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chaoter 14 Phase Equilibrium

Jun 03, 2018

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Haiqal Aziz
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    Chapter 14. Topics in Phase EquilibriumChapter 14. Topics in Phase EquilibriumChapter 14. Topics in Phase EquilibriumChapter 14. Topics in Phase Equilibrium

    The simplest models for vapor/liquid equilibrium

    14.1. The14.1. The14.1. The14.1. The //// formulation of VLE.formulation of VLE.formulation of VLE.formulation of VLE.

    Pyf iiv

    i =

    iii

    l

    i fxf =

    l

    i

    v

    i ff =

    iiiii fxPy =

    Extension of modified Raoults Law

    Overcome the limitation of modified Raoults Law

    Introduce vapor-phase fugacity to explain nonideality

    From eqn (11.52)

    at equilibrium

    - Raoults law

    - Henrys law

    - Modified Raoults law

    sat

    iii PxPy =

    iii HxPy =

    sat

    iiii PxPy =

    => for a species whose Tc Applied only to low pressure

    From eqn (11.90)

    => Vapor phase

    => Liquid phase

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    1sat

    i

    i

    i

    Usually poynting factor (14.2)

    ]RT

    )P-P(Vexp[Pf

    sat

    i

    l

    isat

    i

    sat

    ii =

    From eqn (11.44)

    satiii

    sat

    i

    l

    isat

    i

    ii PxP]RT

    )P-P(V-exp[

    y =

    1 ii ==

    ]RT

    )P-P(Vexp[PxPy

    sat

    i

    l

    isat

    i

    sat

    iiiii =

    (14.1) => gamma/phi formulation

    If => (14.1) becomes raoults Law

    sat

    iiii PxPy =

    1 i =If => (14.1) becomes modified Raoults Law

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    To use eqn(14.1) for the analysis of VLE => need to know the value ofii

    sat

    i ,,P

    i

    i

    i

    sat

    iCT

    B-APln

    +

    =

    )]-2(yy2

    1B[

    RT

    Pexp jk

    j k

    jikiii +=

    sat

    i 0, jkji =

    RT

    PBexp

    sat

    iiisat

    i

    =

    2) => need to obtain and

    (14.3)

    (14.4)

    (14.5)

    1) => obtained by the Antoine eqnsat

    i

    ii

    sat

    i

    Values of the pure species vivial coeff. of the species in the mixture

    (11.69) ~ (11.74)

    : fugacity coeff for pure i as a saturated vapor in eqn(14.4)

    RT

    )-2(yyP2

    1)P-P(B

    exp

    j k

    jkjikj

    sat

    iii

    sat

    i

    i

    i

    +

    ==(14.6)

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    3) : can be obtained from the various models ( Van Laar, Wilson, UNIFAC, etc ..)

    RT

    Py)P-P(Bexp

    12

    2

    2

    sat

    111

    1

    +

    =

    RT

    Py)P-P(B

    exp 12

    2

    1

    sat

    222

    2

    +

    = (14.7b)

    (14.7a)

    i

    For a binary system comprised of species 1 and 2, this becomes

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    Dew point and Bubble point Calculation using Gamma/Phi formulatDew point and Bubble point Calculation using Gamma/Phi formulatDew point and Bubble point Calculation using Gamma/Phi formulatDew point and Bubble point Calculation using Gamma/Phi formulations => need iterationions => need iterationions => need iterationions => need iteration

    )y,,y,y,P,T( 1-N21i

    =

    )x,,x,x,T( 1-N21i =

    )T(fPsati =

    P

    Pxy

    i

    sat

    iii

    i = sat

    ii

    ii

    iP

    Pyx =(14.8) (14.9)

    since 1y,1x ii ==

    i i

    sat

    iii

    PxP =

    i

    sat

    ii

    ii

    P

    y

    1P =(14.10) (14.11)

