
wavelength
dependson
theviscosity
ratio,beingmaxim
umwhen
λV≈
1.Consider-ing
thecase
ofagas
cylinderinsidealiquid
(λV≈
1/55)
themostunsta-
blewavelength
ispredictedto
beλ=
12.5r—which
remains
closeto
thebasic
prediction(Eq.(15))
ofRayleigh.Mostsituations
which
leadto
theform
ationoflong
cylindricalliga-ments
requirethat
thefluid
insideand/or
outsidethe
ligamen
tis
flowing
(Fig.1).Inthis
case,the“tem
poralinstability”discussed
upto
nowisoften
notsufficient.One
mustalso
considerthe
“spatialinstabil-ity”,m
eaningthat
aninitially
localiseddeform
ationpropagates
alsoalong
theligam
entaxis.Researchers
havetherefore
identifiedtw
odif-
ferentscenariosforthe
instabilityto
occur:the“absolute”
andthe
“con-vective”
instability([30]and
referencestherein).
Anabsolute
instabilitycorresponds
toadeform
ationwhich
grows
toofastin
timeand
spaceto
beconvected
bythe
main
flow,itthusprop-
agatesboth
downstream
andupstream
,invadingthe
whole
ligament,
independentlyofthe
flow.A
tafixed
pointinspace,the
growth
ofanun-
stablemode
isnever
limited.By
contrast,theconvective
instabilityim
-plies
perturbationswhich
areconvected
downstream
while
theygrow
.Atagiven
pointin
space,theam
plitudeof
thedeform
ationrem
ains
finite,asthe
flowisfastenough
tosw
eepthe
deformation
away
beforeitbecom
esexponentially
large.Theconvective
regimeallow
sfor
acon-
tinuousand
longerfluidligam
enttosurvive,w
hencom
paredto
theab-
soluteregim
e.Within
thesam
ebubbling
conditionsone
cantypically
switch
between
bothscen
ariosby
appropriatelyadjusting
theflow
ratesofboth
phases.Theconsequences
ofthesedifferent
behavioursare
particularlywellevidenced
anddiscussed
inmore
detailwhen
bub-bles
areblow
nfrom
nozzles(Sections
2.4.1and
2.4.2.)Let
usfinish
with
twoim
portantrem
arks.A
ligament
doesnot
necessarilybreak
into
equal-volumebubbles.Sm
allbubbles
(called“satellite
bubbles”)can
resultfrom
thefinalstep
ofrupture
(Figs.3band
4c).Thisis
discussedin
more
detailinSection
2.4.3.Lastbut
notleast,it
isim
portantto
keepin
mind
that
geometrical
confinem
enthas
adram
aticeffecton
ligamentcurvatures
andtherefore
onits
stabil-ity.In
fact,ifaligam
entisconfinedin
onedirection
(forexample
inaflat
channel)itrem
ainsstableuntilthe
confine mentis
released[27,31].This
canprovide
anim
portantdegreeofcontroloverbubble
formation
andis
oftenused
inmicrofluidic
contexts.
2.4.Bubblegeneration
requiringtopologicalchanges
Many
differentmechanism
sexist
which
allowto
detachabubble
fromagas
pocket.Oneof
themost
common
approachesuses
the
gravity-drivendetachm
entof
abubble
which
isblow
nat
constant
pressureor
flow
rateinto
astation
arysolution
viaan
orifice
(Fig.1and
Section2.4.1).Since
gravityisnotvery
efficientwhen
smalllength
scalesare
involved(sm
allBondnum
bersBo
—Table
2),many
bubblingmechanism
sinvolve
aco-flow
oftheliquid
inorder
tomake
useofvis-
cousor
inertialforcesto
influencethe
break-upprocess.This
co-flowmay
occurinunconfined
conditions—
forexample
onecan
move
anoz-
zlethrough
thefoam
ingsolution.Butin
many
casesitismore
suitableto
work
inconfined
geometries
inwhich
dynamicstresses
canbe
imposed
more
efficientlyand
inabetter
controlledmanner.W
ediscuss
herein
particularthecase
ofconfi
nedco-fl
owand
cross-flow
(Fig.1
andSection
2.4.2).Another
important
mechanism
includesthe
entrainment
ofairat
freesurfaces
(Fig.1and
Section2.4.1)
andthe
breakupoflarge
bubblesinto
smaller
onesunder
shearflow
(Fig.1and
Section2).
Forsim
plicity,weshalldiscus
thevarious
flowproblem
sin
termsof
“flowrates
Q”and
“flowvelocities
U”.This
means
thatthepressures
ad-just
toensure
aconstantflow
rate.Inmany
experimentalscenarios
itis
more
practicaltocontrolthe
pressuresandmeasure
theflow
rates,forex-am
pleto
avoidlong
equilibrationtim
es.Thismeans,how
ever,thatflowrates
arenot
constantand
thephysicaldescription
issom
etimes
more
awkw
ard.Itcanalso
changenon-negligibly
thebehaviour
ofadevice.
2.4.1.Bubblinginto
astationary
liquidDue
toth
etech
nical
importan
ceof
the
process
ofbu
bbling
throu
ghorifi
ce s,thesu
bjecthas
beeninvestigated
inten
sivelyin
thepast.W
hileslow
bubblingcan
bedescribed
inafairly
straightfor-
ward
man
ner
(Section2.4.1.1)
thedescription
ofthedyn
amic
casehas
provento
behigh
lycom
plex(Section
2.4.1.2).This
complexity
isdueto
differen
tfeed
backmech
anism
swith
inth
esystem
,th
emost
importan
ton
ebein
gth
eintricate
couplin
gbetw
eenth
edy-
namic
forcesand
thebubble
shape.Moreover,the
physicsofth
edy-
nam
icsof
thecon
tactan
glebetw
eenth
einterface
andth
eorifi
ce,an
dof
thefinalbreak-u
pmech
anism
(s)are
only
beingelu
cidated
now.The
resultisthatdespite
theavailability
ofsomereview
articles[32,33],th
esu
bjectrem
ainsqu
itescattered
with
differen
tau
thors
presen
ting
differen
tparam
eterran
ges(su
rfaceten
sion,orifi
cedim
ension
san
dsh
ape,wettin
gcon
ditions,liquid
viscosity,gasan
dliq
uid
den
sity,etc.).
Sometim
esth
eresu
ltsseem
contrad
ictory.How
ever,inmost
casesth
esecon
tradiction
sresu
ltfrom
thefact
that
experimen
tsare
donein
differentregim
eswhere
differentpa-
rameters
may
have
avery
differen
t—
evenop
posite
—influen
ce.The
samechallen
geholds
formodelling
attempts
which
necessarilyneed
tosim
plifyth
eproblem
.Theappropriate
approximation
sde-
pen
don
ceagain
onth
ebu
bblingregim
e,which
has
ledto
avast
number
oftheoreticaland(sem
i-)empiricalm
odels,eachdescribing
generally
acertain
parameter
range
only.A
nexten
siveoverview
ofexisting
models
isgiven
inTable
3in
reference
[33].Wesh
allpresenthere
someofthe
keyingredients.
2.4.1.1.Thequasi-static
regime.A
tthe
outset,letus
discussthe
simple
scenario
ofbubblin
gat
constantgas
flow
rateQGinto
astationary
foaming
solutionusing
averticalorifice
ofcircularcross-sectionand
ra-dius
RO(see
Figs.1and
5).Letusassum
ethatthe
bubblingoccurs
suffi-ciently
slowly
tobe
inthe
quasi-staticregim
e(Fig.5),i.e.Ca
≪1and
We≪
1(Table
2),andthatthe
generationprocess
istherefore
dominat-
edby
surfacetension
andgravitationalforces
(buoyancy).Ph
otographsand
simulations
ofa
typicalquasi-static
blowing
processare
shown
inFig.
6a.During
this
processthebubble
goesthrough
awell-defined
seriesofpressure
stateswhich
aresketched
inFig.6b.The
pressureinitially
increases
(which
somerefer
toas
the
“nucleationstage”)
beforereaching
amaxim
umwhen
thebubble
isa
hemisphere,i.e.w
henthe
bubbleradius
RBisequalto
theorifice
radiusRO .A
tthis
point
ΔPmax ¼
2γRO;
ð17Þ
which
followsnaturally
fromthe
Young–Laplace
law(Eq.(1)).This
pressureis
important,as
anybubblin
gapplication
needsto
providepressures
abovethis
value.Due
tothe
inversedependence
oftheblow
-ing
pressureon
theorifice
radius,thepressures
forvery
smallorifices
may
becomeofthe
orderofa
fewbar,w
hichcan
beunfeasible
forcer-
tainapplications.
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renckhan,A.Saint-Jalm
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W,Saint-Jalm
esA,The
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ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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Acertain
reductionofthe
maxim
umpressure
may
beobtained
usingorifices
with
more
complex
geometricalcross-sections
[159].Ifthe
appliedpressure
ishigher
thanthe
maxim
umpressure,the
bubblegrow
sbeyond
thehem
isphericalshape(leading
toapressure
decrease)and
detachesvia
theinstability
mechanism
sdiscussed
inSection
2.3when
thesurface
tensionforce
Fγ(w
hichkeeps
thebubble
“stuck”to
theorifi
ce)is
oftheorder
ofthebuoyancy
forceFG .If
the
orificesize
ROismuch
smaller
thanthe
capillarylength
(Eq.(10)),i.e.ifR
O≪
lc ,onemay
approximate
theshape
ofthedetaching
bubbleby
asphere
ofvolume4/3π
RB 3.This
leadsto
abuoyancy
forceof
FG=
4/
3ΔρgR
B 3,while
thesurface
tensionforce
canbe
written
asFγ=
2πγRO .
RBmay
thereforebe
approximated
as
RB �
γΔρg
��
2=3R
1=3
O¼
l 2=3
cR
1=3
O¼
ROBo
−1=
3for
RO ≪
lcð
Þ;ð18Þ
where
thelen
gthscale
Lin
thedefi
nition
ofth
eBon
dnumber
Bo(Eq.(5))
has
beench
osento
betheradius
oftheorifi
ceRO .In
order
Fig.5.Variation
ofbubblingregim
ewith
increasingflow
velocities.Theblack
arrowindicates
where
break-upoccurs.
Fig.6.Blowing
bubblesfrom
anorifice
intoastationary
solution.(a)Bubble
evolutionas
afunction
oftimefor
twodifferentorifice
materials
(wetting
andnon-w
etting)com
paringeach
timephotographs
froman
experiment(top
row)and
computer
simulations
(bottomrow
)(adapted
from[36]).(b)
Schematic
pressureevolution
duringthe
generation.(c)Finalbubble
volumeas
afunction
oforificewetting
properties(expressed
incontactangle)
fortw
odifferent
orificediam
eters(adapted
from[37]).
7W.D
renckhan,A.Saint-Jalm
es/A
dvancesin
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as:Drenckhan
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esA,The
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ing,Adv
ColloidInterface
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forthe
bubbleto
detach,Botherefore
needsto
beatleastofthe
orderofunity.
Ifth
eorifi
cerad
iusis
ofth
eord
erof
thecap
illarylen
gth,i.e.
RO≥lc ,on
eneeds
totake
into
accountth
egravity-driven
deforma-
tionof
thebu
bblebefore
detachmen
t.Research
ersfindth
atth
isis
wellcap
tured
bysligh
tlymod
ifyingth
eexp
onen
tin
Eq.(18)su
chthat
RB �
RO Bo
−α=
3for
RO≥lc
ðÞ;
ð19Þ
with
α≈
1.06[34].In
bothcases,it
isclear
thatthebubble
sizeisset
bytheorifi
cedim
ensionsand
bythe
capillarylength
lcwith
smaller
orifices
leadingto
smaller
thebubbles.Sin
cethis
isnot
astrong
de-pen
denceitisoften
more
appropriateto
work
with
co-flow
scenari-
os(Section
2.4.2),especially
ifsm
allbubbles
andhigh
prod
uction
ratesare
needed.Th
epinch
-offprocess
(seealso
Section2.3)
isgen
erallymuch
fasterthan
thebubble
blowing
process,which
iswhy
itsduration
iscom
mon
lyneglected
inmodels.A
fterthepinch
-offthegas
thread
re-tracts
fullyback
to(often
eveninto)
theorifi
ceand
theperiodic
pro-cess
restarts.Due
tothe
periodicityofthis
process,foamsgen
eratedvia
bubblin
gin
thequ
asi-staticregim
eten
dto
behigh
lymon
odis-
perse.
Typical
bubble
sizeswhich
canbe
prod
uced
with
this
ap-
proach
arebetw
eena
fewhundred
microm
etresan
da
fewmillim
etres.In
somecases,on
emay
belookin
gto
prod
uce
largebu
bbles.Alook
atEq.(18)
suggests
theuse
ofalarge
orifice
forth
ispurp
ose.How
ever,when
thesize
ofth
eorifi
ceis
largerth
anth
ecap
illarylength
lcone
has
todealw
ithgravity-driven
instabilitiesofthe
gas/liquid
interface
leadingto
aneffect
called“w
eaping”
(liquiden
terstheorifi
ce).Anelegan
tapproach
isto
“tune”
gravityinstead
bylet-
tingthe
bubblegrow
underneath
aninclined
plane(Fig.7)
[35].The
pre-factorsin
Eqs.(18)an
d(19)
areofthe
orderofunity,but
dependsensitively
onthe
geometry
oftheorifi
ceand
onits
wettin
gprop
ertieswith
respect
toth
efoam
ingliqu
id.Th
emore
theliqu
idwets
theorifi
ce,themore
thegas
thread
remain
sconfi
ned
with
inthe
orifice
boundaries,leadingto
smaller
bubblesand
toaclearer
de-pen
denceofthe
bubblesize
onthe
orifice
dimensions.This
issh
own
intheim
agesequences
inFig.6a
(adaptedfrom
[36])and
alsoin
thefinalbubble
sizemeasurem
entsofFig.6c
(adaptedfrom
[37]),which
show
show
thebu
bblesize
dep
endson
thewettin
gcon
dition
s(expressed
bythe
contactangle
oftheliquid
onthe
nozzlematerial).
Italso
show
sth
atth
eorifi
cesize
plays
aless
importan
trole
inth
ecase
ofanon-w
ettingorifi
ce.Eq.(18)
allowsus
toapproxim
atein
which
rangeoffl
owrates
we
canapproxim
atethebubbling
processas
quasi-static.Since
viscousforces
tendto
play
amore
importan
trole
atlow
ervelocities
than
inertialforces,w
emay
requirethat
Ca≪
1,hence
QG ¼
UπR2O ≪
γηπR2O:
ð20Þ
Using
Eq.(18),wecan
calculateacorresponding
bubblingfrequency
fBfB ¼
QG
VB≪
Δρg
ηRO:
ð21Þ
Thisgives
fB≪
100fora
nozzlewith
RO=
100μm
.Bubblingfrequen-
ciesin
thetruly
quasi-staticregim
eare
therefore
rarelyabove
afew
bubblesper
second,which
istoo
slowfor
most
applicationswhich
thereforetend
tobe
runin
adynam
icregim
e(Section
2.4.1.2).
2.4.1.2.Thedynam
icregim
e.Upon
moving
away
fromquasi-static
bub-bling
conditions,differentdynamic
forcesneed
tobe
consideredin
thebubbling
processwhich
aresketched
inFig.8a.For
example,viscous
dragexerted
bythe
liquidon
thebubble
slowsdow
nthe
detachment
andtherefore
leadsto
largerbubbles.Bubbledetachm
entisalso
resistedby
inertialforcesofthe
liquid,while
theinertialforces
ofthegas
helpin
pushingthe
bubbleaw
ayfrom
theorifice.
Images
ofthebubble
generationprocess
with
increasinggas
flowrate
aresketched
inFig.5
andsom
ecorresponding
graphsin
Fig.8b.Ifsurface
tensionand
inertialforcescan
beneglected,researchers
find
[38]thatthe
resultingbubble
sizemay
beapproxim
atedby
RB �
ηL Q
G
Δρg
��
1=4�
RO
CaBo
��
1=4;
ð22Þ
where
theconstant
ofproportionalityisoforder
1and
dependson
theorifi
cecon
ditions(geom
etry,wetting).
Theim
portantobservation
hereisthat
unlikein
thequasi-static
regime,the
bubblesize
nowde-
pendson
theviscosity
ηLofthe
liquidand
thegas
flowrate
QG .M
orespecifically,the
bubblesize
increaseswith
ηLand
QG .
