35
EMULSIFICATION IN TURBULENT FLOW A. GOAL AND PROBLEMS 1. REFERENCES H = Hinze, J. O. Turbulence, McGraw-Hill, New York, 1975. TL = Tennekes, H; Lumley J. L.; A first course in turbulence, The MIT Press, Cambridge, 1972 B = Batchelor, G. K The theory of homogeneous turbulence, Cambridge, 1953. L = Levich, V. G. Physicochemical Hydrodynamics, Prentice Hall, Englewood Cliffs, New Jersey, 1962. T = Coulaloglou, C. A.; Tavlarides, L.L Description of interaction processes in agitated liquid-liquid dispersions. Chemical Engineering Science 1977, 32, 1289. P = Princen, H. M. The equilibrium shape of interfaces, drops, and bubbles. In Surface and Colloid Science, Matijevic, E. Ed.; Wiley, New York, 1969, Vol. 2, p. 1. 2. NARROW SLIT HOMOGENIZER ( ) L u V Q p S 3 = = ε Isotropic turbulence (chaotic and non-directional)

A. GOAL AND PROBLEMS 1. R EFERENCES Hfluid.ippt.gov.pl/conex/sofia_meeting/Emulsification... · 2003. 11. 8. · HYDRODYNAMICS INTERACTION 12434 1244344 Π Π If Π in both phases

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  • EMULSIFICATION IN TURBULENT FLOW

    A. GOAL AND PROBLEMS 1. REFERENCES H = Hinze, J. O. Turbulence, McGraw-Hill, New York, 1975. TL = Tennekes, H; Lumley J. L.; A first course in turbulence, The MIT

    Press, Cambridge, 1972 B = Batchelor, G. K The theory of homogeneous turbulence, Cambridge,

    1953. L = Levich, V. G. Physicochemical Hydrodynamics, Prentice Hall,

    Englewood Cliffs, New Jersey, 1962. T = Coulaloglou, C. A.; Tavlarides, L.L Description of interaction

    processes in agitated liquid-liquid dispersions. Chemical Engineering Science 1977, 32, 1289.

    P = Princen, H. M. The equilibrium shape of interfaces, drops, and bubbles. In Surface and Colloid Science, Matijevic, E. Ed.; Wiley, New York, 1969, Vol. 2, p. 1.

    2. NARROW SLIT HOMOGENIZER

    ( )Lu

    VQp

    S

    3∆==ε

    • Isotropic turbulence (chaotic and non-directional)

  • 3. OVERALL GOAL (1) Drop size distribution vs. stirring (ε), interfacial tension (σ),

    viscosity ratio (ηd/ηc) and drop life-time (τD) (surfactant adsorption Γ and distribution).

    (2) Phase inversion 4. IMMEDIATE GOAL

    • Understand the emulsification mechanism. • Describe quantitavely variations of drop size ∆R vs. variation of

    life time ∆τD due to surfactants. ∆N

    R RR+∆R

    τD

    τD+∆τD

    N 5. APPROACH Grasp the main factors and the overall scheme

    (a) Account for polydispersity by considering discrete set of sizes

    (b) Neglect dependence of rate constants on size (c) Assume that drops split always on two equal size drops (d) Assume that only equal size drops coalesce

  • B. DROPS AND FILMS 1. MAIN EVENTS DURING FLOCCULATION OR COALESCENCE

    F = Driving Force (Buoyancy F , Brownian, Turbulent, Surface Interactions)

    Rd=43

    3π ∆ρg

    Main parameters

    • Drop Shape • Life Time, τ

    • Rate of Thinning, V V d hd t

    = − ;

    VVhdcrh

    inith

    1∝=τ ∫

    • Critical Thickness of Rupture, hcr • Interfacial Mobility (Surfactant)

  • 2. TRANSITION SPHERE - FILM

    22

    Ta

    Re 2 hFV

    V

    σπ=

    Inversion (Film Formation) Thickness, hi:

    1Ta

    Re =VV

    σπ

    =2

    Fhi

    Inversion at the same dissipation of energy •

    3. FILM RADIUS ( ) FRPP lf =π− 2

    cldf R

    PPP σ+== 2

    FR

    Rc

    =σπ 22 σπ

    =2

    2 cRFR

    3

    34

    cRgF ρ∆π=

  • 4. LIFE TIME OF DROPS DRIVEN BY BUOYANCY

    VVhd

    h

    h

    1~final

    in

    ∫=τ

    ( )52

    32

    Re2Ta1~

    322~

    32

    ccc

    c RRFhVR

    RFhV

    ηπσπ=

    ηπ=

    • Increasing drop radius increases the driving force but thereby

    increases also the film radius, thus decreasing the drainage rate and increasing life time.

