C Thermodynamic Relationships Involving the Equilibrium Constant1

For the gas-phase reaction

A+baBca+daD(2-2)

1. The true (dimensionless) equilibrium constant

RTlnk=ΔG

K=aCcaaDd/aaAaBb/a

where ai is the activity of species i

ai=fifi

where fi = fugacity of species i

fi = fugacity of species i at the standard state. For gases, the standard state is 1 bar, which is in the noise level of 1 atm, so we will use atm.

ai=fifi=γiPi

where γi is the activity coefficient

K = True equilibrium constant
Ky = Activity equilibrium constant
Kp = Pressure equilibrium constant
Kc = Concentration equilibrium constant

Images

Kγ has units of [atm](d/a+c/aba1)=[atm]δ

Kp has units of [atm](d/a+c/aba1)=[atm]δ

For ideal gases Kγ = 1.0 atm

2. For the generic reaction (2-2), the pressure equilibrium constant KP is

Kp=PCc/aPDd/aPAPBb/aPi=partial pressure of speciesi,atm, kPa.Pi=CiRT(C-1)

3. For the generic reaction (2-2), the concentration equilibrium constant

Kc=CCc/aCDd/aCACBb/a(C-2)

It is important to be able to relate K, Kγ, Kc, and Kp.

4. For ideal gases, Kc and Kp are related by

Kp=Kc(RT)δ(C-3)

Where for the generic reaction (2-2),

δ=ca+daba1(C-4)

5. KP is a function of temperature only, and the temperature dependence of KP is given by van’t Hoff’s equation:

dlnkpdT=ΔHRx(T)RT2       (C-5)

Van’t Hoff’s equation

dlnKpdT=ΔHRx(TR)+ΔCP(TTR)RT2(C-6)

(http://www.umich.edu/~elements/5e/11chap/summary-biovan.html).

6. Integrating, we have

lnKp(T)Kp(T1)=ΔHRx(TR)TRΔCpR(1T11T)+ΔCpRlnTT1(C-7)

Kp and Kc are related by

Kc=Kp(RT)δ       (C-8)

when

δ=(da+caba1)=0

then

Kp=KC

7. Kp neglecting ΔCp. Given the equilibrium constant at one temperature, T1, KP (Ti), and the heat of reaction, ΔHRx, the partial pressure equilibrium constant at any temperature T is

KP(T)=KP(T1)exp[ΔHRxo(TR)R(1T11T)]       (C-9)

8. From Le Châtelier’s principle we know that for exothermic reactions, the equilibrium shifts to the left (i.e., K and Xe decrease) as the temperature increases. Figures C-1 and C-2 show how the equilibrium constant varies with temperature for an exothermic reaction and for an endothermic reaction, respectively.

Graph shows a horizontal axis labeled T, a vertical axis labeled K, and a curve that extends rightward from a point on the vertical axis, slides, and extends rightward.

Figure C-1 Exothermic reaction.

Graph shows a horizontal axis labeled T, a vertical axis labeled K, and a curve that rises from a point on the vertical axis, extends rightward, rises, and extends rightward.

Figure C-2 Endothermic reaction.

Variation of equilibrium constant with temperature

9. The equilibrium constant for the reaction (2-2) at temperature T can be calculated from the change in the Gibbs free energy using

RTln[K(T)]=ΔGRx(T)(C-10)

ΔGRxo=caGCo+daGDobaGBoGAo       (C-11)

10. Tables that list the standard Gibbs free energy of formation of a given species Gi are available in the literature (webbook.nist.gov).

11. The relationship between the change in Gibbs free energy and enthalpy, H, and entropy, S, is

ΔG=ΔHTΔS(C-12)

See bilbo.chm.uri.edu/CHM112/lectures/lecture31.htm. An example on how to calculate the equivalent conversion for AG is given on the Web site.