Upon
furtherincrease
ofQG ,inertial
forcesbegin
toplay
anon
-negligible
role(W
eGN1).W
ithgrow
ingW
ebernum
berWeGof
the
gas,theform
ingbubble
becomes
more
elongated,sinceinertialforces
becomeincreasingly
important
with
respectto
therestoring
surfacetension
forces.Thepinch-offpointofthe
gasthread
moves
increasinglyaw
ayfrom
theorifice,leading
eventuallyto
theform
ationofa
gas-jetwhich
breaksup
intobubbles
atits
tip.Thisjet
widens
away
fromthe
nozzle,asthe
gasisdecelerated
dueto
viscousfriction.For
sufficientlyhigh
WeG ,bubble
detachmentisentirely
drivenby
thedynam
icallygen-
eratedbubble
shape.Theinfluence
ofgravitybecom
esthereforenegligi-
ble,which
hasalso
beenconfirm
edin
micro-gravity
experiments
[39].One
cantherefore
thinkoftw
oextrem
escenarios,one
inwhich
bub-ble
pinch-offisdriven
entirelyby
gravity(Bo
N1)
versusone
where
itisdriven
byinertialforces.W
henthe
bubbleform
ationisdom
inatedby
gravityand
viscousforces,one
generallyspeaks
ofthe“dripping”
re-gim
e(in
analogyto
thedripping
tapproblem
).When
inertialforcesdom
inate,onespeaks
ofthe“jetting
regime”.A
number
oftheoreticaland
experimen
talstudies
havesh
ownthat
inertial
forcesdom
inatethe
pinch-offwhen
WeGN1–10
[33,39–41].Inmost
situations,gravityand
inertia
acttogether,
which
issh
own
intheph
asediagram
inFig.
8b,which
usestheBo
and
theWeGnum
berto
predictunder
Fig.7.Blowing
largebubbles
viatuning
theeffective
gravityacting
onthe
bubble.(a)Schem
aticrepresentation.(b)
Experimentalrealisation
from[35].
8W.D
renckhan,A.Saint-Jalm
es/A
dvancesin
Colloidand
InterfaceScience
xxx(2015)
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thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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which
flowconditions
bubbledetachm
entoccurs
(unstableregion).A
number
ofstudieshave
investigatedthe
transitionfrom
thedripping
tothe
jettingregim
e—
andwewilldiscuss
thephysics
ofthesetransi-
tionsin
more
detailwhen
discussingbubbling
underco-flowconditions
inSection
2.4.2.What
isim
portantto
noteat
thispoint
isthat
atthe
transition,importantnon-lineareffects
canplay
arole,leading
tomulti-
plebubble
periodsand
evenchaotic
bubbling.Thisleads
tofoam
swith
bubblesofm
ultipleorpolydisperse
sizesand
isdiscussed
inmore
detailin
Section3.2.1.1.
Ifsurfacetension
andviscousforces
canbe
neglected,thebubble
sizein
theinertialregim
emay
beapproxim
atedby
[32,38]
RB �
Q2=
5G
g1=
5 �ROFrG
2=5¼
RO
WeG
Bo
��
1=5;
ð23Þ
where
thefactor
ofproportionalityisoforder
one,itsvalue
dependingon
themodelused.In
thisregim
epolydispersity
ofthebubbles
tendsto
increasesignificantly.
Inmostpracticalcases,gravity,surface
tension,viscosityand
inertiaact
simultaneously.In
thiscase,the
modelneeds
totake
intoaccount
thevarious
contributions,renderingitquite
complex.O
neofthe
fre-quently
usedmodels
isthe
oneproposed
byJam
ialahmadietal.[42]
RB ¼
RO
5:0
Bo1:08 þ
9:261
FrG0:36
GaG0:39
þ2:14
FrG0:51
"#
1=3:
ð24Þ
Notice
theim
portanceofthe
Froudenum
berFr,w
hichcaptures
theratio
ofinertial
andgravitational
stressesand
which
canalso
beexpressed
asFr
2=
We/Bo
inorder
tomake
thelin
kwith
previousdiscussions.
2.4.2.Bubblinginto
aflow
ingliquid
Scientistshave
developedalarge
number
ofbubbling
techniques
which
involvethe
activeflow
oftheliquid
phase.Thiscreates
additionalviscous
andinertial
forceswhich
canplay
avery
important
rolein
bubbledetachm
ent.Thefirst
groupoftechniques
involvesthe
co-flow(Fig.9a,b)
orthe
cross-flow(Fig.9c)
inunconfined
conditions.Thelat-
termay
beachieved
bydragging
theorifice
throughalarge
liquidpool,
anapproach
originallyused
byBragg
[43]toblow
smallbubbles.The
in-fluence
oftheflow
ingliquid
phasecan
beincreased
ifco-or
cross-flowtake
placeunder
confinedconditions
(Fig.9d–g),sincehigh
shearrates
andhigh
flowvelocities
canbe
obtainedin
theconfined
flowregions.
Theconfining
geometry
thereforeplays
anim
portantrole
inthe
bub-bling
process,asitfixes
theflow
fieldand
thereforethe
dynamicforces
actingon
thebubble.Sm
ithwas
oneofthe
firstscientiststo
usethis
ap-proach
systematically
inorderto
blowsm
all(er)bubbles
forBragg
[44].Tow
ardsthe
endofthe
20thcentury
thesubjecthas
foundan
explosiverebirth
with
emerging
microfl
uidictechniques
[45–49].Amore
sub-stantialbody
ofwork
hasbeen
doneon
droplet,ratherthanbubble
gen-eration,
butwith
many
physical
mechanism
sbeing
thesam
e,the
interestedreader
willfind
important
inspirationin
thedroplet
litera-ture
[50–52].Inmost
oftheconfined
co/cross-flowdevices,the
influ-en
ceof
gravitycan
beneglected
becauseof
the
small
devicedim
ensions(i.e.
Bo≪
1)or
theim
portanceof
thedynam
icforces
(Ca≫
1,and/orW
e≫
1, etc.).Thisiswhy
wewillnotdiscuss
theinflu-
enceofgravity
inthe
following.
2.4.2.1.Thequasi-static
regime.W
henboth,the
gasand
theliquid
flowrate,are
smallenough
sothatthe
dynamicforces
canbe
neglected,un-confined
flowgives
thesam
eresults
asbubble
blowing
intoastationary
liquid(Section
2.4.1).Inthe
absenceofgravity
thereisno
detachment
force,hencebubbles
cannotbe
generated.Thisis
verydifferent
when
thebubble
isgenerated
under
appropriatelyconfi
nedconditions.In
this
case,thebubble
canblock
theen
tirechannel
orconstriction
inwhich
itisgenerated.The
liquidflow
thenleads
toafilling
ofthechan-
nelortheconstriction,w
hichpinches
offthebubble
(Fig.1).Thebubble
iscarried
away
bythe
slowflow
andthe
periodicprocess
restarts.Thisregim
ehas
beencalled
the“squeezing”
regime[48]
sinceitisentirely
controlledby
thenorm
alpressuresacting
onthe
interface.Sincethe
bubblecontinues
tobe
blownatconstantflow
rateQGwhile
theliquid
fillsthe
constrictionofvolum
eVcat
constantflow
rateQL ,one
findsa
simple
relationshipwhich
relatesthe
finalbubblevolum
eto
thechan-
nelgeometry
andthe
flowrates
toagood
approximation
[53,54]
VB
�VCQ
G
QL:
ð25Þ
Theprefactor
dependson
theprecise
geometry.The
volumeofthe
constrictionmay
bereplaced
bythe
3rdpow
erofa
characteristicchan-
neldimension,ifthe
geometry
doesnotcontain
awell-defined
constric-tion.W
iththis
approach,onecan
thereforegenerate
foamsover
awide
rangeofbubble
sizes(10–1000
μm)and
gasfractions
Φ,since
Φ¼
QG
QG þ
QL:
ð26Þ
Thesqueezing
regimeleads
tohighly
monodisperse
foams(PI
b2%).
Someexam
plesofobtained
foamsare
shownin
Fig.10.
2.4.2.2.Thedynam
icregim
e.Thesim
plestcasein
thedynam
icregim
eis
when
theviscous
dragwhich
isexerted
onthe
bubbleby
thefluid
over-com
esthecapillary
forcewhich
attachesthebubble
tothe
orifice
(Fig.8a).Anexam
plefrom
anexperim
entisshow
nin
Fig.11b.Thevis-
cousStokes
force,which
may
beapproxim
atedas
FV=
6πRB η
L UL ,plays
thesam
erole
asgravity
inSection
2.4.1.Equatingthe
viscousand
thecapillary
force(2πγ
RO )
leadsto
asim
pleexpression
forthe
obtainedbubble
size
RB �
γηl U
RO ¼
Ca−1
LRO:
ð27Þ
Fig.8.(a)Sum
mary
ofthedifferentforces
actingon
abubble
duringcreation.(b)
Sketchof
variationofbubble
radiusRBand
polydispersityPIw
ithgas
flowrate
QG .Corresponding
images
areshow
nin
Fig.5.(c)Stability
diagramofthe
bubblingprocess.Bubbles
detachfrom
theorifice
ifeithertheBond
number
Boorthe
Webernum
berWeGofthe
gasare
suf-ficiently
high.Inspired
from[40].
9W.D
renckhan,A.Saint-Jalm
es/A
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as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
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Hence,the
obtainedbubble
sizeisinversely
proportionaltothe
cap-illary
numberCa
L oftheliquid
anddepends
linearlyon
theorifice
radiusRO .In
thecase
ofconfinedgeom
etriesone
observesawell-defined
tran-sition
fromthe
“squeezing”(Section
2.4.2.1)to
the“dripping”
regime
when
viscousforces
startto
win
oversurface
tensionforces,i.e.above
acriticalCa
L[57,58].
Upon
increasingthe
gasorthe
liquidflow
rate,oneobserves
thatthepointofbubble
detachmentm
ovesaw
ayfrom
theorifice,leading
tothe
creationof
ajet
whose
lengthdepen
dson
theflow
velocities.Thischange
ofbehaviourmarks
anim
portanttransitionfrom
the“dripping”
(or“bubbling”)to
the“jetting”
regime[51,59,60].This
transitionisgen-
erallyrationalised
usingthe
conceptofabsoluteand
convectiveinstabil-
ities,which
wediscussed
attheend
ofSection2.3.In
thesqueezing
anddripping
regimes,the
break-upofthe
gasligamentis
causedby
anabso-
luteinstability,w
hichinvades
theentire
systemand
thereforeoccurs
al-ways
attheorifice.W
iththe
presenceofnon-negligible
viscousand/or
inertialforces,theevolution
oftheinstability
canbe
slowed
downand
hencebe
“convected”with
theflow
.Thesystem
cantherefore
createa
jetwhich
breaksat
thepointw
herethe
jetis“old
enough”so
thatthe
capillaryinstability
hadenough
timeto
develop.Twodifferentextrem
esofjetting
scenariosexist.In
thefirstcase,the
jettingisdom
inatedby
theexternalflow
(Fig.11c).Thisleads
tothe
formation
ofajetw
hichthins
away
fromthe
orificeas
theinner
fluidisbeing
accelerated,leadingto
theform
ationofbubbles
which
aresm
allerthan
theorifi
cediam
eter(since
thebubble
diameter
isof
theorder
ofthe
jetdiam
eteras
discussedin
Section2.3).In
thesecond
case,thejetting
isdom
inatedby
inertialcontributionsofthe
innerfluid,leading
toajet
ofincreasingthickness
asthe
innerfluid
isdecelerated
bythe
outerfluid
(Fig.11d),and
tobubble
sizeswhich
arelarger
than
theorifi
cediam
eter.Thiscase
was
alreadydiscussed
inSection
2.4.1.2.In
thefirstcase,researchers
havebeen
ableto
showthatthe
transi-tion
between
drippingand
jettingiswelldefined
bythe
Weou
t andRe
out
numbers
ofthe
outerfluid
[61].Thisis
show
nin
aphase
diagramin
Fig.11e(redraw
nfrom
[61]).Thetransition
dependsstrongly
onthe
densityratio
λDand
onthe
viscosityratio
λVofboth
fluids.Interestingly,one
cansee
that
Weout and
Reout are
proportionalatlow
Renum
ber,meanin
gthat
the
transitionoccurs
ata
fixed
Canum
bersince
Ca=
We/Re.This
observationwas
confirmed
bydifferentexperim
ents
andawide
rangeoffluid
couplesand
flowconditions
[51,61].Fig.11fshow
san
example
ofatypicalphase
diagramobtained
forthegeom
etryshow
nin
Fig.11a(from
[61]).What
thisphase
diagramalso
showsis
thatthe
capillarynum
berofthe
outerflow
definesthe
transitiononly
ifinertial
forcesof
theinner
fluid
canbe
neglected.In
thelim
itof
smallCa
out ,the
transitionseem
sto
bedefined
byacriticalW
ebernum
-ber
Weinofthe
innerfluid.Forinterm
ediatecases
(andifReynold
num-
bersare
sufficientlylow
)one
observesthatthe
transitionoccurs
when
Wein+
Weou
t ≈O(1)
[61].The
discussionbetw
eendripping
andjetting
may
seemsom
ewhat
academic.H
owever,it
isvery
usefulevenfor
thepractitioner.The
firstreason
isthat
asone
entersthe
jettingregim
e,monodispersity
com-
monly
drops.Thisisdue
tothe
factthatthemaxim
umofthe
curvegiv-
ingthe
unstablewavelengths
(Fig.4b)is
quitesm
ooth,meaning
thatthe
systemmay
selectawider
rangeofbubble
sizes.Moreover,w
henthe
systemisin
thejetting
state,thebubbles
donot
needto
be“nucle-
ated”with
theassociated
problemsofthe
initialentrypressure,helping
with
pressurereduction
indevices
andfor
parallelisation.Lastbut
notleast,w
ithbubble
sizesbeing
oftheorder
ofthejet
diameter
atbreak-up
(Section2.3),creating
thinjets
isan
efficientway
tocreate
alarge
number
ofsmallbubbles,dow
nto
afew
microm
etres[62,63].
Theobtained
bubblesizesdepend
onthe
operatingregim
eofthe
de-vice.Bubble
sizesin
thedripping
regimetend
tobe
welldescribed
byEq.(27).Bubble
sizesin
thejettin
gregim
edom
inatedby
theouter
fluidphase
arefound
tobe
wellcaptured
bysim
plescalings
ofthetype
RB
RO �
QG
QL
��
β;
ð28Þ
with
thepre-factor
andβdepending
onthe
flowgeom
etryand
onthe
viscosityratio
λV .Typically,β
hasbeen
foundto
liebetw
een0.4
and0.5.For
example,researchers
foundexperim
entallyand
theoreticallythatβ
=0.5
ifQG/QL→
0,andβ=
2/12
ifλV=
ηG/η
L→
0[26].For
highReynolds
andW
ebernum
bersitwas
foundthatβ
=2/5[64].
Upto
nowwehave
only
discussedperiodic
bubblingregim
es.Itneeds
tobe
saidthat
justas
inthecase
ofbubblin
gfrom
anorifi
ceinto
astation
aryliquid
(Section3.2.1)
co-flow
canlead
toperiod-
Fig.9.Selectionofthe
most
commonly
usedgeom
etriesto
generatebubbles
inconditions
where
both,thegas
andthe
liquidare
flowing.The
flowmay
eitherbe
unconfined(a–c)
orconfined
(d–g).Flowpatterns
aretypically
thatofco-flow
ofbothphases
(a,b,d–f)or
ofcross-flow(c,g).
10W.D
renckhan,A.Saint-Jalm
es/A
dvancesin
Colloidand
InterfaceScience
xxx(2015)
xxx–xxx
Pleasecite
thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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doublingand
chaoticbubbling
[65](Section
3.2.2).Suchphenom
enaoccur
oftenatthe
transitionbetw
eenregim
es.
2.4.3.Breakupofbubbles
undershear
Inthis
sectionweconsider
thebubbles
aspassive
objects,which
arealready
inthe
liquid.Weask
ourselveshow
thesecan
bebroken
intosm
allerbubbles
bythestresses
imposed
byan
activeextern
alshearflow
(Fig.1).Thisprocess
hasbeen
widely
studied.Eventhough
itis
conceptuallysim
ple,aproperphysicaldescription
turnsouttobe
highlycom
plex.How
ever,thegeneralphenom
enologyis
welldocum
ented,and
canbe
summarised.
Sincemost
oftheexperim
ental
work
hasbeen
doneon
dropsrather
thanon
bubbles,andsince
theconcepts
arevery
similar,w
eshallstay
onarather
generallevelhereby
simply
consideringtw
oim
miscible
fluidsLet
uscon
sideradrop
ofafluid
(gasor
liquid)of
viscosityηD
suspendedin
afluid
ofviscosityηCexposed
toashear
flow(Fig.12a).
Thebubble/drop
isfirst
deformed
into
anelongated,
steadysh
apewhose
geometry
dependson
thecapillary
number
Caofthe
imposed
shearflow
[66–70].Examples
ofresultingbubble
shapesare
shownin
Fig.12b(adapted
from[70]).W
ithincreasing
Caand
ηCthe
bubblesbe-
comeincreasingly
elongated—
butstill
reachasteady
equilibriumsh
ape.Note
howstrongly
suchabubble
canbe
steadilydeform
ed
without“breaking”.The
deformation
iscom
monly
measured
bythe
as-pect
ratioD=
(A−
B)/(A+
B)(Fig.12a).
