An isolated system is in mechanical equilibrium if no changes occur in pressure, in thermal equilibrium if no changes occur in temperature, in phase equilibrium if no transformations occ
Trang 1Chapter 16
CHEMICAL AND PHASE EQUILIBRIUM
In Chapter 15 we analyzed combustion processes under
the assumption that combustion is complete when there is
sufficient time and oxygen Often this is not the case,
however A chemical reaction may reach a state of
equilib-rium before reaching completion even when there is sufficient
time and oxygen.
A system is said to be in equilibrium if no changes occur
within the system when it is isolated from its surroundings.
An isolated system is in mechanical equilibrium if no changes
occur in pressure, in thermal equilibrium if no changes occur
in temperature, in phase equilibrium if no transformations
occur from one phase to another, and in chemical
equilib-rium if no changes occur in the chemical composition of the
system The conditions of mechanical and thermal
equilib-rium are straightforward, but the conditions of chemical and
phase equilibrium can be rather involved.
The equilibrium criterion for reacting systems is based on
the second law of thermodynamics; more specifically, the
increase of entropy principle For adiabatic systems, chemical
equilibrium is established when the entropy of the reacting
system reaches a maximum Most reacting systems
encoun-tered in practice are not adiabatic, however Therefore, we
need to develop an equilibrium criterion applicable to any
reacting system.
In this chapter, we develop a general criterion for chemical
equilibrium and apply it to reacting ideal-gas mixtures We
then extend the analysis to simultaneous reactions Finally,
we discuss phase equilibrium for nonreacting systems.
Objectives
The objectives of Chapter 16 are to:
• Develop the equilibrium criterion for reacting systems based
on the second law of thermodynamics.
• Develop a general criterion for chemical equilibrium applicable to any reacting system based on minimizing the Gibbs function for the system.
• Define and evaluate the chemical equilibrium constant.
• Apply the general criterion for chemical equilibrium analysis
to reacting ideal-gas mixtures.
• Apply the general criterion for chemical equilibrium analysis
• Apply the Gibbs phase rule to determine the number of independent variables associated with a multicomponent, multiphase system.
• Apply Henry’s law and Raoult’s law for gases dissolved in liquids.
Trang 216–1 ■ CRITERION FOR CHEMICAL EQUILIBRIUM
Consider a reaction chamber that contains a mixture of CO, O2, and CO2 at
a specified temperature and pressure Let us try to predict what will happen
in this chamber (Fig 16–1) Probably the first thing that comes to mind is achemical reaction between CO and O2to form more CO2:
This reaction is certainly a possibility, but it is not the only possibility It isalso possible that some CO2in the combustion chamber dissociated into COand O2 Yet a third possibility would be to have no reactions among thethree components at all, that is, for the system to be in chemical equi-librium It appears that although we know the temperature, pressure, andcomposition (thus the state) of the system, we are unable to predict whetherthe system is in chemical equilibrium In this chapter we develop the neces-sary tools to correct this
Assume that the CO, O2, and CO2mixture mentioned above is in chemicalequilibrium at the specified temperature and pressure The chemical compo-sition of this mixture does not change unless the temperature or the pressure
of the mixture is changed That is, a reacting mixture, in general, has ent equilibrium compositions at different pressures and temperatures There-fore, when developing a general criterion for chemical equilibrium, weconsider a reacting system at a fixed temperature and pressure
differ-Taking the positive direction of heat transfer to be to the system, theincrease of entropy principle for a reacting or nonreacting system wasexpressed in Chapter 7 as