Example C-1 Water-Gas Shift Reaction

The water-gas shift reaction to produce hydrogen

H2O+COCO2+H2

is to be carried out at 1000 K and 10 atm. For an equimolar mixture of water and carbon monoxide, calculate the equilibrium conversion and concentration of each species.

Data: At 1000 K and 10 atm, the Gibbs free energies of formation are GCO=47,860cal/mol;GCO2=94,630cal/mol;GH2O=46,040cal/mol; andGH2=0.

Solution

We first calculate the equilibrium constant. The first step in calculating K is to calculate the change in Gibbs free energy for the reaction. Applying Equation (C-10) gives us

ΔGRx=GH2+GCO2GCOGH2O                                                    (EC-1.1)=0+(94,630)(47,860)(46,040)=730cal/molRTlnK=ΔGRx(T)                                                                                     (C-10)lnK=ΔGRx(T)RT=(730cal/mol)1.987cal.molK(1000K)                                                (EC-1.2)=0.367

then

K=1.44

Expressing the equilibrium constant first in terms of activities and then finally in terms of concentration, we have

K=aCO2aH2aCOaH2O=fCO2fH2fCOfH2O=γCO2PCO2γH2PH2γCOPCOγH2OPH2O(EC-1.3)

where ai is the activity, fi is the fugacity, γi is the activity coefficient (which we shall take to be 1.0 owing to high temperature and low pressure), and γi is the mole fraction of species i.2 Substituting for the mole fractions in terms of partial pressures gives

K=PCO2PH2PCOPH2O(EC-1.4)

Pi=CiRT(EC-1.5)

K=CCO2CH2OCCOCH2O(EC-1.6)

Calculate ΔGRx

Calculate K

In terms of conversion for an equimolar feed, we have

K=CCO,0XeCCO,0XeCCO,0(1Xe)CCO,0(1Xe)(EC-1.7)

=X2(1Xe)=1.44(EC-1.8)

Graph shows the relationship between temperature in degrees kelvin and (log subscript 10) (K subscript P).

Figure EC-1.1 Modell, Michael, and Reid, Robert, Thermodynamics and Its Applications, 2nd ed., © 1983. Reprinted and electronically reproduced by permission of Pearson Education, Inc., Upper Saddle River, NJ.

Relate K and Xe

From Figure EC-1.1 we read at 1000 K that log KP = 0.15; therefore, KP = 1.41, which is close to the calculated value. We note that there is no net change in the number of moles for this reaction (i.e., δ = 0); therefore,

K = Kp = Kc (dimensionless)

Taking the square root of Equation (EC-1.8) yields

Xe1Xe=(1.44)1/2=1.2(EC-1.9)

Solving for Xe , we obtain

X,1.22.2=0.55

Then

Images

Figure EC-1.1 gives the equilibrium constant as a function of temperature for a number of reactions. Reactions in which the lines increase from left to right are exothermic.

The following links give thermochemical data. (Heats of Formation, CP, etc.)

1) www.uic.edu/~mansoori/Thermodynamic.Data.and.Propertyjhtml

2) webbook.nist.gov

Also see Chem. Tech., 28 (3) (March), 19 (1998).

Calculate Xe, the equilibrium conversion

Calculate CCO,e, the equilibrium conversion of CO

Images

Links

1 For the limitations and for further explanation of these relationships, see, for example, K. Denbigh, The Principles of Chemical Equilibrium, 3rd ed. (Cambridge: Cambridge University Press, 1971), p. 138.

2 See Chapter 17 in J. R. Elliott and C. T. Lira, Introductory Chemical Engineering Thermodynamics, 2nd ed. (Upper Saddle River, NJ: Prentice Hall, 2012), and Chapter 16 in J. W. Tester and M. Modell, Thermodynamics and Its Applications, 3rd ed. (Upper Saddle River, NJ: Prentice Hall, 1997).

..................Content has been hidden....................

You can't read the all page of ebook, please click here login for view all page.
Reset
3.138.122.195