Upon
furtherincrease
ofthecapillary
number,a
criticalcapillarynum
berCa*
(andhence
acriticaldeform
ationD*)
isreached
beyond
which
thebubble
canno
longersustain
asteady
shape.A
saconse-
quence,Dincreases
andeventually
reachesapoint
where
capillaryin-
stabilities(Section
2.3)break
theelongated
objectinto
pieces.Thus,theinstability
ofthe
aspectratio
isdirectly
linkedto
thebreakup
ofthe
bubble—
eventhough
theyare
notsim
ultaneous.W
hatsets
thecriticalcapillary
number
Ca*?Anim
portantpiece
ofwork
was
doneby
H.P.G
race[71]
forthe
caseofdroplets.H
eshow
edthat
Ca*depends
stronglyon
theviscosity
ratioλV ,w
hichisshow
nin
thegraph
inFig.13a
andby
correspondingph
otographsof
bubblesand
dropstaken
justbefore
Ca*isreached
inFig.13b.It
isstraightfor-
ward
tosee
theasym
metry
ofthecurve:
with
twogiven
fluids
ofdifferentviscosities,results
aredifferentdepending
onwhich
fluidisin-
sideor
outsidethe
drop.When
theinnerfluid
hasamuch
lower
viscos-ity
(asfora
bubbleinside
water,w
hereλV~10
−2),the
resultsshow
thatthe
bubblecan
supportreasonably
highCa*
≈3before
beingirrevers-
iblyextended
andruptured.
Once
theelongated
mother-bubble
(ormother-drop)
hasruptured
justaboveCa*,the
resultingsize
ofthecreated
objectsisdirectly
linked
Fig.10.Examples
ofmonodisperse
foamsgenerated
viaco-flow
ofgasand
foaming
solutionthrough
aconstriction.(a)
Examples
offoamsofdifferentbubble
sizeand
liquidfraction
ina
channeljustafterthegeneration
(from[55]).(b)
Ordered
foamswith
differentliquidfraction
(from[56]).(c)
Monodisperse
foamundergravity
(courtesyA.van
derNet)
(allbubblesizes
200–500μm
).
Fig.11.Thedripping
tojetting
transitionin
co-flowconditions.(a)
Schemeofa
commonly
usedsetup.(b)
Dripping
regime—
thebubble/drop
iscreated
atthetip
oftheorifice.(c)
Jettingregim
edom
inatedby
theexternalflow
.(d)Jetting
regimedom
inatedby
theinternalflow
.(a–dfrom
[59])(e)
Transitionbetw
eendripping
andjetting
fordifferentdensity
andviscosity
ratioswhen
thebehaviour
isdom
inatedby
theflow
oftheexternalfluid
(redrawnfrom
[61]).(f)Transition
between
drippingand
jettingwhen
atlowReynolds
number
andwhen
both,the
internalandthe
externalfloware
important
(from[59]).
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renckhan,A.Saint-Jalm
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tothe
criticalelongationD*:the
ligamentradius
atCa*provides
anesti-
mation
ofthediam
eterofthe
newly
createdentities
(seeSection
2.3).Since
boththe
criticalcapillarynum
berCa*and
theassociated
deforma-
tionD*increase
with
decreasingλVforλ
Vb1(Fig.13),this
implies
thatthe
sizeofthe
resultingobjects
decreasesfor
decreasingλV .
Theabove
descriptionscorrespond
todeform
ationsgenerated
bya
pureshear
flow.In
fact,itwas
rapidlydiscovered
thatthe
deformation
andstability
ofbubblesand
dropsin
aflow
fielddepend
stronglyon
thetype
ofimposed
flow[68,72,73].Elongational,rotationalor
simple
shearflowdoes
notdeformabubble
inthe
sameway,and
consequent-ly,the
criticalcapillarynum
berCa*
dependson
thetype
offlow.A
vastbody
oftheoreticalandnum
ericalresearchdeals
with
suchissues,con-
sideringgradually
varyingtypes
offlow,w
hichare
shownin
Fig.14a.Such
flowfields
canbe
expressedvia
thevelocity
gradient
∇u¼
12G
1þα
1−α
0−1þ
α−1−
α0
00
0
2435;
ð29Þ
where
Gfixes
theam
plitudeofflow
field.Thebalance
between
shearand
vorticityof
aflow
canthen
besim
plydescribed
bythefactor
α,
which
givespurely
extensionalflow
inthecase
ofα=
1and
simple
shear
flow
forα=
0(see
flow
patternsin
Fig.14a).Experimen
tally,such
kindof
flow
scan
begenerated
byfour
independen
tlyrotating
cylinders.The
capillarynum
berof
these
flow
sis
thentypically
expressedas
Ca¼
GηR
B
γ;
ð30Þ
where
RBisthe
radiusofthe
undeformed
bubble/drop.Asshow
nin
Fig.14b,thedependence
ofCa*on
theviscosity
ratioλV
dependsnon-negligibly
onα.In
thelim
itofbubbles(sm
allλV ),the
crit-icalcapillary
number
Ca*decreases
asone
goesfrom
α=
0(pure
shearflow
)to
α=
1(purely
extensionalflow
).For
curiosity,note
the
differenceswith
theregim
eat
highλV :
with
onlysim
pleshear
(α=
0)one
cannotbreak
veryviscous
drops,while
with
extensionalshearitispossible
(αapproaching
1).Besides
theRayleigh–Plateau
instability(Section
2.3)which
breaksthe
elongatedligam
ents,thereare
twoother
important
mechanism
swhich
canalso
leadto
thecreation
ofsmaller
bubbles/drops.Thefirst
phenomenon
iscalled
“tipstream
ing”and
isshow
nin
Fig.15.Itcreatesathin
threadwhich
startsatthe
tipofan
elongatedbubble/drop,w
hereithas
anon
-trivialshape[74].This
thread
breaksinto
tinybubbles/
drops.This
isvery
differentfrom
therupture
ofthe
main
bubble(drop)
[75].Asshow
nin
thegraph
ofFig.13a,thisphenom
enonoccurs
wellbelow
thecriticalcapillary
number
Ca*for
breakup.Thepresence
ofsurfactantsplays
anim
portantrolein
thisprocess
andnum
erousim
-portantadvances
havebeen
made
recentlyin
orderto
elucidatethe
keymechanism
satplay
inthis
process[[]].
Anotherm
odeofrupture
oftheelongated
bubble/dropwhich
occurswellbefore
theonset
ofthecapillary
instabilitytakes
placewhen
theflow
issuddenly
stopped,orifthe
bubble/dropisconvected
towards
aregion
oflow
ercapillary
number
[14,26,69].Assh
owin
Fig.16a,inthe
absenceof
deforming
stresses,thebubble/drop
tendsto
goback
toits
minim
alsurfaceshape,w
hichisasphere.In
thisprocess
ofcon-traction
,aneffect
called“en
d-pinching”can
occur:abulbous
headform
sat
eachen
dof
thefilam
ent.Thefilam
entbecom
esunstable
inthe
vicinityofthe
head,creatingtw
osm
allerheads
attherem
ainingfil-
amentand
soforth.This
canbe
nicelyseen
inthe
rightimage
sequenceofFig.16a.W
hetherend-pinching
occursdepends
onanum
berofpa-
rameters.Recently,a
phasediagram
was
proposedby
Driessen
etal.
[26](Fig.
16b),show
ing
underwhich
condition
therelaxation
ofstretched
dropsofdifferent
viscositiesin
airare
stableor
not.Itseem
sthat
asin
thecase
ofinfinitelylong
fluidcylinders
(Section2.3),one
ofthe
controlparameters
isthe
Ohnesorge
number
Oh(Table
2).Thesec-
ondcontrolparam
eteris
thedeform
ationofthe
dropat
themom
entwhen
thedeform
ingsh
earflow
isstopped.O
nceagain
,most
ofthe
Fig.12.(a)Schem
eofa
bubblebeing
deformed
inashear
flow.(b)
Photographsofthe
equilibriumshape
ofasheared
bubbleatdifferentCapillary
numbers
Caand
atdifferentviscosityratios
λV(adapted
from[70]).D
isameasure
ofthedeform
ationgiven
byD=
(A−
B)/(A+
B).
Fig.13.(a)The
“Grace
plot”:Criticalcapillarynum
berCa*
beyondwhich
thedrop/bubble
becomes
unstablein
apure
shearflowas
afunction
oftheviscosity
ratioλVofthe
dispersedand
continuousphase(adapted
from[71]).(b)Photographsofdrop/bubble
shapesatthecriticalpoint,generated
inan
extensionalflowfora
wide
rangeofviscosity
ratiosλV(adapted
from[68]).
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renckhan,A.Saint-Jalm
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esA,The
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ing,Adv
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experiments
havebeen
performed
with
drops,ratherthan
with
bub-bles,but
thephysicalph
enom
enacon
cernedhere
arevalid
forboth
systems.
2.4.4.Gas
entrainmentatfree
surfacesIfone
considersthe
flowofliquid
with
afree
surface,many
sourcesof
perturbationsof
theinterface
canlead
tothe
entrain
men
tof
the
surrounding,passiveair.This
phenomenon
isgenerally
relatedto
thepresence
ofageom
etricalcon
straintor
anabrupt
changeof
cross-section
orspeed
between
neighbouringfluid
zones[13].W
ell-known
examples
includethe
plungingjet
(Fig.17a)[80],in
which
theregion
ofgas
incorporation
opens
likea
cone,
orthe
hydraulicjum
p(Fig.17c)
(Section3.2.3),w
here
airis
entrained
when
theaverage
flow
speedof
aliquid
slowsdow
nsuddenly.Sim
ilarsituation
sarise
when
theflow
isaccelerated
temporarily
asitpasses
overobstacles
orwhen
thefree
interfacewith
airvanishes,forexample
when
flowdisap-
pearsunder
aninclined
plane(Fig.17d).
Theplunging
jetisthe
most
documented
situationin
foam-related
work
[80].Due
toits
practicalrelevance(for
example
inthe
kitchensink
andthe
bathtub),itisused
asastandardised
foamability
technique(Ross–M
ilestest,Section
3.2.3).Moreover,itcorresponds
toaprototype
(orparadigm
)experim
ent,with
which
onecan
probethe
basicmecha-
nismsat
work
inmore
complex
hydrodynamic
processes[80].O
neof
thekey
parameters
inthis
processis
theim
pactvelocity
ofthejet
U,
i.e.itscapillary
number
Ca=
ηL U
/γ.Below
athreshold
value,asteady
deformation
oftheinterface
isobtained
without
theincorporation
of
gas(insetofFig.18).A
nim
portantfeatureisthatthe
radiusofcurvature
ratthe
edgeofthe
gas“cusp”
vanishesexponentially
with
thecapillary
numberCa,i.e.r~
exp(−Ca)
[80].Thissteady
interfacialdeformation
be-com
esunstablebeyond
acriticalcapillary
numberCa
c (andan
associatedcriticalcusp
radiusrc ):a
viscouspum
pingofthe
entrainedfluid
intothe
narrowing
nosegenerates
alubrication
pressure,which
finallyprevents
anysteady
forcebalance
[80].Asin
thecase
ofbubblebreak-up
undershear,above
thisCa
c thecusp
isincreasingly
stretcheduntiliteventually
breaksinto
smaller
bubblesby
themechanism
sdiscussed
inSection
2.3.The
entireprocess
issketched
inFig.1.It
canproduce
quitemonodis-
persefoam
swith
bubble-sizesand
monodispersity
dependingon
thejet
speed—
asthe
regularbath
tuberor
dishwasher
may
confirm.
Thephysics
ofplungingjets
hasbeen
investigatedin
detailforhigh-
viscosityliquidsin
air,asbothexperim
entsand
modelisation
turnoutto
beeasier
toperform
thanfor
low-viscosity
fluids.Different
investiga-tion
slead
totheprediction
that,as
longas
inertia
canbe
neglected(sm
allRe),thecriticalcapillary
number
Cac scales
logarithmically
with
theviscosity
ratioλV[80,81]
Cac �
−ln
ηG
ηL
��
¼ln
λV
ðÞ:
ð31Þ
Thisis
shownin
Fig.18(adapted
from[80]).Lorenceau
etal.[81]
haveshow
nthat
thisrelationship
canbe
extendedover
fiveorders
ofmagnitude
tosm
allerviscosity
ratioswhen
working
with
twoliquids.
Fig.14.(a)Differenttypesofflow
fieldsinwhich
thebubbles/dropsare
deformed,ranging
frompurely
extensional(α=
1)to
pureshearflow
(α=
1)(adaptedfrom
[68]).(b)Effectofthe
flowtype
onthe
criticalcapillarynum
berCa*
beyondwhich
thebubble/drop
shapebecom
esunstable
(adaptedfrom
[68]).
Fig.15.Tip-streaming:production
oftinybubbles
atthetip
ofbubblessheared
inaCouette
cell(aand
bfrom
[79])and
atthetip
ofadrop
(cfrom
[24]—Leonhard,H
.,1996,“Experiments
ontipstream
ing,”unpublished).
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renckhan,A.Saint-Jalm
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Anothernon-trivialresultconcerns
therate
ofgasentrained.Itturns
outthat
itdepends
onlyon
thegas
viscosity,and,surprisingly,noton
thefluid
viscosity[80].This
isdue
tothe
factthatthegas
filmdecouples
thejet
fromthe
restofthefluid.
Incontrast
tothe
previouslydescribed
visco-capillaryentrainm
entmodes,
thephysics
oflow
-viscosityplunging
jetsis
commonly
characterisedby
highReynolds
numbers
(ReN100)
andlow
capillarynum
bers(Ca
b1).U
ndersuch
conditions,differentinertialinstabilities
ofthegas/liquid
interface
candevelop
alreadybefore
theim
pact,sothatthe
cross-sectionofthe
jetisno
longerconstant.One
oftheseinsta-
bilitiesisthe
Kelvin–H
elmholtz
instability[82].It
ariseswhen
twoim
-miscible
fluids
with
differentdensities
flow
sideby
sideat
verydifferent
velocities(Fig.19a).Beyond
acriticalvelocity
differencecer-
tainwave
lengthsofnaturalinterfacialfl
uctuationsbecom
eunstable
andare
amplified
bythe
flow[82].A
nexam
pleofthis
instabilityon
asim
plewater
jetin
airisvisible
onthe
leftside
ofthejet
inFig.19b.If
thisinstability
developsbefore
theviscous
pumping
effectstarts
tobe
important
theymodify
inanon-trivialm
annerthe
entrainment
andbreak-up
mechanism
.Differentscenarios
arisewhich
areoften
studiedin
separateregim
esdepending
ontheinitialam
ountof
disturbancerelative
tothe
speedofthe
jet[80].
TheKelvin–H
elmholtz
instability
canlead
toanother
typeof
airentrainm
entwhen
itisdriven
tosufficiently
highW
ebernum
bersWe
(i.e.bothRe
andCa
needto
behigh
sinceWe=
ReCa).Inthis
casethe
destabilisationofthe
interfaceisgreatly
amplified,leading
tocom
plexflow
structureswhich
tendto
leadto
theform
ationofsm
allerligaments
which
thenagain
undergothe
typeofcapillary
instabilitiesdiscussed
inSection
2.3.This
kindof
fluid
break-upis
called“atom
isation”or
“fragmentation”
(rightside
ofthejet
inFig.19b
andwave
breakingin
Fig.19c)[30,83–86].U
nderthe
rightflowconditions,it
canlead
tothe
entrainment
ofasignificant
amount
ofairand
henceto
foamgenera-
tion,as
shown
bythe
example
ofbreaking
waves
inFig.
19cand
discussedbriefly
inSection
3.2.3.Gas
entrain
men
tdoes
not
necessarily
require
high
velocityflow
:trappingpockets
ofgasin
afluid
canoccu
rat
lowflow
veloc-ities
inth
epresen
ceof
confined
geometries
andwhen
flow
condi-
tionsvary
fasten
ough
soth
atth
efree
interface
getslocally
suffi
ciently
deform
edto
entrain
agas
pocket.
Wash
ing
your
han
dswith
soapis
probably
enou
ghof
anexp
erimen
tto
convin
ceyou
rselfof
this
effect.High
lyviscou
sfluidsmay
alsosim
ply
befold
edin
away
totrap
air.