(16–1)
A system and its surroundings form an adiabatic system, and for such systems
Eq 16–1 reduces to dSsys 0 That is, a chemical reaction in an adiabaticchamber proceeds in the direction of increasing entropy When the entropyreaches a maximum, the reaction stops (Fig 16–2) Therefore, entropy is avery useful property in the analysis of reacting adiabatic systems
When a reacting system involves heat transfer, the increase of entropyprinciple relation (Eq 16–1) becomes impractical to use, however, since itrequires a knowledge of heat transfer between the system and its surround-ings A more practical approach would be to develop a relation for theequilibrium criterion in terms of the properties of the reacting system only.Such a relation is developed below
Consider a reacting (or nonreacting) simple compressible system of fixed
mass with only quasi-equilibrium work modes at a specified temperature T and pressure P (Fig 16–3) Combining the first- and the second-law
relations for this system gives
FIGURE 16–1
A reaction chamber that contains a
mixture of CO2, CO, and O2at a
specified temperature and pressure
100%
products
Violation of second law
S
Equilibrium composition
Equilibrium criteria for a chemical
reaction that takes place adiabatically
mass
T, P Q
FIGURE 16–3
A control mass undergoing a chemical
reaction at a specified temperature and
pressure
Trang 3The differential of the Gibbs function (G H TS) at constant
tempera-ture and pressure is
(16–3)
From Eqs 16–2 and 16–3, we have (dG) T,P 0 Therefore, a chemical
reac-tion at a specified temperature and pressure proceeds in the direcreac-tion of a
decreasing Gibbs function The reaction stops and chemical equilibrium is
established when the Gibbs function attains a minimum value (Fig 16–4)
Therefore, the criterion for chemical equilibrium can be expressed as
(16–4)
A chemical reaction at a specified temperature and pressure cannot proceed
in the direction of the increasing Gibbs function since this will be a
viola-tion of the second law of thermodynamics Notice that if the temperature or
the pressure is changed, the reacting system will assume a different
equilib-rium state, which is the state of the minimum Gibbs function at the new
temperature or pressure
To obtain a relation for chemical equilibrium in terms of the properties of
the individual components, consider a mixture of four chemical components
A, B, C, and D that exist in equilibrium at a specified temperature and
pres-sure Let the number of moles of the respective components be N A , N B , N C,
and N D Now consider a reaction that occurs to an infinitesimal extent
during which differential amounts of A and B (reactants) are converted to C
and D (products) while the temperature and the pressure remain constant
(Fig 16–5):
The equilibrium criterion (Eq 16–4) requires that the change in the Gibbs
function of the mixture during this process be equal to zero That is,
(16–5)
or
(16–6)
where the g – ’s are the molar Gibbs functions (also called the chemical
poten-tials) at the specified temperature and pressure and the dN’s are the
differen-tial changes in the number of moles of the components
To find a relation between the dN’s, we write the corresponding
stoichio-metric (theoretical) reaction
(16–7)
where the n’s are the stoichiometric coefficients, which are evaluated easily
once the reaction is specified The stoichiometric reaction plays an
impor-tant role in the determination of the equilibrium composition of the reacting
100% products
Violation of second law
G
Equilibrium composition
REACTION CHAMBER
An infinitesimal reaction in a chamber
at constant temperature and pressure
Trang 4mixtures because the changes in the number of moles of the components areproportional to the stoichiometric coefficients (Fig 16–6) That is,
(16–8)
where e is the proportionality constant and represents the extent of a tion A minus sign is added to the first two terms because the number of
reac-moles of the reactants A and B decreases as the reaction progresses.