    Qb + ll

    0

    50

    100

    150

    0.00 0.02 0.04 0.06 0.08 0.10

    Dwodqhldms S`xknq qdfhld

    τ < /-034 . Qb

    Life

    time,

    τ, s

    ec

    Small drops (no film)

    1 / Rc , mm-1

    0

    20

    40

    60

    80

    100

    120

    0 100 200 300 400 500 600 700

    Life

    time,

    τ, s

    ec

  • 5. ROLE OF THE ADSORPTION

    Dis

    join

    ing

    pres

    sure

    Thickness

    Pc'

    Pc''

    ∆P P= c- ( )Π t

    2

    d

    PRσ∆ = − Π 36

    hA Beh

    −κΠ = − +π

    Ads

    orpt

    ion,

    Γ

    Concentration, C

    Initialconcentration~ 100 CMC CMC

    Effectiveconcentration

    • The effective concentration is much lower than the real bulk

    concentration.

  • Surface coverage θ

    0.0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1.0

    Life

    time,

    sec

    onds

    0

    20

    40

    60

    80

    100

    120

    140

    1.5x10-4 wt.% BLG1.5x10-4 wt.% β−casein1x10-3 wt.% β−casein3x10-2 wt.% β−casein

    Colliding Drop Technique

    θCR = 0.75

    • Variation of bulk concentration, C, and surface age, tW.

    Surface potential, ψs, mV

    0 20 40 60 80 1

    Life

    time,

    τ, s

    econ

    ds

    0

    20

    40

    60

    80

    100

    120

    140

    5 µM10 µM25 µM

    1 µMBubbles: Drops:

    10 µM50 µM100 µM146 µM200 µM

    DDBS (12 mM NaCl)• Both lead to change of Γ. 00 • For DDBS there is a rather sharp transition between unstable and

    stable films, depending on the surface potential. • The bubbles are stable with surface potential higher than

    =70 – 80 mV. thSψ

  • 6. DRAINAGE RATE AND LIFE TIME OF THIN FILMS • Surfactant Balance

    Convection + Diffusion = 0 • Stress Balance

    Shear = Elastic + Viscous

    hh

    VV S+= 1Re

    23

    Re 32

    RPhV

    η∆=

    TkDh SS Γ

    η= 6

    ScrcrC

    hhxx

    xxxhP

    R /;1ln23 2

    2

    2

    =

    +−η=τ

    - with θ = 0.1, hS = 300 nm – strong surface mobility - with hcr = 40 nm, τ = 21 s

    • Role of the surface viscosity

    2~elasticitySurfaceviscositySurface

    RhSS

    ηη

    • The true surface viscosity, ηS, can play a role only for small films and mobile surfaces when hS >> h, but then ηS ≈ 0.

    • For dense monolayers hS ~ 0.5 ÷ 1 nm - the surface mobility is not important.

  • Interfacial Viscosity

    2

    2

    rv

    rzv r

    Sr

    ∂∂η+

    ∂Γ∂

    Γ∂σ∂=

    ∂∂η

    ( ) SSSSG

    rS hR

    RDE

    rvr

    ηη

    ηη

    η∂∂η∂σ∂ 2

    222 ~//~

    //~

    ViscousElastic

    Surface viscosity is coupled with surface mobility (through hS) and can play a role ONLY for mobile surfaces.

    But then the TRUE surface viscosity is small.

    Even for small films (R = 10 µm) and mobile surfaces (hS = 10 nm) the effect of surface viscosity is comparable to surface elasticity only if ηS > 0.1 sp.