    1) BUBL P calculation

    => Calculation (yi) and P , given xi and T

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    Bubble P calculationsBubble P calculationsBubble P calculationsBubble P calculations

    Fig. 14.1 Block diagram for the calculation BUBL P

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    2) Dew P calculation

    => Calculation xi and P , given yi and T

    - BUBL P and Dew P calculation : temperature is given => can calculatesat

    iP

    i

    i

    sat

    i C-lnP-A

    BT =

    sat

    iP

    - BUBL T and Dew T : T is unknown => need initial estimate for T to do iteration

    i) (for BUBL T) (for Dew T)i

    sat

    iiTxT = i

    sat

    iiTyT =

    where (14.12)

    ii) Multiply eqn(14.10) (14.11) by (outside summation) and didice by

    (inside summation)

    sat

    iP

    i

    sat

    j

    sat

    iiii

    sat

    j)P/P)(/x(

    PP = )

    P

    P(

    yPP sat

    i

    sat

    j

    i i

    iisat

    j = (14.14)(14.13)

    iii) Calculate corresponding T from eqn(14.3)

    jsat

    jj

    jC-

    lnP-A

    BT =

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    Dew P calculationsDew P calculationsDew P calculationsDew P calculations

    Fig. 14.2 Block diagram for the calculation DEW P.

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    BUBL T calculationBUBL T calculationBUBL T calculationBUBL T calculation

    => Calculate (yi, T) given xi and P

    Fig. 14.3 Block diagram for the calculation BULB T.

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    DEW T calculationDEW T calculationDEW T calculationDEW T calculation

    => Calculate (xi , T) given yi and P

    Fig. 14.4 Block diagram for the calculation DEW T.

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    Flash calculationFlash calculationFlash calculationFlash calculation

    )N,,2,1i(1)-K(1

    Kzy

    i

    ii

    i =

    +

    =

    In chap 10. Flash calculation is based on Raoults law and K-value correlation

    => Use the gamma/phi formulation

    )N,,2,1i(1)-K(1

    zx

    i

    ii

    =

    +

    =

    (10.16)

    First,yii F01-y,1y ===

    i i

    ii

    y 01-1)-K(1KzF =

    +

    =

    i i

    i

    x 01-1)-K(1

    zF =

    +

    =

    (14.17)

    (14.18)

    Second,xii F01-x,1x ===

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    14.2 VLE from Cubic Equation of State14.2 VLE from Cubic Equation of State14.2 VLE from Cubic Equation of State14.2 VLE from Cubic Equation of State

    For VLE, li

    v

    i ff =

    ,Px

    f

    i

    i

    i = l

    ii

    v

    ii

    l

    ii

    v

    ii xyPxPy ==

    (11.48)

    Since,

    Vapor pressure for a pure speciesVapor pressure for a pure speciesVapor pressure for a pure speciesVapor pressure for a pure species

    - Usually , can be obtained by experimental measurement

    Generic Cubic Equation of state

    sat

    iP

    - at equilibrium can be obtained using EOSsat

    iP

    b)b)(vv(

    )T(a

    b-v

    RTP

    ++

    =

    If P -> , V -> b , if P -> 0, V ->

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    Fig. 14-7

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    0ln-lnlnln vil

    i

    l

    i

    v

    i ==

    )P,T( ii =

    satPP

    )T(fPsat

    i =

    in that case

    - For pure species,

    and

    - For a saturated liquid or vapor )P,T( sat

    iii =

    P

    ZRT

    v=

    )Z()-Z(

    -Zq-1Z

    iiii

    ii

    iiii++

    +=

    where

    - Two widely used cubic eqn of state

    Sorve / Redlich / kwung (SPK) eqn

    Peng/Robinson (PR) eqn

    - Vapor & vapor-like Roots of the Generic Cubic EOS (use )

    ii

    ii

    iiiiii q

    Z-1)Z)(Z(Z

    +

    +++=

    (3.52) -> (14.31)