For example, if the reactants are C2H6 and O2 and the products are CO2and H2O, the reaction of 1 mmol (106 mol) of C2H6 results in a 2-mmolincrease in CO2, a 3-mmol increase in H2O, and a 3.5-mmol decrease in O2
in accordance with the stoichiometric equation
That is, the change in the number of moles of a component is one-millionth(e 106) of the stoichiometric coefficient of that component in this case.Substituting the relations in Eq 16–8 into Eq 16–6 and canceling e, weobtain
(16–9)
This equation involves the stoichiometric coefficients and the molar Gibbs
functions of the reactants and the products, and it is known as the criterion for chemical equilibrium It is valid for any chemical reaction regardless
of the phases involved
Equation 16–9 is developed for a chemical reaction that involves tworeactants and two products for simplicity, but it can easily be modified tohandle chemical reactions with any number of reactants and products Next
we analyze the equilibrium criterion for ideal-gas mixtures
FOR IDEAL-GAS MIXTURES
Consider a mixture of ideal gases that exists in equilibrium at a specifiedtemperature and pressure Like entropy, the Gibbs function of an ideal gasdepends on both the temperature and the pressure The Gibbs function val-
ues are usually listed versus temperature at a fixed reference pressure P0,which is taken to be 1 atm The variation of the Gibbs function of an idealgas with pressure at a fixed temperature is determined by using the defini-tion of the Gibbs function and the entropy-change relation
Thus the Gibbs function of component i of an ideal-gas mixture at its partial pressure P i and mixture temperature T can be expressed as
n
FIGURE 16–6
The changes in the number of moles
of the components during a chemical
reaction are proportional to the
stoichiometric coefficients regardless
of the extent of the reaction
→0
Trang 5where g – i * (T ) represents the Gibbs function of component i at 1 atm
pres-sure and temperature T, and P irepresents the partial pressure of component
i in atmospheres Substituting the Gibbs function expression for each
com-ponent into Eq 16–9, we obtain
For convenience, we define the standard-state Gibbs function change as
Therefore, the equilibrium constant K Pof an ideal-gas mixture at a specified
temperature can be determined from a knowledge of the standard-state
Gibbs function change at the same temperature The K P values for several
reactions are given in Table A–28
Once the equilibrium constant is available, it can be used to determine the
equilibrium composition of reacting ideal-gas mixtures This is
accom-plished by expressing the partial pressures of the components in terms of
their mole fractions:
where P is the total pressure and Ntotalis the total number of moles present
in the reaction chamber, including any inert gases Replacing the partial
pressures in Eq 16–13 by the above relation and rearranging, we obtain
(Fig 16–7)
(16–15)
where
Equation 16–15 is written for a reaction involving two reactants and two
products, but it can be extended to reactions involving any number of
reac-tants and products
Trang 6EXAMPLE 16–1 Equilibrium Constant of a Dissociation Process
Using Eq 16–14 and the Gibbs function data, determine the equilibrium
constant K P for the dissociation process N2 → 2N at 25°C Compare your
result to the K Pvalue listed in Table A–28.
Solution The equilibrium constant of the reaction N2 → 2N is listed in Table A–28 at different temperatures It is to be verified using Gibbs func- tion data.
Assumptions 1 The constituents of the mixture are ideal gases 2 The
equi-librium mixture consists of N2and N only.
Properties The equilibrium constant of this reaction at 298 K is ln K P
367.5 (Table A–28) The Gibbs function of formation at 25°C and 1 atm is
O for N2and 455,510 kJ/kmol for N (Table A–26).
Analysis In the absence of K P tables, K Pcan be determined from the Gibbs function data and Eq 16–14,
where, from Eq 16–11,
Substituting, we find
or
The calculated K Pvalue is in agreement with the value listed in Table A–28.
The K Pvalue for this reaction is practically zero, indicating that this reaction will not occur at this temperature.
Discussion Note that this reaction involves one product (N) and one reactant (N2), and the stoichiometric coefficients for this reaction are nN 2 and
nN
2 1 Also note that the Gibbs function of all stable elements (such as N 2 )
is assigned a value of zero at the standard reference state of 25°C and 1 atm The Gibbs function values at other temperatures can be calculated from the enthalpy and absolute entropy data by using the definition of the Gibbs func- tion, , g * 1T 2 h1T 2 T s*1T 2 where h 1T 2 h* f h T h298 K
Determine the temperature at which 10 percent of diatomic hydrogen (H2) dissociates into monatomic hydrogen (H) at a pressure of 10 atm.
Solution The temperature at which 10 percent of H2dissociates into 2H is
to be determined.
Assumptions 1 The constituents of the mixture are ideal gases 2 The
equi-librium mixture consists of H2and H only.