    Apparent Dilatational Viscosity

    ;~~2

    2

    2

    appdG

    SS

    hR

    RR

    EhD

    hh

    ηηη

    diffGS

    Gappd tED

    RE ==η2

    The apparent surface viscosity is due to dissipation through diffusion and is NOT related to intermolecular interaction

    appdη depends on the film radius, i.e. it is NOT a property of the

    adsorbed layer and CANNOT be directly measured in a separate experiment.

    It is extremely high even at low concentration:

    ( ) sp1.0~10

    101~ 5

    23

    −ηappd

  • 7. BASIC EQUATIONS FOR FILM DRAINAGE Lubrication

    h

    z

    r

    2

    2

    dzv

    rp r∂η=

    ∂∂

    0=∂∂

    zp

    0=∂∂+

    ∂∂

    zv

    rv zr

    Boundary Condition at z = ±h/2

    dtdhVvUv zr 2

    12

    =−==

    2

    2

    rv

    rzv r

    Sr

    ∂∂η+

    ∂σ∂=

    ∂∂η

    zcD

    rD

    rU

    S ∂∂−=

    ∂Γ∂−

    ∂∂Γ 2

    2

    0

    ( ) 22

    10 RzCrCc +=

    ( )∫ −π=FR

    drrppF0

    02

    Emulsions

    ∂∂+

    ∂∂η=

    ∂∂ρ 2

    2

    2

    2

    zv

    rv

    rvv rrrr

    z

  • 8. RUPTURE OF THINNING FILMS

    Wave pressure:

    ( ) ζ ′′σ+ζΠ′+=2

    hPP plw

  • 9. EMULSION FILMS SURFACTANT IN THE DROP PHASE (SYSTEM II)

    Uniform Distribution of the Surfactant on the Film Surface

    (a) (b)

    0=∆Γ � 0=Γ

    ∆Γ=σ∆ GE

    � ReII VVV pure >>=

    • The surfactant has no effect on the rate of thinning.

    Chemical Demulsification

    DemulsifierEmulsifier Emulsifier

    • The demulsifier fills in the spaces between the adsorbed

    emulsifier molecules damps the interfacial tension gradient ∆σ and increases many times the rate of thinning and coalescence.

  • Comparison of the Life Times of Systems I and II

    System I

    Water

    Water

    Oil

    Oil

    System II

    ∫∞

    −=τcrh

    Vhd

    ;s3. O/Wτ0W/O =τ1000100Re

    ÷=≈VpureV

    ~O/W

    W/O

    W/O

    O/Wτ

    τ

    V

    V s35=

    The ONLY DIFFERENCE between the two systems is the SURFACTANT LOCATION.

    • The surfactant concentration does not affect the life time of the emulsion W/O (system II).

  • 10. GENERALIZED BANCROFT RULE

    System I

    Water

    Water

    Oil

    Oil

    System II

    c1~ ; 1 ~S ReG

    h PV VV h

    − Π τ = + E

    ( )ττ

    W/O

    O/W

    O/W

    W/O/≈

    ××

    −−

    −8 10 52 3E

    PPG

    c

    cHYDRODYNAMICS INTERACTION

    124 341 244 344

    ΠΠ

    If Π in both phases is zero, τW/O

  • C. DROP SIZE DISTRIBUTION

    1. ISOTROPIC TURBULENCE (KOLMOGOROV) ε - rate of energy dissipation per unit mass

    lu

    uluu

    322 ~

    /~1 ρρρ

    τερ

    20

    3/23/22 ~;~ uplu ρε

    2. PRESENT THEORIES (STEADY DISTRIBUTION)

    coalescebreak tN

    tN

    ∆∆=

    ∆∆

    break

    coalescence

    EE

    eNNNσ−

    τ=

    τ=∆

    br

    br

    br

    brbr

    ududEdE /~;~;~ br

    232 τρσσ

    ( ) ( )443442143421

    efficiency

    /

    frequencycoll.