    (3.56) -> (14.35)

    Liquid & liquid like Roots of the Generic Cubic EOS

    Parameter : eqn (3.45), (3.46), (3.50), (3.51)

    )q,,b,a( iiii

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    Pure number : )Tr(,,,, i

    v

    i

    l

    i Zd-Zv

    i

    l

    i ln,ln

    iiiiii Iq-)-ln(Z-1-Z=lnFrom (11.37) (11.37)

    => Table 3.1

    - Procedure to obtain for pure for a give T, PsatiP

    1) Calculate using eqn (14.35)(14.36) before that, calculate parameters

    2) Using eqn(11.37), calculate before that, calculate qi, Ii

    3) Check if 0=ln-ln v

    i

    l

    i

    If yes, P -> Psat

    , if no, iterationEqn for calculating vapor pressure -> table 14.3

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    14.3 Equilibrium and Stability14.3 Equilibrium and Stability14.3 Equilibrium and Stability14.3 Equilibrium and Stability

    If system surrounding => thermal and mechemical equilibrium heat exchange(Q) and expansion work (w) are reversible.

    T

    dQ-

    =T

    dQ

    =dSsurr

    surr

    surr

    0T

    dQ-dS t

    0dS+dS surrt

    tTdSdQ

    tttt PdV+dU=dQPdV-dQ=dW+dQ=dU

    0TdS-PdV+dUTdSPdV+dU tttttt

    By thermodynamic 2nd law ,

    By thermodynamic 1st law

    Under these circumstance

    dQ : heat transfer for systemT : system =

    surrT

    (14.65)

    (14.66)

    Inequality : apply to every incremental change of the system between

    nonequilibrium states

    equality : holds for changes between equilibrium states (reversible)

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    eqn(14.61) : too general to apply to practical problem

    => need more restricted version

    0)dS(or0)dU( ttttV,U

    t

    V,S

    t

    0)TS-PV+U(d0TdS-PdV+dUP,T

    tttttt

    tttttt TS-PV+U=TS-H=G

    0)G(d P,Tt

    At const, T, P

    (14.67)

    Determination of equilibrium states

    1) Express Gt as a function of the numbers of moles of the species in the

    several phases

    2) Finds the set of values for mole number that minimize Gt subject to the

    constraints of mass conversion

    At equilibrium 0=)G(d P,Tt (14.68)

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    At constant T, P, must be continuous function of x1, and the'''

    G,G,G

    0>G ''

    => Criterion of stability for single-phase

    0>dx

    )RT/G(d2

    1

    2

    (14.65)(const. T, P)and

    0>dx

    Gd 2

    1

    2

    (const. T, P)

    From eqn(12.30)

    0>dx

    )RT/G(d+

    xx

    1=

    dx

    )RT/G(d2

    1

    E2

    211

    2

    iiE xlnxRT-G=G

    RTG+xlnx+xlnx=

    RTG

    E

    2211

    1

    E

    21

    1 dx)RT/G(d+xln-xln=

    dx)RT/G(d

    )P,Tconst(xx

    1->

    dx

    )RT/G(d

    21

    2

    1

    E2

    (14.65)

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    2211

    E

    lnx+lnx=RT

    G

    1

    2

    2

    1

    1

    121

    1

    E

    dx

    lndx+

    dx

    lndx+ln-ln=

    dx

    )RT/G(d

    21 ln-ln=

    zero Gibbs-Duhem eq.

    1

    2

    1

    1

    2

    1

    E2

    dx

    lnd-

    dx

    lnd=

    dx

    )RT/G(d

    1

    1

    2 dx

    lnd

    x

    1=

    From eqn(12.6)

    In combination with eqn(14.70)

    11

    1

    x

    1->

    dx

    lnd(const T, P)

    )P,Tconst(0>dx

    d,0>

    dx

    fd

    1

    1

    1

    1