Trang 7A double arrow is used in equilibrium equations as an indication that a
chemical reaction does not stop when chemical equilibrium is established;
rather, it proceeds in both directions at the same rate That is, at equilibrium,
the reactants are depleted at exactly the same rate as they are replenished
from the products by the reverse reaction
OF IDEAL-GAS MIXTURES
In the last section we developed three equivalent expressions for the
equilib-rium constant K Pof reacting ideal-gas mixtures: Eq 16–13, which expresses
K P in terms of partial pressures; Eq 16–14, which expresses K Pin terms of
the standard-state Gibbs function change ∆G*(T); and Eq 16–15, which
expresses K P in terms of the number of moles of the components All three
relations are equivalent, but sometimes one is more convenient to use than
the others For example, Eq 16–15 is best suited for determining the
equi-librium composition of a reacting ideal-gas mixture at a specified
tem-perature and pressure On the basis of these relations, we may draw the
following conclusions about the equilibrium constant K P of ideal-gas
mixtures:
1 The K P of a reaction depends on temperature only It is independent of
the pressure of the equilibrium mixture and is not affected by the presence
of inert gases This is because K P depends on ∆G*(T), which depends on
Analysis This is a dissociation process that is significant at very high
tem-peratures only For simplicity we consider 1 kmol of H2, as shown in Fig.
16–8 The stoichiometric and actual reactions in this case are as follows:
Stoichiometric:
Actual:
reactants products (leftover)
A double-headed arrow is used for the stoichiometric reaction to differentiate
it from the actual reaction This reaction involves one reactant (H2) and one
product (H) The equilibrium composition consists of 0.9 kmol of H2 (the
leftover reactant) and 0.2 kmol of H (the newly formed product) Therefore,
NH2 0.9 and NH 0.2 and the equilibrium constant KP is determined
from Eq 16–15 to be
From Table A–28, the temperature corresponding to this K Pvalue is
Discussion We conclude that 10 percent of H2dissociates into H when the
temperature is raised to 3535 K If the temperature is increased further, the
percentage of H2that dissociates into H will also increase.
0.9H20.2H
Equilibrium composition
FIGURE 16–8
Schematic for Example 16–2
Trang 8temperature only, and the ∆G*(T) of inert gases is zero (see Eq 16–14).
Thus, at a specified temperature the following four reactions have the same
2 The K P of the reverse reaction is 1/K P This is easily seen from Eq.
16–13 For reverse reactions, the products and reactants switch places, andthus the terms in the numerator move to the denominator and vice versa.Consequently, the equilibrium constant of the reverse reaction becomes
1/K P For example, from Table A–28,
3 The larger the K P , the more complete the reaction This is also apparent
from Fig 16–9 and Eq 16–13 If the equilibrium composition consists
largely of product gases, the partial pressures of the products (P C and P D)
are considerably larger than the partial pressures of the reactants (P A and
P B ), which results in a large value of K P In the limiting case of a complete
reaction (no leftover reactants in the equilibrium mixture), K P approaches
infinity Conversely, very small values of K P indicate that a reaction does
not proceed to any appreciable degree Thus reactions with very small K P
values at a specified temperature can be neglected
A reaction with K P 1000 (or ln K P 7) is usually assumed to proceed
to completion, and a reaction with K P 0.001 (or ln K P 7) is assumed
not to occur at all For example, ln K P 6.8 for the reaction N2∆ 2N
at 5000 K Therefore, the dissociation of N2 into monatomic nitrogen (N)can be disregarded at temperatures below 5000 K
4 The mixture pressure affects the equilibrium composition (although it does not affect the equilibrium constant K P) This can be seen from
Eq 16–15, which involves the term P∆n, where ∆n nP nR(the ference between the number of moles of products and the number of moles
dif-of reactants in the stoichiometric reaction) At a specified temperature, the
K Pvalue of the reaction, and thus the right-hand side of Eq 16–15, remainsconstant Therefore, the mole numbers of the reactants and the productsmust change to counteract any changes in the pressure term The direction