2.5.Bubblegeneration
without
topologicalchanges—
phasetransitions
One
ofthemain
techniquesto
obtainbubbles
withoutthe
necessityof
atopological
transitionof
theinterfaces
istheir
generationvia
a
liquid→
gasphase
transitionwhich
occurslocally
inthe
fluidto
createbubbles.There
aretw
odifferent
classesofphase
transitionswhich
arecom
monly
usedfor
bubblegeneration
[88–90].Thefirst
classoccurs
inpure
fluids,where
theliquid
phaseturns
intovapour.A
sindicated
inthephase
diagramof
Fig.20a,
this
caneither
betriggered
bya
pressuredrop
(“cavitation”)or
bya
temperature
rise(“boiling”).
Cavitationis
commonly
createdby
rapidflow
swhich
createlocalised
pressuredrops
throughconstrictions
orrotating
propellersor
byhigh
energy
pressurewaves,such
asen
counteredin
ultrasound.
Bubbleand
foamgeneration
byboiling
isknow
nto
most
ofusfor
thecase
ofwater
ormilk
inthe
kitchen.The
secondclass
ofliquid→
gastransitions
occursin
supersaturatedliquids
with
inwhich
agas
isdissolved
which
comes
outof
solutionupon
apressure
drop(Fig.20b)
oratem
peratureincrease.By
farthe
mostcom
monly
usedmechanism
inthe
caseoffoam
generationisthe
oneencountered
uponapressure
drop,which
iscalled
“effervescence”and
which
isparticularly
wellknow
nto
loversoffizzy
drinks,beeror
champagne.
Thesedifferentw
aysofgenerating
bubblesin
anoriginally
homoge-
nousfluid
haveacom
mon
physicalmechanism
:thesystem
needsto
bedriven
intoasupercriticalstate,in
which
smallbubbles
nucleatespon-
taneouslyand
thengrow
(Fig.2).Understanding
thenucleation
ofbub-bles
inaliquid
hasalong-standing
history[88–91],w
ithanum
berof
openquestion
sthat
remain
tobe
answered.The
complexity
ofthis
Fig.16.(a)Abubble
breaksasitrelaxesfroman
elongatedshape
when
theapplied
shearisstopped(from
[68]).Theway
itrupturesdependsonitsinitialaspectratio
andthe
viscosityratio
ofthetw
ofluids.This
isshow
nin
aphase
diagramin
(b)which
showsastable
andan
unstablezone
fordeform
eddroplets
ofdifferentviscosities
inair
usingthe
aspectratio
andthe
Ohnesorge
number
Ohas
keyparam
eter(from
[26]).Here
thefullcircles
correspondto
dropletswhich
contractwithout
breaking.Theem
ptycircles
areobtained
formore
stretchedand
viscousdrop,w
hichfinally
breakas
theyrelax.
Fig.17.Differentconfigurations
leadingto
gasentrainm
entatfreesurfaces.
Adapted
from[13].
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renckhan,A.Saint-Jalm
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esA,The
scienceoffoam
ing,Adv
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subjectresultsfrom
thefactthat
bubblenucleation
needsto
startwith
thecreation
ofasingularity
within
thefluid,w
hichcalls
uponamolec-
ulardescription
oftheprocess
(challengefor
theory)and
which
isex-
tremely
sensitiveto
thepresence
ofim
purities(challen
gefor
experiments).
Ifoneneglects
thevery
initialstageofthe
holeopening,one
may
as-sum
ethatthe
createdbubble
islarge
enoughso
thatonecan
applythe
conceptofa
surfacetension
andabulk
descriptionofthe
gasand
theliquid
phase.Inthis
caseone
canconsider
thetw
okey
contributions
tothe
freeenergy
ofthebubble
formation.O
nthe
onehand,once
thesystem
isin
asupercriticalstate,it
willreduce
itsfree
energyby
thephase
transitionwith
anassociated
changein
thefree
energydensity
ΔGV
ΔGbulk ¼
−VB Δ
GV ¼
−43πR3B Δ
GV:
ð32Þ
Atthe
sametim
e,thecreation
ofabubble
requiresthe
creationofa
vapour/liquidor
gas/liquidinterface,w
hichleads
toan
increasein
freeenergy
ΔGsurf ¼
AB Δ
GS ¼
4πR2B γ
:ð33Þ
Hence,the
totalchangein
freeenergy
may
beapproxim
atedby
ΔGtot ¼
ΔGsurf þ
ΔGbulk ¼
πR2B γ
−43πR3B Δ
GV:
ð34Þ
Makin
gth
eapproxim
ationthat
thesurface
tension
andthevol-
umefree
energy
areindep
enden
tof
thebu
bblesize,on
eobtain
sa
freeen
ergyfunction
which
ischaracterised
byawell-defi
ned
maxi-
mum
,assketch
edin
Fig.21.Thismaxim
umsets
acriticaln
ucleationbarrier
ΔGCwhich
isassociated
with
acriticalbu
bblerad
iusRc .A
spontan
eouslygen
eratedbubble
which
issm
allerth
anth
iscritical
sizewillsh
rinkan
ddisappear,w
hile
abubble
which
isbigger
than
this
criticalsizewillgrow
.Thenucleation
ratenof
bubblesmay
beapproxim
atedby
n�exp
−ΔGC
kT
��:
ð35Þ
Thegrow
thrate
ofthesebubbles
dependson
thesaturation
condi-tions
andcan
beapproxim
ated[88–92]—
butthis
isbeyond
thescope
ofthearticle.
Amore
mechanicalw
ayto
approximate
thecriticalradius
directlyis
touse
theLaplace
law
RC ¼
2γΔP ¼
2γσPf
ð36Þ
where
σisthe
“supersaturation”ofthe
liquid(σ
=α−
1,with
αbeing
the“saturation”)
andPf is
thefinalpressure.The
definitionofthis
super-saturation
dependson
theconsidered
scenarioand
canbe
obtainedfrom
thephysicalparam
etersofthe
system.In
thepresence
ofonephase
only(cavitation
andboiling,index
“1Ph”)one
needsto
takeinto
accountthe
vapourpressure
PVofthe
liquid.One
may
thereforedefine
ΔP¼
PV −
Pf ¼
σ1Ph P
fð37Þ
σ1Ph ¼
α−1¼
PV
Pf −
1:
ð38Þ
Inthe
caseoftw
ophases
(index“2Ph”),i.e.a
liquidbeing
supersat-urated
byadissolved
gas(effervescence),one
needsto
takeinto
ac-count
thevapour
pressureof
thesolven
tand
thepartialpressure
ofthe
dissolvedgas.The
latterbeing
generallymuch
higher,onecan
ne-glectthe
vapourpressureand
expressthe
supersaturationusing
Henry's
law
ΔP¼
Pi −
Pf ¼
HXi −
Xf
ðÞ¼
σPi
ð39Þ
σ2Ph ¼
α−1¼
Xi
Xf −
1ð40Þ
where
H=
Pf /X
f isHenry's
constantandXi and
Xf are
themole
fractionsofthe
dissolvedgas
inthe
initialandfinalstate,respectively.
Due
tothe
nucleationbarrierΔ
GC ,one
generallyfinds
thatsupersat-urations
ofafew
1000are
requiredin
verypure
liquids.Thereason
why
wesee
nucleationand
growth
atmuch
lowersupersaturationsin
every-day
lifeis
dueto
thepresence
ofim
puritiesor
pre-formed
bubbleswhich
actas
nucleationsites
(Fig.22)and
which
may
dramatically
de-crease
thenucleation
barrier.Assketched
inFig.22
(inspiredby
[90]),scientists
groupthe
differentnucleation
scenariosin
twomain
groupsof
nucleation.“H
omogen
eousnucleation
”(Typ
eI)
occurswith
outthe
presenceofany
nucleationagents
andtherefore
atveryhigh
super-saturations.“H
eterogeneousnucleation”
occursin
thepresence
ofnu-cleation
agents.Inthis
caseone
differentiatesbetw
eenthree
types,follow
ingthe
kindof
agentspresent
andthe
specific
physicalconditions
[90]:
Fig.18.Criticalcapillarynum
berCac asa
functionofthe
viscosityratio
λVbeyond
which
airisentrained
byan
impacting
liquidjet.Inset:sketch
oftheinitialentrainm
entsteps.
Adapted
from[80].
Fig.19.(a)Destabilisation
ofagas/liquid
interfacedue
tothe
Kelvin–H
elmholtz
instability.(b)
Kelvin–H
elmholtz
instabilityon
aliquid
jet.Thegrow
thofthe
instabilityatsufficiently
highWeleads
tothe
formation
ofcomplex
patternswhich
canlead
tothe
creationofsm
alldrops
(atomisation,from
)or
theentrainm
entofairbubbles,as
shownby
breakingwaves
in(c)
(from[87]).
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renckhan,A.Saint-Jalm
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Heterogen
eousnucleation
—Type
II(classical):Nucleation
occursin
thepresence
ofsolidim
puritieswhich
caneither
besm
allparti-cles
dispersedin
theliquid
orthesolid
wallofthe
container.Reason-ably
highsupersaturation
sof
order100
arerequired
forbubble
generationin
thiscase.
Heterogen
eousnucleation
—Type
III(classical):Nucleation
occursin
thepresence
ofpre-existinggas
cavities(on
thecontainersurface,
onsuspended
particlesor
freelyfloating
inthe
liquid)ofradius
ofcurvature
smaller
thanthe
criticalradiusRC .H
enceone
stillneedsto
nucleate,butsupersaturations
aresignificantly
lower
thanin
thecase
oftypeIand
IInucleationsince
the“holes”
inthe
liquidare
al-ready
made.
Heterogen
eousnucleation
—Type
IV(non-classical):Bubbles
aregenerated
frompre-existing
gascavities
(onthe
containersurface,
onsuspended
particlesor
freelyfloating
inthe
liquid)ofradius
ofcurvature
largerthan
thecriticalradius
RC .Since
thereisno
energybarrier
toovercom
eitis
referredto
as“non-classical”
nucleation.These
cavitiesgrow
assoon
asasm
all[93]levelofsupersaturationisreached.Type
IVnucleation
may
followtype
IIInucleation,forex-
ample
ifbubblesnucleate
incavities
onthe
wallleaving
behinda
bubblelarge
thanthe
criticalradius.
Inthe
caseofheterogeneous
nucleation,thebubble
generationata
walloratan
impurity
becomes
onewhich
requiresatopologicalchange
todetach
thebubble
fromthe
nucleatingagent.This
providesthe
same
conditionsasdiscussed
inSection
2.4.1with
thedifference
thatthebub-
bleisblow
nby
aphase
transition.
3.Techniqu
esof
foamform
ation
3.1.Introduction
Inthis
sectionwediscuss
someofthe
mostcom
monly
usedfoam
ingtechniques.These
techniquesmake
useof
thefundam
entalmecha-
nismsofbubble
generationdiscussed
inSection
2.How
ever,tothe
de-spair
ofthose
who
want
tomodel
theirbeh
aviour,they
commonly
combine
differentmechanism
s.Moreover,they
arecom
monly
runin
away
thatthegeneration
ofonebubble
cannotbeconsidered
asisolated
fromthegeneration
ofthe
others(as
wedid
throughout
most
ofSection
2).Hen
ce,eventhough
themain
mechanism
sof
most
tech-niques
may
beiden
tified,predicting
theproperties
oftheobtain
edfoam
asafunction
ofthe
differentdevice
parameters
isnot
simply
a
questionofextrapolating
ourdiscussion
fromthe
previoussection
andtherefore
remains
amajorchallenge.M
oreover,onlyfew
ofthecom
plexfoam
ingtechniques
havebeen
investigatedsystem
aticallyin
thepast.
Itisforthis
reasonthatthe
descriptionofthe
differentfoaming
tech-niques
remains
hereon
asom
ewhat
qualitativelevel.W
ehave
triedto
groupthe
differenttechniquesby
theirmain
mechanism
s,goingevery
timefrom
thesim
plestconfiguration—
where
someofthe
actingphys-
icsisunderstood
—to
themostcom
plexone.In
ordertoguide
theread-
erwho
may
consultthis
articlein
the
searchfor
anappropriate
techniquefor
hisapplication,w
ehave
compiled
someofthe
keyfea-
turesofcom
monly
usedtechniques
inTable
3.
3.2.Mechanicalfoam
ingtechniques
3.2.1.Foaming
bybubbling
intoastationary
liquidThe
processof
bubblinginto
astationary
liquidis
ofgreatim
por-tance
inanum
berofindustrialprocesses,the
most
common
examples
beingbubble
columnreactors
[94,95]or
foamflotation/fractionation
tanks[96,97].In
most
applications,bubblingoccurs
throughmany
ori-fices
inparallel,th
roughaperforated
plate(regular
distributionof
equal-sizedholes)
orthrough
aporous
disc(irregular
arrangement
oforifi
cesof
irregularcross-section,but
typicallywith
ach
aracteristicsize).Researchers
findthat
eventhough
—in
principle—
thebubbling
processon
eachindividualorifice
canbe
describedas
inthe
caseofan
Fig.20.Differentpossibilities
tonucleate
bubblesin
asolution.(a)
Liquid→
gastransition
ofonephase
viapressure
drop(“cavitation”)
oratem
peraturerise
(“boiling”).(b)Liquid
→gas
transitionupon
changeofsolubility
ofagas
dissolvedin
aliquid,here
byapressure
drop(effervescence).
Fig.21.Changeoffree
energyduring
bubblegeneration
fromasupercriticalliquid.
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renckhan,A.Saint-Jalm
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ing,Adv
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isolatedorifice
inSection
2.4.1,anum
berofcom
plexinteractions
occurbetw
eenthe
closelyspaced
orificeson
theplate
orthe
discwhich
needto
betaken
intoaccount
[33,94].Theseinteractions
may
arisefrom
acoupling
throughthe
reservoiror
throughthe
liquidby
hydrodynamic
flowsor
directbubblecontact.In
anattem
pttoelucidate
thesecom
plexinteractions,researchers
havestarted
tolook
atmore
simplified
systems
ofafew
orificesofcontrolled
spacingand
dimensions
(Section3.2.1.2).
Characteristic
bubblesizes
with
these
kinds
oftechniques
rangefrom
afew
hundredmicrom
etresto
onecentim
etre.Thefoam
canbe
verymonodisperse,ifidenticalorifices
aredriven
undertherightcondi-
tions(Section
3.2.1.2),orpolydisperse,w
ithpolydispersities
beingtyp-
icallyup
to50%
.Foam
productionrates
dependon
thenum
berof
orifices
used.With
porousdiscs
onecan
easilygenerate
1L/m
in/cm2
ofporesurface.Since
thebubbles
needto
begenerated
inaliquid,the
foamjust
aftergeneration
hasgenerally
ahigh
liquidfraction.A
sbub-
blesrise
away
fromthe
generationsite
theliquid
isdrained
bygravity
tocreate
foamswith
lowliquid
fractions.
3.2.1.1.Complex
bubblingregim
esfor
oneorifice.In
Section2.4.1
wecon-
sideredperiodic
bubblingregim
esonly.H
owever,even
asingle
orificecan
bedriven
inhighly
non-linearbubbling
modes,depending
onthe
bubblingconditions.A
sshow
nin
Fig.23aand
bat
intermediate
gasflow
ratesthe
bubblingperiods
T(tim
ebetw
eentw
obubble
detach-ments)
bifurcate,leadingto
twoor
more
bubblingperiods.In
certainranges
afully
chaoticbubbling
isobserved
with
arandom
distributionofthe
bubblingperiods
[93,98–102].Multiple
bubblingperiods
canlead
tobubble
sizedistributions
with
severalpeaks(bi-
ortri-disperse,etc.)
while
chaoticbubbling
may
generatepolydisperse
foams.W
hichone
ofthe
differentregimes
isselected,depends
stronglyon
theliquid
proper-ties,the
orificeconditions
andthe
gasflowrate.A
ttheoutset,researchers
believedthatthis
complex
behaviourresulted
fromintricate
interactionsbetw
eenthe
detachedbubble(s)and
theone
which
isbeing
generated,orfrom
pressurefluctuations
inthe
reservoir.Theinterpretation
which
seemsto
beem
ergingnow
isthatitis
ratherthe
dynamics
ofthegas/liq-
uidmeniscus
within
andatthe
orificewhich
controlsthis
interestingbe-
haviour[93,100–102].Forexam
ple,Fig.23bshow
sthatthe
complexity
islostas
soonas
theorifice
radiusro
islarge
enough.
3.2.1.2.Bubblingfrom
severalorifices/perforatedplates.If
onebubbles
throughseveralorifices
inparallel,the
resultingbehaviour
dependson
whetherthe
bubblesareblow
nfrom
thesam
egasreservoir.A
ttheoutset
letus
considertw
oorifices
which
arefed
byaseparate
gasinjection.A
slong
asthey
aresufficiently
faraw
ayfrom
eachother
within
thefluid,
Table3
Overview
ofthekey
featuresofsom
eofthe
mostcom
monly
usedfoam
ingtechniques.
