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    MIT OpenCourseWarehttp://ocw.mit.edu

    5.60 Thermodynamics & Kinetics

    Spring 2008

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    5.60 Spring 2008 Lecture #14 page 1

    Multicomponent Systems, Partial Molar Quantities,

    and the Chemical Potential

    So far weve worked with fundamental equations for a closed (nomass change) system with no composition change.

    dU TdSpdV dA SdT = = pdVdH =TdS+Vdp dG = SdT +Vdp

    How does this change if we allow the composition of the system to

    change? Like in a chemical reaction or a biochemical process?

    Consider Gibbs free energy of a 2-component system ( , , 1, 2 )G T p n n

    dG =

    T

    G , , dT +

    G

    p

    dp+

    G

    n1

    dn1 +

    n

    G dn2

    p n n 2 1 2 , ,1 2 , , 2 T p n, , 1 T n n T p n S V 1 2

    We define i G

    as the chemical potentialof species iniT p n, , i

    ( , , ) is an intensive variablei T p nThis gives a new set of fundamental equations for open systems

    (mass can flow in and out, composition can change)

    dG = SdT +Vdp+ idnii

    dH =TdS+Vdp+ idnii

    dU TdSpdV + i i= dni

    dA= SdT pdV + idnii

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    5.60 Spring 2008 Lecture #14 page 2

    G H U Ai = = = =

    S p n , T V n,niT p n, , ji ni , , ji ni S V n, ji ni , ji

    At equilibrium, the chemical potential of a species is the same

    everywhere in the system

    Lets show this in a system that has one component and two parts,

    (for example a solid and a liquid phase, or for the case of a cell

    placed in salt water, the water in the cell versus the water out of

    the cell in the salt water)

    Consider moving an infinitesimal amount dn1 of component #1 from

    phase a to phase b at constant T,p. Lets write the change in state.

    ( , , phase a) = dn T p ( , ,phase b)dn T p 1 1adG = 1

    ( )b 1( ) dn1

    a1( )b < 1( ) dG < 0 spontaneous conversion from (a) to (b)b1

    ( )a < 1( ) dG > 0 spontaneous conversion from (b) to (a)

    At equilibrium there cannot be any spontaneous processes, so

    b1( )a = 1

    ( ) at equilibrium

    e.g. liquid water and ice in equilibrium

    waterice ice( , ) = water( , )T p T p

    at coexistence equilibrium

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    5.60 Spring 2008 Lecture #14 page 3

    water cell T p ( , andFor the cell in a salt water solution, ( ) , > water solution) T p( ) ( )the cell dies as the water flows from the cell to the solution (this is

    what we call osmotic pressure)

    The chemical potential and its downhill drive to equilibrium will be

    the guiding principle for our study of phase transitions, chemical

    reactions, and biochemical processes

    Partial molar quantities

    i is the Gibbs free energy per mole of component i, i.e. the

    partial molar Gibbs free energy

    G = i = Gi ni T p n , , j iG = n + n + + n = n n G"1 1 2 2 i i i i = i i

    i iLets prove this, using the fact that Gis extensive.

    G T p( , , n1, n2 ) = ( , , 1, 2 )G T p n n

    ( , , 1, n ) ( , , 1,dG

    T p n 2 = G T p n n 2 )d

    G

    ( )n

    1

    G

    (

    n2 )

    + = G n n n2 , ,n ( )1 T p, , ( ) T pT pn 2 , , 1 1, , 2 T p n

    n1 n2

    n1 1 + n22 = G

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    __________________________________________________

    5.60 Spring 2008 Lecture #14 page 4

    We can define other partial molar quantities similarly.

    A

    = Ai A= n A+ n A +"+ n A = n A1 1 2 2 i i i i

    i ni , , j iT p n

    partial molar Helmholtz free energy

    note what is kept constant not to be confused with

    n

    A

    = i iT V n , , j i

    H

    n = Hi H = n H + n H +"+ n H = n H1 1 2 2 i i i i

    i i T p n , , j ipartial molar enthalpy

    U

    ni

    , , j i

    = Ui U = nU + n U +"+ nU = i1 1 2 2 i i nUii T p n

    partial molar energy

    Lets compare of a pure ideal gas to in a mixture of ideal gases.

    Chemical potential in a pure (1-component) ideal gas

    o oFrom ( , ) = G ( ) + RTlnp

    ( , ) = T + pG T p T T p ( ) RTlnp0 p0

    Chemical potential in a mixture of ideal gases

    Consider the equilibrium

    pA +pB =ptot

    mixedA,B

    pureApAp 'A , p 'B

    Fixed Partition

    \

    At equilibrium mix T p, , = pureT pA( tot) A( , , A)

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    5.60 Spring 2008 Lecture #14 page 5

    Also pA(pure) =pA (mix) =ptotXA

    Daltons Law

    SoA(mix T p, , tot) = A(pure T ptotXA), ,

    A( ) + RT p X

    = o T ln tot A p0

    = Ao ( )T + RTln

    ptot + RTlnXAp0

    (pure T ptot)A , ,

    A( , , tot) = A(pure T ptot) + RTlnXAmix T p , ,Note XA < 1 A (mix T p , tot) < A ( , tot), ,pure T pThe chemical potential of A in the mixture is always less than the

    chemical potential of A when pure, at the same total pressure. Thisis at heart a reflection about entropy, the chemical potential of A

    in the mixture is less than if it were pure, under the same (T,p)

    conditions, because of the underlying (but hidden in this case)

    entropy change!