of the change depends on the sign of ∆n An increase in pressure at a fied temperature increases the number of moles of the reactants anddecreases the number of moles of products if ∆n is positive, have the oppo-site effect if ∆n is negative, and have no effect if ∆n is zero
speci-5 The presence of inert gases affects the equilibrium composition (although
it does not affect the equilibrium constant K P) This can be seen from Eq
16–15, which involves the term (1/Ntotal)∆n, where Ntotalis the total number
of moles of the ideal-gas mixture at equilibrium, including inert gases The
sign of ∆n determines how the presence of inert gases influences the librium composition (Fig 16–10) An increase in the number of moles ofinert gases at a specified temperature and pressure decreases the number of
267.7
76.80 97.70
0.00 0.16 14.63
K P = 0.0251 1.240 mol H 0.380 mol H2
1 mol N2
FIGURE 16–10
The presence of inert gases does not
affect the equilibrium constant, but it
does affect the equilibrium
composition
Trang 9moles of the reactants and increases the number of moles of products if ∆n
is positive, have the opposite effect if ∆n is negative, and have no effect if
∆n is zero
6 When the stoichiometric coefficients are doubled, the value of K P is
squared Therefore, when one is using K Pvalues from a table, the
stoichio-metric coefficients (the n’s) used in a reaction must be exactly the same
ones appearing in the table from which the K Pvalues are selected
Multiply-ing all the coefficients of a stoichiometric equation does not affect the mass
balance, but it does affect the equilibrium constant calculations since the
stoichiometric coefficients appear as exponents of partial pressures in
Eq 16–13 For example,
For
But for
7 Free electrons in the equilibrium composition can be treated as an ideal
gas At high temperatures (usually above 2500 K), gas molecules start to
dissociate into unattached atoms (such as H2 ∆ 2H), and at even higher
temperatures atoms start to lose electrons and ionize, for example,
(16–16)
The dissociation and ionization effects are more pronounced at low
pres-sures Ionization occurs to an appreciable extent only at very high
tempera-tures, and the mixture of electrons, ions, and neutral atoms can be treated as
an ideal gas Therefore, the equilibrium composition of ionized gas mixtures
can be determined from Eq 16–15 (Fig 16–11) This treatment may not be
adequate in the presence of strong electric fields, however, since the
elec-trons may be at a different temperature than the ions in this case
8 Equilibrium calculations provide information on the equilibrium
compo-sition of a reaction, not on the reaction rate Sometimes it may even take
years to achieve the indicated equilibrium composition For example, the
equilibrium constant of the reaction at 298 K is about
1040, which suggests that a stoichiometric mixture of H2 and O2 at room
temperature should react to form H2O, and the reaction should go to
com-pletion However, the rate of this reaction is so slow that it practically does
not occur But when the right catalyst is used, the reaction goes to
comple-tion rather quickly to the predicted value
A mixture of 2 kmol of CO and 3 kmol of O2is heated to 2600 K at a
pres-sure of 304 kPa Determine the equilibrium composition, assuming the
mix-ture consists of CO2, CO, and O2(Fig 16–12).
Solution A reactive gas mixture is heated to a high temperature The
equi-librium composition at that temperature is to be determined.
2 kmol CO
Initial composition
x CO2
Equilibrium composition at
n n
Trang 10Assumptions 1 The equilibrium composition consists of CO2, CO, and O2.
2 The constituents of the mixture are ideal gases.
Analysis The stoichiometric and actual reactions in this case are as follows:
The closest reaction listed in Table A–28 is CO2∆ CO – 12O2, for which
ln K P 2.801 at 2600 K The reaction we have is the inverse of this, and
thus ln K P 2.801, or KP 16.461 in our case.
Assuming ideal-gas behavior for all components, the equilibrium constant relation (Eq 16–15) becomes
We will do so in the next section.)
1.906CO 2 0.094CO 2.074O 2
z 3 x2 2.047
y 2 x 0.094
x 1.90616.461 12 x2 13 x>22 x 1 >2 a5 x>2 b3 1>2
Trang 11EXAMPLE 16–4 Effect of Inert Gases on Equilibrium
Composition
A mixture of 3 kmol of CO, 2.5 kmol of O2, and 8 kmol of N2 is heated to
2600 K at a pressure of 5 atm Determine the equilibrium composition of
the mixture (Fig 16–13).