    22

    coalesce

    contacteife ττ−×=∆∆ eNdu

    tN

    3

    contact /~;/~ dNud Φτ

    2/1eife3/4

    3/2 ln ετ+Φ−=

    εσ dd

  • 3. APPROXIMATION OF ∆N/N BY δ - FUNCTION ∆N

    RK RR t( )c

    ( )t t+∆

    ( )t

    N

    ( )( )

    ( ) dRetN

    tRdN cRR 2, −α−πα= ( )tα=α

    • Kolmogorov’s drops become important at longer times

    ( ) ( )∫=KR

    K tRdNtN0

    ,

    Since

    ( ) 1== ∫∫ dRRfNdN

    one can set

    απ=

    −δ= adRa

    RRaN

    dN c1

    • This reduces most equations to the monodisperse case, including

    those for coalescence rate:

    ( )2coal ~~ cRR RNdNdNV ∫ ′

    • Justifies assumptions (b) and (d). • Fails at Rc t RK (small drops). • Works better when coalescence is present.

  • D. TURBULENT PRESSURE AND DROP SHAPE

    • Eddies are NOT molecules

    [TL] Correlation coefficients

    =−

    eddiesfor1-0.5moleculesfor10 6

    (H., p. 310) For large Reynolds numbers and small distance, r, the pressure gradient does NOT depend on time

    ( ) ( 3/4222 4 rApp )BA ερ=−

    ( ) ( ) 3/22 2~~ rApp ερ∆∆

    ( ) ( ) pprp ∆+= 0

    • Laplace equation [P] Outside pressure p = p(r), inside pressure pin = const.

    ( ) ( ) →×σ=− curvatureinprp “Equilibrium” shape of stable drops.

    2l

    2Rturb

    • Under dynamic conditions – inside pressure is replaced by the viscous normal stress pnn.

    • Possible role of time and temporal pressure fluctuations (a) Through the time dependence of the velocity correlation

    function Qpp(r, t) (H, p. 308 Eqs. (3.298), (3.296)). (b) Through the time spectra and distribution functions (TL, p. 274

    and Chapter 6).

  • E. DROP BREAKAGE

    1. CRITICAL (KOLMOGOROV) SIZE, RK If ( ) Rrp /σ>∆

    lcr

    2x

    • Find local capillary pressure Pc(x). • Determine lcr from drop volume and the maximum Pc:

    ( ) 0=

    ∂∂

    xxPc

    • Determine the drop radius RK, at which the maximum in Pc

    disappears – this will give a generalized form of Kolmogorov size with numerical coefficient:

    6.04.06.0~ −− ρεσKR

    2. BREAKAGE TIME, τB

    • Time needed for deformation from sphere to breakage at lcr

    2

    2

    rv

    rp

    tv

    ∂∂η+

    ∂∂−=

    ∂∂ρ

    • Scalling

    ( ) Rplvlrt B /~/~~~ σττ=τ

  • • Inertia regime

    rp

    tv

    ∂∂

    ∂∂ρ ~

    lRl /~/ σ

    ττρ

    2321212

    in ~~ RRl

    σρ

    σρτ

    • Viscous regime

    2

    2~

    rv

    rp

    ∂∂η

    ∂∂

    2/~/l

    llR τησ

    Rσητ ~visc

    • Limiting radius between the two regimes

    ( )

    ( )( )( ) τη

    ρτητρ

    ∂∂η∂∂ρ=

    2

    2

    2

    22 ~//~

    // l

    lll

    rvtvRe

    From Re = 1 and τvisc (or τin)

    →σρ

    η=

    2

    lim

    2

    Rl

    σρη2

    lim ~R

  • • Rayleigh instability – only inertia regime (Shih-I Pai, Fluid dynamics of jets, § 1.9)

    R0

    l R-2 0

    - Determine R0 and l from the conservation of volume - Critical wave with length λcr ≈ (l-2R0)cr = 2πR0

    ( )( ) ( ) ( )0

    2

    0

    030

    2Ray

    ;11 RkxxxiJ

    xiJxiR

    =−′

    ρσ=

    τ

    2/30

    21

    ~ R

    σρτ

    - Formally coincides with the previous result but with different

    quantities. - The total breakage time is obtained by adding to τRay the time

    for expansion to length l.