PrincipleTechnique
Bubblesize
(mm)
Polydispersity(%)
Initialgasfraction
φProduction
rate(L/m
in)Section
Bubblinginto
astationary
liquid(active
gasphase,passive
fluid
phase)Individualorifice
0.1–102–40
b0.60
b1
2.4.1and
3.2.1.1Many
orifices/perforatedplate
0.1–102–40
b0.60
b5(per
cm2)
3.2.1.2Porous
disc0.1–10
10–50b0.70
b5(per
cm2)
3.2.1.3Co-flow
oofgas
andliquid
(activegas
phase,activefluid
phase)Individualorifice
0.01–12–30
b0.99
b0.1
2.4.2and
3.2.2.1Porous
media
0.01–1N30
b0.90
b1
3.2.2.2Static
mixer
0.01–1N30
b0.95
b15
3.2.2.3Straight
tube0.01–1
N30
b0.97
b10
3.2.2.4Airentrainm
entandbreak-up
undershear
(passivegas
phase,activefluid
phase)Ross–M
iles(plunging
jet)0.1–5
10–40b0.60
b1
3.2.3.2Venturihose
0.01–0.1b30
b0.90
b5
3.2.3.2Propeller
N1
b30
b0.97
b1000
3.2.3.2Kitchen
blender0.01–1
b40
b0.97
b1
3.2.3.3Rotor–stator-m
ixer0.01–0.1
b30
b0.90
b10
3.2.3.3Foam
ingby
shaking0.1–10
b70
b0.80
Depends
3.2.3.4Phase
transitionNucleation
0.001–0.0110–40
b0.60
b1
3.3.1Aerosolcans
N0.01
N30
b0.99
b1
3.3.2Cavitation
≈0.001
N20
b0.60
b0.001
3.3.2Electro-chem
icalElectrolytic
cell0.001–0.01
10–30b0.60
b0.001
(percm
2)3.3.3
Fig.22.Differenttypes
ofnucleationand
growth
processesencountered
inbubble
formation
(inspiredfrom
[90]).
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renckhan,A.Saint-Jalm
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bothorifices
functionindependently
following
thebehaviour
discussedin
Section2.4.1.H
owever,below
acriticalspacing
(which
dependsonpa-
rameters
likethe
bubblingvelocity),both
orificesbegin
tocom
municate
viahydrodynam
icinteractions
[103,104]throughthe
liquid.Theresultis
thatbothorifices
cansynchronise
suchthatthe
bubblesare
generatedin
analternating
fashionas
isshow
nin
Fig.24awith
correspondingflow
fieldsin
Fig.24b(from
[103]).Thissynchronisation
issensitive
tothe
bubblingspeed
andisgenerally
lostat
verylow
bubblingvelocity
andatvery
highbubbling
speed,when
theorifice
isin
thejetting
mode.
Iftheorifices
arefed
fromthe
samereservoir,as
isthe
casefor
per-forated
plates(Fig.24c–e),on
eadds
anim
portantcouplin
gthrough
fluctuationsin
thepressure
andflow
fieldofthe
gaswithin
thereser-
voir.Letus
imagine
thatat
thebeginning
allorificesare
closed.Asthe
pressureincreases
inthe
reservoir,thegas/liquid
interfacesat
theori-
fices
startto
curveoutw
ardsuntilthe
maxim
umpressure
isreached
when
theinterface
isahem
isphere(Fig.6b).Beyond
thispoint,the
bub-ble
growsatincreasing
speed(since
theresisting
Laplacepressure
oftheinterface
decreaseswith
increasingbubble
volume).The
resultingrapid
inflowinto
thebubble
thereforeleads
toapressure
dropofa
certainex-
tensionin
theunderlying
reservoir.Thispressure
dropcan
beso
strongand
long-range,thatacertain
number
oforificesaround
theone
where
thebubble
isgenerated
willnotbe
ableto
reachthe
maxim
umpressure
forbubble
formation.The
resultisthatatlow
flowrates
onperforated
platesonly
acertain
number
ofholesare
activein
thebubbling
process.Atypicalexam
pleisshow
nin
Fig.24d.Thecharacteristic
distancebe-
tween
theactive
holesdepends
onthe
influencelength
within
theres-
ervoir,which
inturn
dependson
theflow
rate.Which
holesare
activedepends
onwhich
onemanages
tofire
first,which
generallydepends
onsm
allfluctuationsin
thehole
size,with
largerholes
firing
first.As
theflow
rateisincreased,m
oreand
more
holesstart
tobe
involvedin
thebubbling
process.Fig.24esh
owsan
example
oftheactive
hole
fractionas
afunction
oftheinjected
gasvelocity
(from[105]).This
in-crease
isdue
totw
oreasons.The
increasein
gasflow
velocityleads
toan
increasingdynam
icpressure
dropat
eachhole
[106]. Once
thedy-
namicpressure
dropisofthe
orderofthe
maxim
umcapillary
pressure,allholes
shouldbe
ableto
generatedbubbles.A
secondreason
isthatfor
sufficientlyhigh
gasflow
velocities,i.e.beyondacharacteristic
Weber
number(see
Section2.4.1.2),inertialforces
playan
importantrole
lead-ing
tothe
formation
ofagas
jet.Thisim
pliesthatthe
holesrem
ainopen
permanen
tlyand
themaxim
umcapillary
pressureloses
itsmeaning
oncethe
holeisfiring.This
canbe
seenin
Fig.24e,where
allholesare
activewhen
theflow
velocityis
about12
m/s
which
correspondsto
We≈
2and
thereforeto
thejetting
regime(Section
2.4.1.2).Sincethe
jetshave
acertain
cross-section,thefinal
number
ofactive
orifices
may
besm
allerthan
100%ifthe
orificespacing
issm
allerthan
atypical
jetdiameter
[107].Thebubble
sizeateach
orificecan
beapproxim
atedusing
thegas
flowrate
peractive
orificeand
therelations
providedin
Section2.4.1.H
owever,one
needsto
keepin
mind
thatthe
couplingcan
leadto
flowrate
fluctuationsbetw
eenthe
orificesand
thereforeto
thegeneration
ofbubblesofdifferentsizes.
Formany
purposesitis
desirableto
drivethe
porousplate
inaslow
bubblingmode
tomaintain
themonodispersity
ofthebubbles.A
nele-
ganttrick
toavoid
thepressure-coupling
oftheorifi
cesis
toincrease
theflow
resistance
between
them
inthereservoir.This
canbe
doneby
increasingthe
flowresistance
ofeachorifice
(longslender
orifices)or
byreplacing
thepart
ofthereservoir
underneath
theorifi
cesby
afine
porousmedium
[106].Apartfrom
thequestion
ofthenum
berofac-tive
orifices,couplingofthe
bubblebreak-up
canoccur
forsufficiently
closeorifices.Researchers
find[108–110]thatbubbling
issynchronised
atlow
andahigh
flowrates
(jettingregim
e),while
itisasynchronous
forinterm
ediateflow
rates.Thesynchronisation
dependson
theorifice
spacingand
organisation.
Fig.23.Perioddoubling
andchaotic
bubblingbehaviourupon
gasinjection
intoastationary
liquid(a,b)
andin
co-flowconditions(c).(a)
Left:Bubblingperiods
Tas
afunction
ofreservoirpressure.Right:Corresponding
images
forperiod-1,-2and
-4behaviour(adapted
from[99]).(b)
Bubblingperiods
asafunction
ofgasflow
rateQGfortw
odifferentorifice
sizes.Thecom
-plexity
disappearsfor
thelarger
orifice(adapted
from[102]).(c)
A:Bubbling
devicefor
thecreation
ofco-flowconditions.B:Bifurcation
diagramshow
ingthe
bubblediam
eterdbas
afunction
oftheliquid
flowrate
Q(atconstant
gaspressure)
andcorresponding
photographsofthe
bubblingprocess
(adaptedfrom
[65]).
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renckhan,A.Saint-Jalm
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3.2.1.3.Spargingfrom
porousdiscsandmore
exoticspargergeom
etries.Themost
commonly
usedspargers
forfoam
generationare
probablyofpo-
roustype,as
shownin
Fig.24f.Themost
popularspargers
aresintered
glassdiscs,sincethey
arehydrophilic,easy
toclean
andsince
theyprovide
awide
rangeand
agood
controloverthe
characteristicpore
dimensions.
Inporous
spargers,allofthepreviously
discussedmechanism
sinteract
simultaneously
togive
thefinalfoam
properties.Thefinalbubble
sizedistribution
dependssensitively
onthe
pore-sizedistribution,the
wetting
propertiesand
theflow
conditions.Thereare
twoim
portantdifferencesbetw
eenporous
spargersand
perforatedplates.The
firstliesin
thewide
distributionofpore
sizes(asshownin
Fig.24f).Sincethe
initialmaxim
umcapillary
pressureto
beovercom
eisinversely
proportionaltopore
radius(Eq.(17))the
bubblingwilloccurthrough
thelargestpores.Thisisw
hyat
lowflow
rates,porousdiscs
canproduce
foamsofhigh
monodispersity
(Figure24g
from[111]).W
ithincreasing
gasflow
rate,thepressures
atthe
smaller
holesincrease
sothatan
increasingnum
berofsm
allerpores
areactive,m
akingthe
foamincreasingly
polydisperse.Asin
thecase
ofasingle
orifice,asarule
ofthumb,the
averagebubble
sizeofa
spargerisproportionalto
itsaverage
poresize.The
seconddifference
liesin
thefactthatthe
differentporesofa
spargerareless
coupledby
pressurefluc-
tuationsthan
theorifices
ofaperforated
plate,sincethe
gasencounters
ahigh
flowresistance
asitpassesthroughthe
complex
porenetw
ork.How
-ever,this
simplification
regainscom
plexityby
thefactthatdepending
onthe
dynamicconditions
thegas
may
choosedifferentpreferred
passagesthrough
theporous
material.D
ependingon
theflow
conditions,bubblesize
distributionsfrom
porousspargers
havebeen
characterisedby
thepresence
ofseveralpeaks[112]orbyasm
oothW
eibulldistribution[113].
Thegas
fractionofthe
foamgenerated
justabovethe
spargertends
tobe
verylow
,thefinalgas
fractionofthe
foambeing
createdby
acom
-petition
between
foamrise
andliquid
drainage[114].Care
needsto
be
takenwhen
thegas
influxisso
highthat
afoam
iscreated
rightat
theoutlet
ofthesparger.In
thiscase,bubble
generationmechanism
smay
changedram
atically,leadingto
adependence
ofthebubble
sizewith
flow
ratewhich
may
becom
pletelydifferent
(eventheinverse)
towhat
hasbeen
discussedabove.
Aselection
ofmore
exoticspargers
hasbeen
developedin
thepast,
generallywith
theaim
toobtain
abetter
controloverthe
bubblesize
distributionwhile
increasingthe
foamproduction
rate.Amon
gstthe
most
elegantare
techniqueswhich
employ
theinstability
ofgas/liquidinterfaces
inparticulargeom
etricconditions.Exam
plesinclude
periodicbubble
generationat
anarrow
gap[116,117]
orat
astep
[118,160],which
canproduce
highlymonodisperse
bubbles,asshow
nin
Fig.25.Sim
ilarto
thecase
oforificebubbling,the
bubblesizes
may
bevaried
viathe
gap/stepwidth
andthe
gasflow
rate.
3.2.2.Foaming
viaco-injection
ofgasand
liquidAsalready
discussedin
Sec tion2.4.2,the
bubblingtechniques
oftheprevious
sectionare
oftenim
provedby
imposing
aflow
ofthefoam
ingsolution.This
helpsin
carryingthe
bubblesaw
ayfrom
thebubbling
siteand
insetting
upadditionalstresses
which
provideim
provedcontrol
overthe
bubblesizes
andthe
obtainedgas
fraction.Individualco-flowdevices
areoften
parallelisedto
increase
theproduction
rates(Section
3.2.2.1).One
common
approachof
parallelisingthe
co-flowmechanism
isto
letgas
andfoam
ingsolution
flow
through
complex
poregeom
etries.Inthis
case,bothphases
travelthroughan
intercon-nected
network
ofrandomor
purpose-shapedpores
(Sections3.2.2.2
and3.2.2.3),being
exposedto
arange
ofdifferentmechanism
swhich
turnone
largegas
pocketsinto
many
smallbubbles.O
neofthe
keydif-
ferencesbetw
eenco-fl
owin
individual
pores(as
discussedin
Section2.4.2)
andco-flow
inmore
complex
pore-networks,is
thatthe
Fig.24.Bubblingwith
increasingcom
plexity.(a)Synchronisation
ofbubblingfrom
neighbouringorifices
viainteraction
throughthe
liquid(from
[103]).(b)Sim
ulationofthe
flow-field
aroundgenerated
bubblesat
twoorifices
fortw
odifferentorifice
spacing(from
[103]).(c)Exam
pleofbubble
generationon
aperforated
plate(adapted
from[115]).(d)
Bubblingata
perforatedTeflon
plateshow
ingthat
bubblingoccurs
onlyvia
alim
itednum
berofholes
[106].(e)Variation
ofactivehole
fractionat
which
bubblesare
generatedwith
gasflow
ratefor
differentliquidheights
(from[105]).(f–g)
Image
ofaporous
discand
ofbubblesgenerated
fromitfor
increasinggas
flowrate
(from[111]).
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renckhan,A.Saint-Jalm
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ing,Adv
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systemcan
choosebetw
eenmany
differentflowpaths,adding
yetan-
otherlevelofcom
plexity.Different
typesofpore
geometries
andflow
conditionscan
beused
forefficient
foamgeneration.W
ediscuss
some
ofthemhere.
3.2.2.1.Complex
bubblegeneration
andparallelisation
ofco-flowdevices.
Asin
thecase
ofbubblin
gfrom
anorifi
ceinto
astation
aryliquid
(Section3.2.1.1),even
individualco-flowdevicesm
ayexhibita
complex
behaviourat
intermediate
bubblingregim
es.Anexam
pleis
shownin
Fig.23cforthe
co-flowthrough
aconstriction,w
hichshow
speriod
dou-bling
andchaotic
bubblingfor
certainranges
ofliquidflow
ratesatcon-
stantgas
pressure[65].
Evenifco-fl
owdevices
cangenerate
upto
106bubbles/m
in,this
tendsto
correspondto
smallfoam
productionrates
sincebubble
sizesare
small.Efforts
havetherefore
beenmade
toparallelise
theindividual
devices[62,119].In
thesqueezing
ordripping
regime(Section
2.4.2)com
plexcoupling
isobserved
between
the
differentorifi
ces(Figure
26afrom
[119]),which
islargely
dueto
thecom
pressibilityof
theair
andthe
dynamics
ofthemeniscus.A
sin
thecase
oftheporous
disc(Section
3.2.1)this
couplingcan
bereduced
byincreasing
the
pressures/flowrates
andtherefore
moving
towards
thejetting
regime,
where
most
ofthephysics
happensat
thetip
ofthejet
andnot
atthe
outletof
theorifi
ce.An
extremeexam
pleof
parallelisationof
the
break-upofthin
gasjets
isshow
nin
Fig.26b[62].These
gasjets
canbe-
comevery
thinunder
extremeco-flow
conditions,andbubble
sizescan
thereforebe
oftheorder
ofamicrom
etre.
3.2.2.2.Foamgeneration
inporous
media.In
thelim
itofvery
smallpore
sizesand
lowflow
velocitiesone
findsthe
applicationoffoam
genera-tion
inporous
media
(oftensandstone)
foren
hancedoil
recovery[120–124].In
this
field,typical
poresizes
areof
theorder
ofsom
emicrom
etres,leadingto
stronglylam
inarflow
which
isdom
inatedby
surfacetension
andviscous
forces(i.e.sm
allReand
Wenum
bers).
Inaporous
medium
,atsufficiently
lowflow
rates,bothfluids
may
followseparate
paths(“no-foam
regime”
inFig.27a
andc),leading
toalow
flowresistance
andhence
asm
allpressuredrop
acrossthe
porousmaterial.U
ponincreasing
theflow
rates,oneobserves
anincrease
inthe
pressuredrop,being
associatedwith
thecreation
ofacoarse
(“weak”)
foam(Fig.27a
andc).W
henacriticalpressure
gradient∇P*
isreached
inthe
porousmedium
uponfurther
increaseofthe
flowrates,the
pres-sure
dropjum
psabruptly
toamuch
highervalueas
aresultofthe
onsetofefficient
foaming
mechanism
staking
placewithin
thepores.Three
differentfoam
ingmechanism
shave
beenidentified
[120,121]which
areshow
nin
Fig.27d.“Lamellea
division”divides
analready
existingfoam
lamella,w
hile“Leave-behind”
createsone
dueto
theflow
aroundobstacles.The
thirdmechanism
is“Snap-off”,w
hichoccurs
inthe
porethroats
(narrowsection
between
twopores).Sim
ilartothe
phenomena
discussedin
Section2.4.2,
pressureand
flow
condition
slead
toa
destabilisationofthe
gasthread
inthe
pore,which
breaksup
togener-
atesm
allbubbles.Atthis
stage,about10
differentmechanism
softhis
snap-off
havebeen
identifi
ed[125],
themost
common
onebein
gprobably
“Roof-snap-off”,which
occurswhen
gasinvades
aliquid-
filled
pore,sim
ilarto
the
caseof
co-flow
through
acon
striction(Section
2.4.2).The
differencebein
ghere
that
one
dealswith
aparallelisation
ofmany
co-flowdevices
ofdifferentdimension,i.e.a
sit-uation
ofevenhighercom
plexitythan
theone
shownin
Fig.26afor
theparallelisation
oftwoidenticaldevices.A
livelydebate
istaking
placein
thecom
munity,w
hether“Snap-off”
or“Lam
elleadivision”
isthe
main
foaming
mechanism
[125].Since
foaming
andfoam
flowin
aporous
medium
aredom
inatedby
what
happensin
thepore
throats
(snap-off
andlam
ellaneed
tobe
pushedthrough
thepore
throats)the
criticalpressuregradient
∇P*
atwhich
foaming
occursisrelated
tothe
dimensions
ofthepore
throatsRP[124]
∇P ��
RP−2;
ð41Þ
Fig.25.(a)Sparging
fromanarrow
gap(gap
width:75
μm(top
image)
&100
μm(bottom
image))
viaan
instabilityofthe
air/water
interface(adapted
from[116]).(b)
Generation
ofequal-volum
ebubbles
onastep
usingthe
samemechanism
asin
(a)(adapted
from[118]).
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renckhan,A.Saint-Jalm
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anddepends
onthe
geometry
ofthepores.This
means
thatfor
small
porethroats,required
pressuregradients
forreliable
foamproduction
canbe
extremely
high.Above
thiscriticalpressure
gradient(andthe
as-sociated
criticalflowrates),foam
isgenerated
efficientlywith
bubblesizes
beingofthe
orderofthe
poresizes,i.e.m
icrometric.Bubble
sizesand
gasfraction
canbe
tunedby
tuning
theoveralland
therelative
flowrates,w
iththe
bubblesize
beingroughly
inverselyproportional
tothe
totalflowrate
Q=
QG+
QLin
theporous
medium
[126]
RB
�Q
−1:
ð42Þ
Anexam
pleofthis
isshow
nin
Fig.28.Unfortunately,little
system-
aticwork
hasbeen
doneatthis
stageto
establishaquantitative
linkbe-
tween
theporous
material,
theflow
conditionsand
thefinal
foamproperties.In
realporousmedia
with
microscopic
poresizes,pressures
tendto
becomeso
highthatthey
leadto
frequentfilmrupture.H
ence,an
understandingofthe
globalmechanism
sneeds
totake
intoaccount
coalescence.Aninteresting
(andfor
thepractitioner
important)
findingis
thatthere
isawide
rangeofpressure
gradientswhich
leadto
anunstable,
oftenoscillatory
flow
,andhen
ceoscillating
foamproperties.This
issh
ownby
thedotted
linein
Fig.27a.Researchersassociate
this
with
theoccurrence
ofintricatefeedback
mechanism
swithin
theporous
ma-
terial[122,124].Fig.27bshow
show
thetransition
between
theweak
andthestrong
foamregim
edepends
onthegas
andtheliquid
flow
rate.Anybody
lookingto
generateahom
ogeneousfoam
shouldthere-
forestrive
forsufficiently
highflow
ratesin
orderto
bein
the“strong
foam”regim
e.Most
considerationsoffoam
generationin
porousmedia
takeinto
accountindividual
bubbleson
ly.Asin
thecase
offoam
generationun
dersh
ear(Section
3.2.3),researchers
haverecen
tlybeen
ableto
showthatcollective
bubbleeffects
may
playanon-negligible
rolein
en-couraging
thebreak-up
oflargerbubbles
intosm
allerones.A
nillustra-
tiveexam
ple(from
[127])isshow
nin
Fig.29,where
onecan
seehow
thebubble
which
traversesthe
bottomofthe
constrictionbreaks
thebubble
which
passesatthe
top,which
thenbreaks
thebubble
atthebot-
tom.A
nindividualbubble
ofthesam
esize
which
traversesthisconstric-tion
atthesam
evelocity
doesnot
break.
3.2.2.3.High-speed
foaming
throughfibre
matrices
andstatic
mixers.In
orderto
obtainhigh
erfoam
ingrates,
scientists
usea
rangeof
purpose-designedporous-type
media
throughwhich
liquidand
gasare
co-injectedat
highvelocities
(upto
severalmetres
persecond).In
thiscase,bubble
generationprofits
alsofrom
thepresence
ofstrongvis-
cousand
inertialforces.One
classofdevices
isprovided
bystatic
mixers
(Fig.30a–c)[129–131]
which
arepurpose-designed
suchthat
arapid
flowofthe
gasand
theliquid
throughthe
interconnectednetw
orkof
poresleads
toan
optimised
shearingaction
onthe
bubbles,andhence
tobubble
break-up(Section
2.3).Thesemixers
canbe
drivenin
thelam
-inar
regime,leading
typicallyto
bubblesizes
oftheorder
of100
μm
(Fig.30d)with
awide
rangeofgas
fractions.Orthey
canbe
drivenat
highflow
ratesin
theturbulen
tregim
e,leading
tosm
allerbubble
sizesand
lower
gasfractions.In
[130,131], onecan
findaguideline
forsuch
staticmixers,linking
thetype
ofmixer
tobe
usedas
afunction
ofthe
fluidproperties
andapplications
foreseen.Other
typesofstatic
mixers
may
includethe
passagethrough
finegrids
ofdifferent
mesh
sizesor
through
systemslike
compact
steelwool
[132](or
similar
typesof
fibrous
materials).The
advantageof
suchsystem
sisthatthey
haveareasonably
highperm
eability,despitehaving
asm
allcharacteristiclength
scalewhich
fixesthe
obtainedbub-
blesize.These
“mixing
units”may
bepositioned
attheentry
ofa“foam
homogeniser”
which
may
simply
consistofavery
longtube
which
actson
thepre-foam
edsystem
sas
discussedin
Section3.2.2.4.Such
kindof
combinations
areoften
usedin
“compressed
airfoam
systems”,typical-
lyknow
forthegeneration
offirefighting
foams[132,133].The
obtainedfoam
scan
coverawide
rangeofbubble
sizes(dow
nto
someten
sof
microm
etres)and
canhave
awide
rangeofgas
fractions.
3.2.2.4.High
rateco-injection
instraighttubes.Efficientfoam
ingdoes
notnecessarily
requirecom
plexfoam
inggeom
etries.Under
certaincondi-
tions,a
simple
tubeis
sufficient.Co-injection
ofgas
andliquid
intoa
straighttube
atsufficiently
highflow
velocitiesleads
tocom
plexpat-
ternsoftw
ophase
flow(Fig.31a)
[134],many
ofwhich
generatebub-
blesand
thereforefoam
s,especiallyin
thepresence
ofsurfactants.Thephysics
oftheseprocesses
ishighly
complex,m
ixingdifferent
typesof
airentrain
men
t(Section
2.4.4)and
bubblebreak-up.U
ntilrecen
tly,this
hasbeen
studiedmostly
forengineering
purposeswhere
bubblegeneration
needsto
beavoided
oratleastunderstood
tooptim
isepres-
suredrops
andheatflow
problems.Researchers
havenow
realisedthat
someofthese
regimes
areextrem
elyefficientfoam
generators(Fig.31b
andc),providin
gfoam
swith
smallbubbles
andwell-controlled
gasfractions
[87,132,133,135].One
example
consistsofthe
co-injectionofgas
andfoam
ingsolution
atconstant
pressure(or
flowrate)
intoastraight
tubeof
typicallymillim
etricdim
ensions[87,135]
(Fig.31b).Thetube
needsto
bemuch
longerthan
itsdiam
eter(typically
afew
hundredtim
eslonger
thanthick)
inorder
forthe
mechanism
towork
efficiently.Moreover,the
Weber
numbers
Weof the
flowneed
tobe
sufficientlyhigh
sothatiner-
tialforcesplayarole
inthe
foaming
process.Upon
choosingthe
rightflowconditions,foam
scan
beobtained
with
verysm
allbubblesizes
(orderof
10μm
)(Fig.31d),at
veryhigh
productionrates
(litresper
second)and
overnearly
theentire
rangeofgas
fractions.Sm
allerquantities
offoams,butw
ithavery
precisecontrolover
thegas
fraction,can
beobtained
usingthe“D
ouble-Syringetechnique”
(Fig.31c)[87,161].This
usesasim
ilarmechanism
asin
theprevious
case,buthere
twosyringes
areconnected
toeither
sideofa
shorttubein
orderto
pushthetw
o-phase
mixture
backand
forththrough
the
tube.Atthe
outset,onesyringe
containsthe
gas,while
theother
onecontains
thefoam
ingliquid.Both
mix
efficientlyafter
afew
cycles,giv-ingrise
tofoam
swith
verysm
allbubbles(around
10μm
)and
with
Fig.26.Parallelisationofco-flow
devices.(a)Com
plexcoupling
ofparallelbubblingdevices
(from[119]).The
leftsideshow
sphotographs
andthe
rightsidethe
bubblingactivity
ofeachhole.From
topto
bottom,the
gaspressure
isincreased
atconstantliquidflow
rate.Thenotation
is[P
G(psi),Q
L (mL/h)].(b)
Parallelisationofm
icro-bubblegeneration
inthe
jettingregim
e(from
[62]).One
cansee
thingas
threadsform
edby
rapidgas/liquid
co-flowcom
ingoutofcapillaries
inatip-stream
ingmanner
(Section2.3).These
gas-threadsbreak
intomicrom
etricbubbles
furtherdow
nstream.
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renckhan,A.Saint-Jalm
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ing,Adv
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extremely
well-controlled
gasfractions
(Fig.31e).Obtained
bubblesize
distributionsare
similar
tothose
obtainedin
thecontinuous
flow.M
ostinterestingly,ascan
beseen
inFig.31e,they
areindependentofthe
finalliquid
fractionofthe
foam[87].
3.2.3.Gas
entrainmentatfree
surfacesand
bubblebreak-up
undershear
3.2.3.1.Breakingwavesand
hydraulicjum
ps.Asdiscussed
inSection
2.4.4,gas
entrainm
entis
mostly
associatedwith
highfluid
velocityand/or
underabrupt
variationsofthe
velocityfield
oftheflow
.Thisoccurs
inmany
naturalprocesses,awell-know
nexam
plebeing
thatofcascades.
Itisalso
atthe
originoffoam
ingat
theshore
breakon
thesea
[13,80]or
athydraulic
jumps.In
theseprocesses,m
anyofthe
basicsituations
describedin
Section2.4.4
may
simultaneously
occur,andany
under-standing
ofsuchcom
plexflow
srelies
onhow
faritcan
bedescribed
bycom
biningthe
elementary
mechanism
s.Researchershavedeveloped
anum
beroflab-scaleprototypes
inan
attemptto
simplify
thecom
plex-ity
oftheprocesses
[80,136].In
thecase
offoamgeneration
bywave
breaking,asshow
nin
Fig.32b,afulldescription
ofhowexactly
thewaves
trapthe
surroundingair
hasnot
yetbeen
obtained.Nevertheless,the
main
time-sequences
oftheph
enom
enologyare
knownand
summarised
inFig.32a
[80].First,amajor
partof
airen
trainment
occursas
theplunging
wave
hitsits
frontface(Fig.32a
—im
ageA).This
isthe
moststudied
andunderstood
mode
ofentrainment
(Section2.4.4),as
onemight
expectto
linkitto
thephysics
ofaplunging
jetconfiguration
(Section3.2.3.2).H
owever,
itsign
ificantly
differsfrom
theprototypal
scenario
discussedin
Section2.4.4
sincethe
impacting
jetisnot
continuous,itsgeom
etryis
much
more
complex
(with
anglesofim
pactchanging
with
time)
andthe
liquidreceiving
theim
pactundergoesitselfa
complex
flow(parallel
tothe
surfaceand
moving
upslope).With
suchcom
plexity,simulations
havebeen
apow
erfulsourceto
providesom
eprelim
inaryinsights
ofhow
much
aircan
beentrainm
entbythis
firstim
pactofthe
wave
(seereferences
in[80]).Then,there
areseveralpost-jetim
pactentrainment
modes,
allmostly
linkedto
thesplash
ofthefirst
impact.
Thisis
schematised
inFig.32a
—im
agesBand
Cwhere
subsequentim
pactsof
theforw
ardand
backward
splashesen
trappedsom
eair.
Lastly,som
eturbulen
ten
trainmen
tsoccur
allover
thevarious
subsequent
splashes,andat
theleading
edgeof
theturbulent
region(Fig.32a
—im
ageD).G
oingmuch
beyondaphenom
enologicaldescriptionofthis
processisrendered
challengingalso
becausethe
breakingwave
situa-tion
correspondsto
flowsof
low-viscosity
fluids,which
addsfurther
complexity
(disturbances,instabilities)
asdiscussed
beforefor
the
basicplunging
jetconfiguration
(seeSection
2.4.4).Let
usmen
tionth
atwhile
aplun
gingwave
isareason
ablyeffi
-cien
tmean
toincorp
oratelarge
amou
nts
ofair
into
water
(as
Fig.27.Foamgeneration
inporousm
ediain
thelow
velocitylim
it.(a)Sketchofthe
variationofthe
pressuregradientacrossthe
porousmaterialasa
functionofthe
totalflowrate
(inspiredby
[124])show
ingthe
differentfoaming
regimes.(b)
3D-illustration
of(a)considering
thegas
andliquid
flowrate
independently(from
[124]).(c)Differentflow
scenariosencountered
inthe
porousmaterial(from
[122]).(d)The
threemain
mechanism
sresponsible
forfoam
generation(from
[127],adaptedfrom
[120]).
0,00,4
0,81,2
1,60
100
200
300
400
500
6000,025 L/m
in0,057 L/m
in0,089 L/m
in0,121 L/m
in0,153 L/m
in
Averag bubble radius <RB> ( m)
Total flow rate Q
G + QL (L/m
in)
Liquid flow rate Q
L
µ
Fig.28.Dependence
ofaveragebubble
radiusoffoam
generatedby
co-flowofgas
andliq-
uidthrough
aporous
medium
generatedby
closelypacking
2mm
glassspheres.
Data
courtesyofR.-M
.Guillerm
ic,pre-work
to[128].
22W.D
renckhan,A.Saint-Jalm
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Colloidand
InterfaceScience
xxx(2015)
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as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
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Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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everyonecan
experien
cewhile
lookingat
thesh
orebreak
ona
beach),it
has
not
(yet)been
transform
edinto
aded
icatedfoam
ing
device.Gas
entrainments
within
hydraulicjum
ps(Fig.17c)
belongto
the
samefam
ilyof
self-aeratedsituations,w
hereair
isincorporated
asa
consequenceofrapidly
flowing
jetsassociated
tostrong
free-surfacede-
formations.It
isclear
thatnot
allhydraulicjum
psprovide
airentrain-
ment.
Usual
jumps
inasink
giveno
signsof
foamingor
bubbling.
How
ever,ifon
eincreases
thevelocity
oftheim
pactingjet,one
canstart
tosee
thefirst
bubblesentrained
inthe
fluid,originatingat
thejum
pwhere
thefluid
thickness
abruptlyvaries,as
shownin
Fig.32c.In
fact,itis
onlyfor
highenough
Froudenum
berFr
(typicallyFr
N3)
that
airis
entrained
[137],andthis
canbecom
ean
efficien
tfoam
ingmechanism
,asseen
inFig.32d.Experim
entsshow
thatinorder
toob-
tainsignificantairentrainm
ent,alarge
turbulentshearregion—
usuallycalled
a‘roller’—
needsto
beform
ed.Thisroller
islocated
atthetop
ofthe
thickfluid
region,asshow
nin
theschem
eofFig.32c
[137].Thegas
isthen
entrainedatthe
toeofthis
highshearregion,characterised
byin-
tensiveturbulen
ce.Thelength
ofthis
rolleris
directlyrelated
tothe
Froudenum
ber(see
referencesin
[137]).Similarly,the
amount
ofgasentrained
alsoincreases
with
theFroude
number.H
owever,there
arestillno
clearmodels
unambiguously
describingthiseffect,and
onlyphe-
nomenologicallaw
sare
proposedwhich
lacksatisfying
agreementw
ithexperim
entaldata.Infact,the
geometry
oftheexperim
entalsetupplays
arole,as
wellas
theam
ountofpre-entrainedgas
inthe
impacting
jet.
Eventhough
theentrainm
entconditionsby
bothmechanism
s,wave
breakingand
hydraulicjum
ps,havebeen
investigatedintensively
inthe
past,whatis
lackingalm
ostentirelyatthis
stageare
thoroughinvestiga-
tionsinto
theobtained
bubblesize
distributions,which
would
beim
-portant
forfoam
ingapplications.
3.2.3.2.Plungingjets
andfoam
inghoses.O
nefoam
ingtechnique
which
makes
systematic
useofair
entrainment
andbubble
break-upunder
shear
byaplun
gingjet
(Section2.4.4)
inacontrolled
manner
hasbeen
turned
intoastandardised
testmethod:
theRoss–M
ilestest
[138].Thehistoric
set-upisshow
nin
Fig.33awith
sometypicalexam
-ple
curves(Fig.33b)
andim
agesofthe
entrainment
process(Fig.33c).
Thisfoam
ingtest
belongsto
theASTM
databankof
testmethods
(identifi
edun
derthenum
berASTM
D1173-53(2001)).
Inpractice,
50mlofthe
solutionisplaced
inacylinder.U
singapipette
andafunnel
fixedata
heightof90cm
,200mlofthe
samesolution
isallow
edto
fallinto
thecylinder.A
ssoon
asallof200
mlsolution
hasfallen,the
foamheight
isrecorded.N
otethat
ifthe
impact
isinitially
ontheliquid
layer,thisisno
longerthe
caseonce
thefew
firstlayers
ofbubblesare
created.During
theprocess,bubbles
might
alsobe
destroyed(or
not)by
thefallin
gliquid,th
usmixin
gfoam
ingand
stabilityissues
atthe
s ametim
e.Foamsproduced
with
thistechnique
canbe
highlymonodis-
perseor
highlypolydisperse,w
ithpolydispersity
increasingwith
im-
pactvelocity
ofthejet.A
veragebubble
sizestend
tobe
oftheorder
ofafew
hundredmicrom
etresallthe
way
upto
afew
millim
etres.Foamproduction
ratesare
low,ofthe
orderof1
L/min.The
initiallyobtained
gasfraction
sare
verylow
andgenerally
increaseby
gravity-drivendrainage
ofthefluid
asthe
foamaccum
ulatesat
theliquid
surface.Themost
popularuse
ofthisfoam
ingtechnique
isprobably
thatoffilling
ourbathtub
with
foam.
Other
techniqueshave
beendeveloped
touse
airentrainm
entin
amore
systematic
andcontrolled
manner
forfoam
generation.Thisair
entrainmentm
ayhappen
attheoutletofnozzles
(Fig.34a)or
atspecif-ically
designedcross-sectionsofV
enturi-typenozzles,in
which
thefluid
flowcreates
anunderpressure
andtherefore
entrainssurrounding
air(Fig.34b).W
iththis
approach,lowto
intermediate
gasfractions
canbe
obtained.Inorder
toincrease
thegas
fractionofthe
foam,air
needsto
beinjected
actively.This
canbe
doneusing
compressed
air(Fig.34d)
orapropeller
system(Fig.34d–g).In
thelatter
case,anair/
water
mixture
isprojected
athighspeed
ontoafine
mesh.This
gener-ates
amixture
ofbubble
blowing/air
entrainment
throughthe
mesh
andbubble
break-upby
shear.Foamproduction
ratescan
reachmore
than
acubic
metre
perminute.
How
ever,bubble
sizestend
tobe
millim
etricin
thiscase,giving
riseto
areasonably
coarsefoam
.
3.2.3.3.Breakupunder
activeshear.In
orderto
obtainsm
allerbubbles,a
wide
rangeoffoam
ingdevices
hasbeen
developedby
engineerswhich
usemore
activelythe
fundamental
mechanism
sof
bubblebreak-up
Fig.29.Bubble–bubbleinteractionsm
ayplay
anim
portantrolein
bubblebreak-up.H
ereit
canbe
seenthatthe
bubblepassing
throughthe
bottomofthe
constrictionbreaks
theone
passingon
thetop,w
hichthen
breaksthe
oneon
thebottom
.From
[127].
Fig.30.High
speedco-flow
ofgasand
liquidthrough
purpose-designedstatic
mixers
generatesefficiently
foams.(a–c)
Examples
ofstaticmixer
geometries.(d)
Typicalbubblesize
distributionsobtained
inastatic
mixer
fordifferenttotalflow
ratesatconstantgas
fraction(Φ
=0.92)
(from[130]).
23W.D
renckhan,A.Saint-Jalm
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as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
undershear
describedin
Section2.4.3.In
thesedevices,the
foaming
fluidand
thegas
aredrastically
andheterogeneously
shearedin
orderto
effi-ciently
createafoam
with
sub-millim
etricbubbles.The
main
issuein
de-signing
andoptim
isingsuch
devicesisnotonly
toobtain
thedesired
foamin
termsofbubble
sizeand
gasfraction,butalso
toensure
thatthedevice
isefficient(rapid
foaming
atlowpow
erconsum
ption).One
highlypopular
foaming
devicewhich
isbased
onair
entrain-ment
andsystem
aticbubble-breakup
undershear
iscertainly
known
tomost
ofthe
readers:thekitchen
blender.
Inthis
device,air
isen
trainedat
thefree
surfaceof
theblended
liquid(Section
2.4.4),which
createslarge
bubbles,which
arethen
brokenunder
thecontinu-
ousshearin
gaction
ofthe
blender.The
interactionbetw
eenair
entrainm
entand
bubblebreak-up
leadsto
agradualin
creaseof
the
gasfraction
(asshow
nin
Fig.35a)and
adecrease
oftheaverage
bubblesize
overtime—
thisisnoticed
bythe
userasthefoam
becomes
increas-ingly
white
andsolid-like.This
processhappens
untilanequilibrium
stateisreached,w
hosecharacteristic
gasfraction
andbubble
sizede-
pendon
therheologicalproperties
oftheliquid
andthe
rotatingvelocity
oftheblender.A
sarule
ofthumb,the
higherthe
viscosityofthe
liquid,the
smaller
thebubbles
andthe
lower
thegas
fractionwhich
canbe
ob-tained
(Fig.35b).Depending
onthe
beatingtim
eand
thebeating
speed,obtained
bubblesizes
canrange
between
sometens
ofmicrom
etresand
afew
millim
etres.Extremeshearing
conditionsand
unusualfoamfor-
mulations
may
leadto
sub-micron
bubblesizes
[139].Ascan
beseen
Fig.31.(a)Typicaltw
o-phaseflow
patternsin
straighttubeswith
increasingratio
ofgasto
liquidflow
rate.Someofthese
regimes
canbe
usedto
generatefoam
sathigh
productionrates
andwith
smallbubble
sizes.One
example
isthe
continuousflow
inasim
plecapillary
(orlargertube)show
nin
(b),asecond
example
pushesthe
gas/liquidmixtures
repeatedlyback
andforth
throughatube
usingadouble
syringeshow
nin
(c).Bothtechniquesprovide
accesstoawide
rangeofgasfractionsand
toextrem
elysm
allbubblesizes.Exam
plesofsizedistributions
areshow
nin
(d)for
thestraighttube
andin
(e)for
thedouble
syringe.Panels
b–efrom
.[87]
Fig.32.(a)Schem
e(from
[80])and
(b)photograph
ofairentrainm
entbywave
breaking.(c)Schem
eand
(d)photograph
ofairentrainm
entat
ahydraulic
jump(both
from[13]).
24W.D
renckhan,A.Saint-Jalm
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W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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inFig.35a,the
initialfoaming
ratein
thecase
oflow-viscosity
liquidscan
bequite
rapid(about
1L/m
in),butthe
finalbubblebreak-up
may
takemuch
longer.Themain
issuewith
thekitchen
blenderfor
largerscale
applicationsisthe
factthatit
isanon-continuous
process.In
orderto
obtaincontinuity
andamore
explicitcontroloverthe
airinput(rather
thanrelying
onpassive
airentrainm
ent)and
theshearing
process,anum
berofadvanced
blendershave
beendeveloped
inthe
past.Afirst
classofdevices
arerotor–stator
mixers
(Fig.36a–d)which
consistofa
setofnarrow
ly-spacedstatic
“stators”and
rapidlyrotating
“rotors”through
which
thefoam
ingsolution
andthe
gasare
pressedsi-
multaneously.A
largebody
ofliteraturedeals
with
theoptim
aldesignof
therotor/stator
asafunction
ofthefluids
tobe
sheared[141–143].In
thiscontext,the
New
tonnum
ber(N
e)(defined
asthe
ratiobetw
eenthe
mechanicaldriving
forceand
theinertialforce)
isoften
usedto
de-scribe
thedevice
behaviour[141–143].
Inthese
devicesone
findsthat
themechanicalenergy
inputis
themostinfluentialparam
eterwhich
controlsthe
propertiesofthe
obtain-ed
foam.It
isafunction
oftherotor
speed,thefluid
viscosityand
thetim
ewhich
thegas/liquid
mixture
spendsin
thedevice
[142–145].The
widely-used
“Ultra-Turrax®
”(Fig.36e)
belongsto
thiscategory
ofrotor–stator
mixers,w
iththe
specialtythat
ittypically
containsonly
onerotor–stator
pair.Bubblesizes
obtained
inthese
kindof
devicescan
bevery
small,dow
nto
theorderofa
fewmicrom
etres,with
reason-ably
highfoam
productionrates.
Another
classofdevices
isbased
onthe
“Narrow
Annular
Gap
Unit”
shownin
Fig.37aand
b.Inthese
devices,gasand
liquidare
generallypre-m
ixedusing
aporous
plate(Section
3.2.1.3).Thispre-foam
isthen
injectedbetw
eenthe
impellers.Souidiet
al.[79]couldshow
thatoneof
themain
mechanism
sofbubble
generationin
thisdevice
appearsto
be“tip
streaming”
(asdiscussed
inSection
2.3and
shownin
Fig.15)which
leadsto
verysm
allbubblesizes
ofthe
orderof
10μm
(Fi g.37c).Themain
advantageisthat
thisdevice
requiresmuch
lower
rotationspeeds
(lower
energyinput)
thanthe
more
classicrotor–stator
devices[79,146].
Besideen
gineeringissues
concerningthedesign
ofsuch
kindof
mixers,one
hasto
beaw
areofthe
effectofbubble“cooperativity”,as
al-ready
mentioned
inthe
introduction.Asthe
bubblesbegin
tobe
closelypacked
theycannotbe
consideredany
more
asisolated
objects(as
donein
Section2).The
effectofthegas
volumefraction
hasbeen
investigatedin
controlledmodelexperim
entsusing
ashear
rheometer
[17,147,148](Fig.38a).The
authorsevidence
differentbreak-upregim
es.Inparticu-
lar,as
inthecase
ofcooperative
bubblebreakup
inconstrictions
(Fig.29),theyrealised
thatbubble–bubbleinteraction
becomes
impor-
tantandleads
tocriticalcapillary
numbersw
ellbelowthose
ofanisolat-
edbubble/drop
(Fig.38b).Theauthors
explainthis
enhancedinstability
bya“m
icrostructure-induced”instability
which
leadsto
apinch-offof
anelongated
bubbleby
itsneighbours
(Fig.38c)and
toacriticalstress
which
needsto
beobtained
inthe
foam(rather
thanacriticalcapillary
number)
[149].
Fig.33.Foamgeneration
byaplunging
jet.(a)The
historicRoss–M
ilestestw
hichlets
afoam
ingsolution
ofdefinedvolum
edrop
intothe
samesolution
fromawell-defined
heightandmeasures
theobtained
foamheight(from
[138]).(b)Exam
plesofthe
evolutionoffoam
heightwith
heightoverwhich
thesolutions
fall(from[138]).(c)
Images
ofplungingjets
andthe
accompanying
bubblegeneration
with
increasingim
pactvelocity(from
[80]).
25W.D
renckhan,A.Saint-Jalm
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dvancesin
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xxx(2015)
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Pleasecite
thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
3.2.3.4.Foaming
byshaking.O
neofthe
simplesttechniques
tofoam
aso-
lutionconsists
ofshakingaclosed
containerwhich
ispartially
filledwith
thesolution.Ifthis
isdone
inacontrolled
manner,the
containerisshak-
enat
specificfrequency,am
plitudeand
foracontrolled
duration.Thefoam
abilityofthe
solutionisthen
determined
bythe
amount
offoamcreated,and
thebubble
sizecan
alsobe
monitored
asafunction
ofthesh
akingparam
eters.Thisis
oftenreferred
toas
the“Bartsch
test”.Inthe
“Bartschtest”
theshaking
isperform
edby
acontrolled
flippingof
thecellat
controlled(and
variable)frequency.N
otethat
thisshaking
canalso
bedone
byhand,and
thisusually
providesagood
andcheap
es-tim
ationofthe
foamabilities
ofvarioussolutions.
Foamgeneration
byshaking
mixes
aboutallthedifferentm
echani-calfoam
ingeffects
which
wehave
discusseduntilnow
andistherefore
difficultto
describequantitatively.To
disentanglethe
differenteffects,
more
simple
experiments
havebeen
developed.Flatcells
were
usedby
Capset
al.[150,151],inassociation
with
arotation
setupproviding
consecutiveupside-dow
nflips
ofthecell.A
sshow
nin
Fig.39a,the
cellsare
soflatthatthey
generateaquasi-2D
foam,i.e.only
monolayers
ofbubbles.Thisconfiguration
allowsus
tovisualise
allthebubbles,as
afunction
ofthenum
berofflips
(Fig.39b).Asequence
ofimages
oftheobtained
foamswith
increasingnum
berofflips
nf is
shownin
Fig.39a,show
inghow
thebubble
size(and
hencethe
number
ofbubblesN)de-
creasedsystem
aticallywith
thenum
berofflips.These
experiments
andfurtheranalysis
ofthissetup
[150–152]finallydem
onstratethat,thanks
tothese
seriesofsuccessive
flipsofthe
flatcell,aspatially
homogeneous
foamcan
beproduced.M
oreover,thebubble
sizedistribution
eventual-ly
saturateswith
aGam
madistribution.The
obtainedaverage
bubble
sizedepends
onthe
initialamount
ofliquidand
canbe
linkedto
thecapillary
lengthofthe
foaming
solution.
3.3.Foaming
throughphase
transitionsand
byelectro-chem
istry
3.3.1.Nucleation
andgrow
thofbubbles
insupersaturated
liquidsThe
greatclassicswhich
make
useofbubble
generationthrough
nu-cleation
andgrow
thofbubbles
inasupersaturated
liquidare
knownto
mostofus
fromthe
beverageindustry:cola,cham
pagneor
beerfoam
s.In
mostcases,the
supersaturatedgas
isCO
2due
toits
highsolubility
inwater.The
supersaturationiseitherachieved
byexplicitly
applyinghigh
pressureswhen
fillingand
closingthe
bottles(fizzy
drinks),oritarises
naturallyas
aresult
oftheferm
entationprocess
(champagne,beer).In
most
ofthesecases,researchers
havebeen
ableto
showthat
bubblesare
generatedby
heterogeneous
nucleation(types
IIIand
IV)at
the
wallor
atimpurities
(Section2.5)
[11,153].Asisobvious
tothe
carefulobserver,
continuousbubble
streams
nucleatefrom
individual
nucleationsites,as
isshow
nin
Fig.40a.Thanksto
thiseffect,supersat-
urationin
these
beveragescan
bekept
lowand
istypically
ofthe
orderof5–10
only.Acham
pagnebottle,for
example,is
typicallyat
apressure
of5–10
barand
releasesaround
5Lof
CO2to
enhance
ourpleasure.
Similar
phenomena
areused
incosm
eticor
otherfood
products.Aclassic
example
isthewhipped
creamdispenser
which
decoratessom
ekitchens
(Fig.40c).Inthis
case,itis
the‘laugh
inggas’(nitrous
oxide)which
isdissolved
underhigh
pressureand
thenreleased
tocre-
atethe
bubblesin
thecream
.
Fig.34.Controlledair
entrainmentfor
foamgeneration:A
ircan
beentrained
bythe
liquidflow
(Ventouri-type
effect)(b,c),leading
tolow
andinterm
ediategas
fractions.(c–g)Gas
frac-tions
canbe
increasedsignificantly
byactively
injectingair,for
example
throughthe
useofa
propellersystem
.Theair/w
atermixture
isthen
propelledonto
agrid,w
herestrong
shearforces
turnthe
water
dropletsinto
airbubbles.(e–f)
Jet-Xfrom
ASU
L.(g)ALPH
AHF+
deLEA
DER
inaction
with
upto
1000Loffoam
/min.
Fig.35.Foaming
with
akitchen
blender(alldata
from[140]).(a)
Changeofair
volumefraction
with
timefor
differentfoaming
mixtures
containingparticles.The
variationofthe
ratiobetw
eenthe
surfactantconcentrationCS
andthe
particleconcentration
CPleads
essentiallyto
avariation
inthe
bulkviscosity
oftheliquid.(b)
Lineardecreaseofthe
maxim
umobtained
airvolum
efraction
with
theviscosity
ofthefoam
edliquid.
26W.D
renckhan,A.Saint-Jalm
es/A
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xxx–xxx
Pleasecite
thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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Inorder
tofoam
highlyviscous
liquidsand
largequantities,on
eoften
usesclassic
extruderscrew
s(Fig.40b)
toexert
highpressures
onthefoam
ingliquid.This
isalso
themethod
ofchoice
inorder
tofoam
thermosensitive
polymers,w
hichare
mixed
with
thegas
athigh
temperatures
underhighpressures,to
givearapid
foaming
(andsim
ul-taneous
solidification)as
theliquid
isreleased
toam
bientpressure.
3.3.2.Cavitationand
boilingAsfaras
weknow
,foaming
throughboiling
iscurrently
littleused
inasystem
aticmanner.Itis
ratherknow
nto
most
ofusas
anunpleasant
surprisewhen
thesoup
orthe
milk
areleft
unwatched
alittle
toolong
onthestove.
Theon
lysystem
aticuse
known
tous
isthat
ofgels
which
foamwhen
incon
tactwith
theskin.These
gelscon
tainsub-
stances(forexample
isopentane)which
areliquid
atroomtem
perature,but
gaseousat
bodytem
perature.Hence,th
econtact
with
theskin
(shavinggels,tooth
pastes,etc.)makes
thesegels
foam.Shearing
the
gelonthe
skinhelps
tobreak
themicro-structure
andto
getthenucle-
ationprocess
going.Asim
ilarfoam
ingsystem
isfound
inthree-phase
aerosolcans,themost
classicbeing
shavingfoam
cans.Inthis
casethe
phasetransition
isdriven
byapressure
change,ratherthan
atem
peraturechange.The
overallsystemconsists
oftwoim
miscible
liquidscreating
anem
ulsionunder
pressure(see
bottomofFigs.2
and40d,B).The
dispersedphase
isaliquid
oflowvapour
pressure(m
ostcommonly
butan/propanmix-
tures)which
remains
liquidunder
thepressure
conditionsofthe
con-tainin
gvessel.
Once
thepressure
isreleased,
thedispersed
liquidchanges
phaseand
theentire
emulsion
dropletturnsinto
agas
bubble.The
finalbubblesize
istherefore
determined
bythe
initialdropletvol-
ume[154].This
iswhy
itisrecom
mended
toshake
thecan
beforeuse
inorder
tore-em
ulsifythe
mixture.Bubble
sizesin
theseapplications
aretypically
around50
μm.
An
increasingly
popularfoam
ingtechnique
employs
cavitation(Section
2.5).Thisis
ofparticular
interestwhen
foamswith
micron-
Fig.36.Aclassic
amongstthe
foaming
devices:therotor–stator
mixer.(a)
Overallsketch
ofthedevice
containingthe
rotating“rotor”
andthe
static“stator”
(from[141])
(b)Side-view
(from[141])
and(c)
topview
(from[70])
ofanelem
entaryunit
ofarotor–stator
mixer.(d)
Photographsofa
typicalstatorand
rotor(from
[70]).(e)The
“Ultra-Turrax®
”—
awidely
usedrotor–stator
devicecontaining
onlyone
rotor/statorpair.
Fig.37.TheNarrow
Annular
Gap
Unit(N
AGU).(a)
Overalldevice
configuration(from
[146]).(b)Exam
plesofpropellers
usedfor
theshearing
action(from
[79]).(c)Exam
plesofbubble
sizedistributions
obtainedfor
differentpropeller
geometries
(rotationspeed:1600
rpm,Q
G=
10mL/m
in,GL=
30mL/m
in)(from
[79]).
27W.D
renckhan,A.Saint-Jalm
es/A
dvancesin
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xxx(2015)
xxx–xxx
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thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
sizedbubble
aredesired.H
istorically,suchkinds
ofbubbleswere
gener-ated
usingacoustic
pressurefields
(sonication).How
ever,sincethe
pro-duction
ratesare
toolow
,hydrodynamic
cavitationis
making
itsway
intofoam
ingdevices
[155,156].Different
devicesexist
touse
arapid
flowofthe
foaming
liquidin
amanner
thatasudden,strong
pressuredrop
occurswhich
leadsto
thegeneration
ofcavitationbubbles.The
most
popularscenario
consistsof
rapidflow
through
acon
striction,
leadingto
apressure
dropjust
behind
theconstriction.Specialcare
needsto
betaken
torender
these
bubblesstable
asthey
aresw
eptaw
aywith
theflow
.Acertain
degreeofsupersaturation
with
anothergas
helps.Themost
importantingredients
arestabilising
agents[156].
3.3.3.Foaming
byelectrolysis
Anelectro-chem
icalway
ofproducinggas
bubblesis
providedby
electrolysis.Forthis
purpose,avoltage
isapplied
acrosstw
oelectrodes
placedwithin
thesam
ewater
reservoir(Fig.41a),turning
oneofthe
electrodesinto
acathode
(negativelycharged)
andone
intoan
anode(positively
charged).Sincewater
molecules
decayand
recombine
per-manently
(2H2 O
↔2H++
2OH−),the
resultingH+protons
willcom
-bine
with
electronsfrom
thecathode
toform
hydrogengas
(H2 ),w
hilethe
OH−ions
willliberate
electronsatthe
anodeto
formwater
andox-
ygen:
Cathode:
4Hþþ
4e−↔2H
2Anode
:4O
H−↔2H
2 OþO
2 þ4e
−:
ð43Þ
Hence,hydrogen
bubblesare
createdat
thecathode,w
hileoxygen
bubblesare
createdat
theanode.In
bothcases,the
bubblesare
blown
atthesurface
oftheelectrode,m
eaningthateithergravity
oranexternal
flowneeds
todetach
themfrom
thesite
where
theygrow
[162].Thebubble
sizeistherefore
controlledby
thesam
emechanism
sdiscussed
inSection
s2.4.1
and2.4.2,th
ekey
differencebein
gthat
thegas
isblow
nby
anelectro-chem
icalreaction.Asecond
keydifference
isthat
theblow
ingsites
occurgenerally
onsm
alldefectson
theelectrode
sur-face.The
bubblesare
thereforeonly
weekly
attachedto
thesurface
(asif
theywere
blownfrom
atiny
orifice)and
theresulting
bubblesizes
aretherefore
ofat
leastan
orderof
magnitude
smaller
than
bubblesblow
nfrom
orifices(typically
sometens
ofmicrom
etres,asshow
nin
Fig.41b[157]).Since
thenum
berofbubbling
sitescan
bevery
highon
anelectrode,this
isan
efficienttechniqueto
producereasonable
quan-tities
offoamswith
tinybubbles.For
thisreason,one
ofthemain
appli-cation
sof
thisfoam
ingtechnique
iselectro-fl
otation.Flotation
efficiencyincreases
with
decreasingbubble
sizesince
thetotalinterfa-
cialareaisinversely
proportionaltothe
bubblesize.A
typicalflotationcellis
shownin
Fig.41c[157].A
common
useis
that
ofwaste
water
treatment
ormineralflotation
(onsm
allscales).Thenum
berofsites
andthe
bubblesize
canbe
variedby
tuning
the
currentdensity
(Fig.41b),which
isconvenient
forapplications.
Particularcontroland
eventhe
generationofhighly
monodisperse
bubblescan
beobtained
byworking
with
stronglypointed
electrodeswhich
canproduce
micron-sized
bubbles(Figure
41cfrom
[158]).As
usual,thisgain
incontrolneeds
tobe
paidby
astrongly
reducedproduc-
tionrate.
Thekey
constraintforapplications
ofbubbleand
foamform
ationby
electrolysisisthe
restrictedchoice
ofgaseswhich
canbe
produced.Thisis
commonly
oxygenor
hydrogen,which
restrictsquite
significantly
theirfield
ofuse.
3.4.Conclusionsand
outlook
Wehope
thatthisreview
showsthatthere
aremany
ways
ofincor-porating
bubblesinto
aliquid
phase.W
ehave
concentratedhere
on
Fig.38.(a)Break-up
ofbubblesunder
shearin
afoam
with
closelypacked
bubbles(from
[149]),which
occursatcapillary
numbers
wellbelow
thoseofisolated
bubbles(b)
from[149].
(b)Com
parisonbetw
eenthe
criticalcapillarynum
berrequired
forbreak-up
ofindividualdroplets(“G
racecurve”
Section2)
andassociated
data(circles)
andbetw
eendensely
packedbubbles
(“Foams”)
anddroplets
(“Emulsions”)
(c)Proposed
reasoningfor
theearlier
break-upofbubbles
inthe
presenceofneighbouring
bubbles:amicro-structure
inducedinstability
(from[149]).
Fig.39.Foaming
byflipping
ashallow
cell(adaptedfrom
[150]).(a)Consecutiveim
agesofthefoam
inthe
cellafternf=1,2,6,12,18,and
24flips.(b)Evolution
ofnumberofbubblesw
ithnum
berofflips
fordifferent
contentsofliquid
(φ)in
thecell.
28W.D
renckhan,A.Saint-Jalm
es/A
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InterfaceScience
xxx(2015)
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thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
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physicaleffects,butthereader
shouldbe
aware
thatawealth
ofchem-
icalandbiologicalfoam
ingtechniques
isalso
available.Itneeds
tobe
addedthatthere
existsalarge
number
of“naturalfoaming
techniques”,where
foamsoccur
naturallyin
nature(on
thebeach,in
waterfalls,etc.)
orin
industrialprocesses.Inboth
cases,thisnaturalfoam
productionmay
poseserious
problems.U
nderstandingthe
mechanism
sattheir
or-igin
cantherefore
bevery
helpfultoavoid
thefoam
formation.
Itis
importan
tto
keepin
mind
thatfor
agiven
fluid
anyfoam
ingtechnique
leadsto
acharacteristic
bubblesize
distribution,gasfraction
andfoam
productionrate
(Table3).The
generationof
foamswith
awide
rangeofthese
parameters
generallyrequires
theapplication
ofdifferentfoam
ingtechniques.
Awealth
ofliteratureisavailable
tocapture
certainkey
propertiesof
differentfoam
ingtechniques.H
owever,at
this
stageon
lythemost
simple
configuration
sare
beginning
tobe
explainedin
asystem
aticmanner
—for
example
bubblingfrom
individual
nozzlesor
bubblebreakup
undershear.A
ndeven
inthese
simple
cases,many
important
questionsrem
ainopen.
Much
more
systematic
work
within
acoherent
physicalframew
orkneeds
tobe
donein
thefuture
toshed
more
lighton
themore
complex
foaming
mechanism
s.Suchwork
needsto
establishthe
roleofthe
differ-ent
dynamicforces.A
swehope
tohave
shownin
thischapter,a
highlyappropriate
framew
orkfor
takinginto
accountthese
differentforces
isprovided
byworking
with
dimensionless
hydrodynamic
numbers,as
listedin
Table2.The
useofthese
numbers
allowsus
togroup
awide
rangeofobservations
bythe
main
physicalmechanism
sofa
process.The
physicalmechanism
softhe
bubblingprocess
aregenerally
well
reflectedby
theobtained
bubblesizes
andsize
distribution.Due
tothe
difficultyofm
easuringbubble
sizedistributions
infoam
s,much
ofthisinform
ationis
lackingin
thepast
literature.Modern
characterisationtechniques
provideamore
straightforward
accessto
thisinform
ation,which
shouldbe
exploitedmore
heavilyin
thefuture.These
techniquesinclude
lightscattering,X-ray
andNMRtom
ographyor
highspeed
im-
aging.Theavailability
ofthesize
distributionsshould
helpus
tograsp
more
profoundlythe
physicalmechanism
swhich
controlthebubble
formation.H
owever,great
careneeds
tobe
takenin
thisexercise:ob-
tainedbubble
sizesand
sizedistributions
may
dependmore
onthe
foamstability
thanon
thefoam
ingtechnique
used!Coalescen
ceand
gasexchange
[1,3]betw
eenbubbles
may
completely
changethe
sizedistribution
within
afew
secondsofthe
lifetim
eofthe
foam.M
uchof
thepast
literaturehas
thereforemixed
measures
offoaming
andfoam
stability—
which
capturevery
differentphysicalphenom
ena.Anum
berofkey
challengesrem
ainto
betackled
inthis
subject.Thefirst
challengerequires
toestablish
adescription
offoaming
which
al-low
sus
tomove
away
fromthe
dilutelim
itof
individualbubbles
inorder
totake
properlyinto
accountthe
many
typesofbubble
interac-tions
which
occurinmostcom
monly
usedfoam
ingtechniques.The
sec-ond
challengeisto
considerthe
influenceofthe
complex
visco-elasticproperties
ofgas/liquid
interfaces
which
contain
stabilisingagents.
Thepresence
oftheseagents
leadsto
anum
berofinterfacialstresses
which
needto
betaken
intoaccount
inaproper
dynamic
description.First
stepsinto
combining
thephysics
ofbubble
break-upin
densefoam
sand
theinfl
uenceof
theinterfacial
viscoelasticityhave
beentaken
byevidencing
theim
portanceofa
criticalstressinthe
foam,rather
thanacriticalcapillary
number
[149].Afinalkey
challengewillbe
thedescription
ofthe
foaming
ofliquids
with
non-N
ewtonian
flow
Fig.40.Examples
offoamgeneration
viabubble
nucleationand
growth.(a)
Continuousbubble
generationand
riseatnucleation
sitesatthe
wallofa
champagne
glass(im
agefrom
[11]).(b)
Awhipped
creamdispenser
usesnitrous
oxide.(c)Afoam
extruderis
typicallyused
tofoam
highlyviscous
liquidsbringing
thegas
(oftenCO
2 )into
solutionat
highpressure.
(d)Aerosolcans
aretypically
usedfor
cosmetic
applications.Thegas
caneither
bein
solution(case
A)or
itcanbe
chosensuch
thatitisan
insolubleliquid
underthe
pressurecondition
inthe
bottle.Inboth
cases,uponrelease
oftheliquid
intoam
bientpressure,the
gascom
eseither
outofsolution
orevaporates
(from[154]).
29W.D
renckhan,A.Saint-Jalm
es/A
dvancesin
Colloidand
InterfaceScience
xxx(2015)
xxx–xxx
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thisarticle
as:Drenckhan
W,Saint-Jalm
esA,The
scienceoffoam
ing,Adv
ColloidInterface
Sci(2015),http://dx.doi.org/10.1016/j.cis.2015.04.001
properties,which
changetheir
flowproperties
upondeform
ationand
with
deformation
rate.Infact,m
anyprocesses
requirethe
successfulfoam
ingofcom
plexfluids
(polymer
melts
andsolutions,particle
sus-pensions,em
ulsions,etc.).Ofgreat
importance
inthe
futurewillbe
todevelop
foaming
tech-niques
which
pushbeyond
currentlimits.The
foaming
ofhighlyviscous
liquids,forexam
ple,remains
agreatchallenge
dueto
theim
portantin-fluence
ofthefluid
viscosityon
thedifferentflow
instabilities.Another
boundaryto
bepushed
willalso
bethatofthe
obtainedbubble
sizes—
especiallytow
ardssm
allbubbles
andlow
gasfraction
.Lowdensity
foamswith
bubblesizes
wellbelow
1μm
havegiant
surfaceto
volume
ratios(1
cm2of“nano-foam
”can
containthe
surfaceofan
entirefoot-
ballfield!)which
isofinterestforcatalytic
reactions.Moreover,therm
alconduction
isreduced
byorders
ofmagnitude,w
henthe
bubblesize
issm
allerthan
themean
freepath
ofthegas
molecules
(about0.1
μmfor
airatroom
temperature
andam
bientpressure).To
sumup,decades
ofconsiderableengineering
work
haveprovided
uswith
awide
rangeofreliable
foaming
techniques.Thecurrent
andfuture
challengeis
tobe
ableto
arriveat
asatisfying
descriptionand
predictionof
thecom
plexfoam
ingprocesses.O
ntheon
ehand,th
isshould
helpto
optimise
currentfoaming
processes,onthe
otherhand,
this
shouldprovide
uswith
thepossibility
togenerate
controlled
foamswith
awiderrange
ofproperties,stimulating
newresearch
direc-tions
andleading
tothe
emergence
ofnewapplications
offoams.
Ackn
owledgem
ents
Theauthors
would
liketo
thankReinhard
Miller
formotivating
thewriting
ofthisarticle
andfor
hisim
portantcontributions
toresearch
onbubbles.W
ealso
thankBillRossen,Stubenrauch,Em
manuelle
Rio,Dom
iniqueLangevin,N
ikolaiDenkov
andJean-Eric
Poirierfor
veryuse-
fulcomments
onthis
manuscript.W
.Drenckhan
acknowledges
fundingfrom
anERC
StartingGrant(agreem
ent307280-POMCA
PS).
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ColloidInterface
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