Solution A gas mixture is heated to a high temperature The equilibrium
composition at the specified temperature is to be determined.
Assumptions 1 The equilibrium composition consists of CO2, CO, O2, and
N2 2 The constituents of the mixture are ideal gases.
Analysis This problem is similar to Example 16–3, except that it involves
an inert gas N2 At 2600 K, some possible reactions are O2∆2O (ln K P
7.521), N 2∆ 2N (ln K P 28.304), – 12O2 – 12N2∆NO (ln K P
2.671), and CO 1 –2O2∆ CO2(ln K P 2.801 or KP 16.461) Based
on these K Pvalues, we conclude that the O2 and N2will not dissociate to
any appreciable degree, but a small amount will combine to form some
oxides of nitrogen (We disregard the oxides of nitrogen in this example, but
they should be considered in a more refined analysis.) We also conclude that
most of the CO will combine with O2 to form CO2 Notice that despite the
changes in pressure, the number of moles of CO and O2and the presence of
an inert gas, the K Pvalue of the reaction is the same as that used in
Total number of moles:
Assuming ideal-gas behavior for all components, the equilibrium constant relation (Eq 16–15) becomes
x CO2
Equilibrium composition at
2600 K, 5 atm
y CO
z O2
8 kmol N22.5 kmol O2
8 N2
FIGURE 16–13
Schematic for Example 16–4
Trang 1216–4 ■ CHEMICAL EQUILIBRIUM
FOR SIMULTANEOUS REACTIONS
The reacting mixtures we have considered so far involved only one reaction,
and writing a K P relation for that reaction was sufficient to determine theequilibrium composition of the mixture However, most practical chemicalreactions involve two or more reactions that occur simultaneously, whichmakes them more difficult to deal with In such cases, it becomes necessary
to apply the equilibrium criterion to all possible reactions that may occur inthe reaction chamber When a chemical species appears in more than onereaction, the application of the equilibrium criterion, together with the massbalance for each chemical species, results in a system of simultaneous equa-tions from which the equilibrium composition can be determined
We have shown earlier that a reacting system at a specified temperatureand pressure achieves chemical equilibrium when its Gibbs function reaches
a minimum value, that is, (dG) T,P 0 This is true regardless of the number
of reactions that may be occurring When two or more reactions are
involved, this condition is satisfied only when (dG) T,P 0 for each reaction
Assuming ideal-gas behavior, the K P of each reaction can be determined
from Eq 16–15, with Ntotal being the total number of moles present in theequilibrium mixture
The determination of the equilibrium composition of a reacting mixturerequires that we have as many equations as unknowns, where the unknownsare the number of moles of each chemical species present in the equilibriummixture The mass balance of each element involved provides one equation
The rest of the equations must come from the K P relations written for each
reaction Thus we conclude that the number of K P relations needed to mine the equilibrium composition of a reacting mixture is equal to the number of chemical species minus the number of elements present in equi- librium For an equilibrium mixture that consists of CO2, CO, O2, and O,
deter-for example, two K P relations are needed to determine the equilibriumcomposition since it involves four chemical species and two elements(Fig 16–14)
The determination of the equilibrium composition of a reacting mixture inthe presence of two simultaneous reactions is here with an example
Then
Therefore, the equilibrium composition of the mixture at 2600 K and 5 atm is
Discussion Note that the inert gases do not affect the K P value or the K P
relation for a reaction, but they do affect the equilibrium composition.
2.754CO 2 0.246CO 1.123O 2 8N 2
The number of K Prelations needed to
determine the equilibrium composition
of a reacting mixture is the difference
between the number of species and the
number of elements
Trang 13EXAMPLE 16–5 Equilibrium Composition
for Simultaneous Reactions
A mixture of 1 kmol of H2O and 2 kmol of O2is heated to 4000 K at a
pres-sure of 1 atm Determine the equilibrium composition of this mixture,
assuming that only H2O, OH, O2, and H2are present (Fig 16–15).