    • Goal – Solve Stokes equation inside the drop with Laplace equation at least for small deformations (from sphere and/or cylinder) to obtain dynamic shape and breakage time with numerical coefficients.

  • F. GENERAL KINETIC SCHEME

    L

    dnj dt¢ j dt¢dq

    • “Convective diffusion“ in time ”space”

    ( ) iii dndqSLdtjjS =+′−′

    ni an Ni= total number and concentration of i – drops j = flux = NiV Nif = const – concentration of i-drops in the feed V = linear velocity dqi = production of i per unit volume in the element θ = L/V = residence time in the element

    θ== ii N

    LVN

    SLSj

    f

    i i idN N N dqdt dtθ

    −= + i

    • Source terms

    coalbreakiii dqdqdq +=

  • G. KINETIC SCHEME WITH ONLY BREAKAGE

    1. MAIN ASSUMPTIONS

    • Drops break in half, forming two smaller drops

    3/1

    11

    11

    22

    == −− iiiiRRvv

    • Drops with size smaller than Kolmogorov’s (Ri ≤ RK) do not

    break. • The rate constant are assumed eventually independent of Ri

    (ki = k). • Since ( )2/3or iiBi RBRa=τ

    Bi

    , all Ni(t) drops break simultaneously after time τ .

    ( ) 0=τ+ Bii tN

    ( ) ( ) 0=τ∂

    ∂+=τ+ BiiiBii t

    NtNtN

    iBiiB

    i

    i NkNt

    N −=τ

    −=∂

    ∂ 1 B

    i

    Bik τ

    = 1

    • depends weakly on vBiτ i and is assumed constant, τ

    B.

    31

    3/11

    3/1

    243

    π==τ ii

    Bi

    vaRa

    8.02 31

    1 ==τ

    τ −+i

    i

  • 2. THREE-SIZE SYSTEM ∆N

    vv1v2vk

    N

    v1 = initial v3 = vk

    • Assume that . Dubious approximation even for a monodisperse emulsion, since N and thereby R and τ

    BBB kkk == 21B changes

    with t, so that τB and kB must depend at least on Rc(t).

    11 Nk

    dtdN B−=

    212 2 NkNk

    dtdN BB −=

    22BkdN k N

    dt=

    ( ) ( kBB NNkNNkd )tdN −=+= 21 kNNNN ++= 21

    • The process stops at R = RK (N=Nk).

  • • Nk can be determined from the volume fraction Φ:

    ∑∑−==Φ

    ki

    k

    ii NvvN1

    111

    12/

    dtdN

    dtdN ik

    i

    ikk ∑−

    =

    −− −=1

    1

    11 22

    • At short times (kt = X Ü 1) Nk Ü N and

    ( )0/ln NNYXY ==

    • Exact solution:

    ( )[ ]XkXX eXYeXYeY −−− +−=== 114;2; 21

    ( ) Xk eXYYYY −+−=++= 23421exact

    • If Nk can be neglected

    1lnorln ==dX

    Ydkdt

    Yd B

    • If the exact function (i.e. experimental data) is approximated by

    lnY, the apparent rate “constant” k is much smaller than k

    ( )tBappB (see the second figure below):

    ( ) BB kXkdXYd

  • 0 1 2 3 4 5 0

    0.66667

    1.3333

    2

    2.6667

    3.3333

    4

    Y

    EXP(X)

    Y3

    Yexact

    Y2 Y1

    Yexact = 4-(3+2*X)*EXP(-X) Y1 = EXP(-X) Y2 = 2*XEXP(-X) Y3 = 4*(1-(1+X)*EXP(-X)) EXP(X)

    0 2 0

    0.25

    0.5

    0.75

    1

    1.25

    Y

    0.1

    0.3

    0.5

    0.7

    0.9

    dY/d

    X

    X

    Yexac = ln(N/N0) =

    X = kt

    4 6 0

    0.25

    0.5

    0.75

    1

    1.25

    Y

    0.1

    0.3

    0.5

    0.7

    0.9

    dY/d

    X

    LN(4-(3+2*X)*EXP(-X))

    = kt

  • 3. CONTINUOUS PROCESS WITHOUT COALESCENCE For the i-size in moment t:

    ( ) ( ) ( )KitNkNktNNdt

    dNi

    Bii

    Bi

    iifi ,...,12 11 =−+θ−

    θ= −−

    • Sum up over all i. • Summation stops at Kolmogorov size with Ni = Nk. • Assume kiB = kB = 1/τB. • For the n-th pass:

    ( ) ( )tNtN nK

    i

    ni =∑

    =1

    ( ) ( )[ ]tNtNNdt

    dN nk

    nB

    nf

    n−

    θ−

    τ+

    θ= 11

    (a) Slow Breakage (τB > θ)

    ( )011 >−=θ

    −τ

    slslB kk

    • Neglect nkN

    ( )

    τθ−

    τθ−= − tkBB

    nfn sle

    NtN 1

    /1

    ( )

    τ+=→ B

    nf

    n tNtN 10

    • Steady state kslt → ∞ (follows also from dNn/dt=0):

    ( ) Bnfn NtNτθ−

    =∞→/1

  • (b) Fast Breakage (τB < θ)

    011 >=θ

    −τ

    fB k

    ( )

    τθ

    −τθ= 1

    1/tk

    BB

    nfn fe

    NtN

    ( )

    τ+=→ B

    nf

    n tNtN 10

    t

    Nfn

    Nk

    N≤( )∞

    N

    slow

    fast

    • In the fast regime there can be also a plateau if the Kolmogorov size is reached.

  • H. COALESCENCE RATE

    tZ

    tZNkNkN

    Ndt

    dN iiiBi

    Biifi

    ∂∂−

    ∂∂+−+

    θ−

    θ= +− 22 11

    tZi∂

    ∂ = number of coalescence events between drop of volume vi in unit time.

    1. COALESCENCE OF SPHERICAL DROPS (BIMOLECULAR REACTION)

    212 AACk

    i →

    tZ

    ∂∂

    = number of successful collisions

    ENdtZ 23/73/1επ=

    ∂∂

    E = efficiency factor, analog of activation energy F = driving force for coalescence Fext = external (turbulent) force Fint = interaction (repulsive) force between the drops

    F = Fext - Fint

    • Since both Fext and Fint depend on R, some collisions (for which F < 0) will NOT be efficient.

  • F

    ξ = reaction coordinate (distance )-1

    Fext≤

    Fext ≤ - efficientFext

    ¢

    Fext¢ - non-efficient

    Fint

    2. CONSECUTIVE IRREVERSIBLE REACTIONS FOR DROPS FORMING

    A FILM

    212 AZADc kk →→

    τDτc Z = intermediate complex F coalescence

    flocculation

    ξ

    Fext≤

    Fext≤

    FextFint

    ¢

  • SINGULAR PERTURBATION

    L

    dnj dt¢ j dt¢dq

    dtdqN

    dtdN i

    ii +∆

    θτ=

    θτ

    • Macroscale

    • Microscale

    • Back to macroscale – coupling of macro and micro events: - The rocket slows down the train - The speed of the train affects the taking aim

  • • The barrier depends also on the size, since the driving pressure is ∆P = 2σ/R - Π.

    • Successful coalescence corresponds to

    02 max >Π−σ=∆

    RP

    Kinetic Scheme

    CI

    Bii

    iii dqdqdqdtdqN

    dtdN +=+

    θ∆= ;

    00

    t0 and θ = macroscopic time and time scale τ = microscopic time scale scaled times: t = t0/θ and t = t0/τ

    dtdqN

    dtdN i

    ii +∆

    θτ=

    θτ

    If τ/θ → 0, then →= 0dtdqi blow up of the micro-events.

    • Micro-kinetic scheme in microtime t (scaling time is the collision

    time – scale, τc).