Solution A gas mixture is heated to a specified temperature at a specified
pressure The equilibrium composition is to be determined.
Assumptions 1 The equilibrium composition consists of H2O, OH, O2, and
H2 2 The constituents of the mixture are ideal gases.
Analysis The chemical reaction during this process can be expressed as
Mass balances for hydrogen and oxygen yield
The mass balances provide us with only two equations with four unknowns,
and thus we need to have two more equations (to be obtained from the K P
relations) to determine the equilibrium composition of the mixture It
appears that part of the H2O in the products is dissociated into H2and OH
during this process, according to the stoichiometric reactions
The equilibrium constants for these two reactions at 4000 K are determined
from Table A–28 to be
The K Prelations for these two simultaneous reactions are
x H2O
Equilibrium composition at
Trang 14Solving a system of simultaneous nonlinear equations is extremely tediousand time-consuming if it is done by hand Thus it is often necessary to solvethese kinds of problems by using an equation solver such as EES.
It was shown in Section 16–2 that the equilibrium constant K P of an idealgas depends on temperature only, and it is related to the standard-stateGibbs function change ∆G*(T) through the relation (Eq 16–14)
In this section we develop a relation for the variation of K Pwith temperature
in terms of other properties
Substituting ∆G*(T) ∆H*(T) T ∆S*(T) into the above relation and
differentiating with respect to temperature, we get
At constant pressure, the second T ds relation, T ds dh v dP, reduces to
T ds dh Also, T d(∆S*) d(∆H*) since ∆S* and ∆H* consist of entropy
and enthalpy terms of the reactants and the products Therefore, the last twoterms in the above relation cancel, and it reduces to
(16–17)
where is the enthalpy of reaction at temperature T Notice that we
dropped the superscript * (which indicates a constant pressure of 1 atm)from ∆H(T), since the enthalpy of an ideal gas depends on temperature only
and is independent of pressure Equation 16–17 is an expression of the
vari-ation of K Pwith temperature in terms of , and it is known as the van’t Hoff equation To integrate it, we need to know how varies with T For
small temperature intervals, can be treated as a constant and Eq 16–17can be integrated to yield
Trang 15This equation has two important implications First, it provides a means of
calculating the of a reaction from a knowledge of K P, which is easier to
determine Second, it shows that exothermic reactions such as
combustion processes are less complete at higher temperatures since K P
decreases with temperature for such reactions (Fig 16–16)
1h R 6 02
h R
of a Combustion Process
Estimate the enthalpy of reaction for the combustion process of hydrogen
H2+ 0.5O2→ H 2O at 2000 K, using (a) enthalpy data and (b) K Pdata.
Solution The at a specified temperature is to be determined using the
enthalpy and K pdata.
Assumptions Both the reactants and the products are ideal gases.
Analysis (a) The of the combustion process of H2at 2000 K is the amount
of energy released as 1 kmol of H2 is burned in a steady-flow combustion
chamber at a temperature of 2000 K It can be determined from Eq 15–6,
Substituting yields
(b) The value at 2000 K can be estimated by using K P values at 1800
and 2200 K (the closest two temperatures to 2000 K for which K Pdata are
available) from Table A–28 They are KP
1 18,509 at T1 1800 K and
KP
2 869.6 at T2 2200 K By substituting these values into Eq 16–18, the value is determined to be
Discussion Despite the large temperature difference between T1 and T2
(400 K), the two results are almost identical The agreement between the
two results would be even better if a smaller temperature interval were used.
h R251,698 kJ/kmol
ln 869.618,509 8.314 kJhR>kmol # K a1800 K1 2200 K1 b
T, K K P
Reaction: C + O2 → CO 2
4.78 10 20 2.25 10 10 7.80 10 6 1.41 10 5
FIGURE 16–16
Exothermic reactions are lesscomplete at higher temperatures