    211

    1 21 Nkdt

    dN c−=τ

    0

    211

    1tZNk

    dtdZ c

    ∂∂+=

    τ

    0

    21tZ

    dtdN

    ∂∂−=

    τ

  • Z = number of complexes (2 drops with film which can rupture). They must rupture at time t0 + τD, where τD is the drainage time:

    ( ) ( ) 00

    0 =τ∂∂+=τ+ DDtZtZtZ

    ZkZtZ c

    D 20

    1 −=τ

    −=∂∂

    Estimate of τ c Scale N1 by N10, the number of drops 1 at t = 0 (N1 = N10N1′)

    ( ) →′−=′τ

    2

    12101

    110 2 NNkdt

    dNN c 101/1 Nkc

    c =τ

    21

    10

    1 2 NNdt

    dN −= (a)

    ZNNdt

    dZD

    c

    ττ−= 21

    10

    1 (b)

    with N1(0) = N10 from (a) and (b):

    tNN

    2110

    1 +=

    ZNK

    dNdZ

    211 2

    1 −−= D

    c NKτ

    τ=2

    10

    Introduce x = K/N1

  • The solution of the linear equation is

    xexxxx

    Z −

    ++

    ×+++−= const...

    !22ln21

    2

    Keep only 1/x. With Z = 0 at x = x0 = K/N10 (i.e. at t = 0) one obtains

    For x → 0 it becomes

    tt

    KN

    xxZ

    21211 10

    0 +=+−=

    Going back to macro-time t0 by substituting t = t0/τc, one obtains for any i (Note that Ni0 is Ni(t0))

    ( )

    00

    020

    0

    1

    200

    202

    0

    2141

    2122

    tkNtNkZ

    dtdN

    tkN

    NkNkdtdN

    cii

    icii

    D

    i

    cii

    icii

    ci

    i

    +=

    τ−=

    +−=−=

    +

    (c)

    • For simplicity we have implicitly assumed (by taking x > τc, corresponds to the outer solution and to scaling t = t0/τD. The determination of the integration constants for this solution requires matching of the inner and outer solution (A.H. Nayfeh, Perturbation methods, John Wiley, 1973, p.114).

    • The coalescence contribution to the balance of Ni is:

    ×−

    +=

    i

    i

    Zidtdq

    complexesofdeathofrate

    21twoof

    ecoalescencofratecoal

    ( ) ( )

    dttdNx

    dttdN

    dtdq iii 21

    coal−= +

    Here t is macro-time and the two derivatives are given by (c).

  • 3. TURBULENT FORCE F ext AND FILM RADIUS R F (a) Collision probability

    • The coalescence process in the emulsion is an ensemble of parallel events, occurring between different pairs of drops. Hence, the overall speed will be determined by the fastest ones.

    • Since τD ~ 1/R , the most favorable collisions between the deformed drops are head on (corresponding to smaller RF):

    2Rturb

    • If Zsph are the collisions between spherical drops, the number of favorable collisions, Z, will be roughly

    2

    =R

    RZZ turbsph

    (b) Force Balance on Film

    2RF

    Rturb

    ∆p r( )

    ∆p

    ( ) drrrpF π∆= ∫ 2ext

    (area outside film)

    2ext

    2FRR

    F πσ≈

  • EMULSIFICATION IN TURBULENT FLOWA. GOAL AND PROBLEMSGrasp the main factors and the overall scheme

    B. DROPS AND FILMS8. Rupture of Thinning FilmsUniform Distribution of the Surfactant on the Film SurfaceChemical DemulsificationC. Drop Size Distribution1. Isotropic Turbulence (Kolmogorov)2. Present Theories (Steady Distribution)

    Justifies assumptions (b) and (d).D. TURBULENT PRESSURE AND DROP SHAPEEddies are NOT moleculesPossible role of time and temporal pressure fluctuations

    E. DROP BREAKAGETime needed for deformation from sphere to breakage at lcrLimiting radius between the two regimes

    F. GENERAL KINETIC SCHEMEV = linear velocityG. KINETIC SCHEME WITH ONLY BREAKAGE

    Drops break in half, forming two smaller dropsH. COALESCENCE RATE

    Singular Perturbation

    For simplicity we have implicitly assumed \(by tThe realistic case, (D >> (c, corresponds to the outer solution and to scaling t = t0/(D. The determination of the integration constants for this solution requires matching of the inner and outer solution (A.H. Nayfeh, Perturbation methods, John WileThe coalescence contribution to the balance of Ni is: