Skip to main content
Chemistry LibreTexts

4.3: Gas Phase Equilibria and Heterogeneous Systems

  • Page ID
    364662
  • \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)

    \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash {#1}}} \)

    \( \newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\)

    ( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\)

    \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\)

    \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\)

    \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\)

    \( \newcommand{\Span}{\mathrm{span}}\)

    \( \newcommand{\id}{\mathrm{id}}\)

    \( \newcommand{\Span}{\mathrm{span}}\)

    \( \newcommand{\kernel}{\mathrm{null}\,}\)

    \( \newcommand{\range}{\mathrm{range}\,}\)

    \( \newcommand{\RealPart}{\mathrm{Re}}\)

    \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\)

    \( \newcommand{\Argument}{\mathrm{Arg}}\)

    \( \newcommand{\norm}[1]{\| #1 \|}\)

    \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\)

    \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\AA}{\unicode[.8,0]{x212B}}\)

    \( \newcommand{\vectorA}[1]{\vec{#1}}      % arrow\)

    \( \newcommand{\vectorAt}[1]{\vec{\text{#1}}}      % arrow\)

    \( \newcommand{\vectorB}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)

    \( \newcommand{\vectorC}[1]{\textbf{#1}} \)

    \( \newcommand{\vectorD}[1]{\overrightarrow{#1}} \)

    \( \newcommand{\vectorDt}[1]{\overrightarrow{\text{#1}}} \)

    \( \newcommand{\vectE}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{\mathbf {#1}}}} \)

    \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)

    \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash {#1}}} \)

    \(\newcommand{\avec}{\mathbf a}\) \(\newcommand{\bvec}{\mathbf b}\) \(\newcommand{\cvec}{\mathbf c}\) \(\newcommand{\dvec}{\mathbf d}\) \(\newcommand{\dtil}{\widetilde{\mathbf d}}\) \(\newcommand{\evec}{\mathbf e}\) \(\newcommand{\fvec}{\mathbf f}\) \(\newcommand{\nvec}{\mathbf n}\) \(\newcommand{\pvec}{\mathbf p}\) \(\newcommand{\qvec}{\mathbf q}\) \(\newcommand{\svec}{\mathbf s}\) \(\newcommand{\tvec}{\mathbf t}\) \(\newcommand{\uvec}{\mathbf u}\) \(\newcommand{\vvec}{\mathbf v}\) \(\newcommand{\wvec}{\mathbf w}\) \(\newcommand{\xvec}{\mathbf x}\) \(\newcommand{\yvec}{\mathbf y}\) \(\newcommand{\zvec}{\mathbf z}\) \(\newcommand{\rvec}{\mathbf r}\) \(\newcommand{\mvec}{\mathbf m}\) \(\newcommand{\zerovec}{\mathbf 0}\) \(\newcommand{\onevec}{\mathbf 1}\) \(\newcommand{\real}{\mathbb R}\) \(\newcommand{\twovec}[2]{\left[\begin{array}{r}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\ctwovec}[2]{\left[\begin{array}{c}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\threevec}[3]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\cthreevec}[3]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\fourvec}[4]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\cfourvec}[4]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\fivevec}[5]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\cfivevec}[5]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\mattwo}[4]{\left[\begin{array}{rr}#1 \amp #2 \\ #3 \amp #4 \\ \end{array}\right]}\) \(\newcommand{\laspan}[1]{\text{Span}\{#1\}}\) \(\newcommand{\bcal}{\cal B}\) \(\newcommand{\ccal}{\cal C}\) \(\newcommand{\scal}{\cal S}\) \(\newcommand{\wcal}{\cal W}\) \(\newcommand{\ecal}{\cal E}\) \(\newcommand{\coords}[2]{\left\{#1\right\}_{#2}}\) \(\newcommand{\gray}[1]{\color{gray}{#1}}\) \(\newcommand{\lgray}[1]{\color{lightgray}{#1}}\) \(\newcommand{\rank}{\operatorname{rank}}\) \(\newcommand{\row}{\text{Row}}\) \(\newcommand{\col}{\text{Col}}\) \(\renewcommand{\row}{\text{Row}}\) \(\newcommand{\nul}{\text{Nul}}\) \(\newcommand{\var}{\text{Var}}\) \(\newcommand{\corr}{\text{corr}}\) \(\newcommand{\len}[1]{\left|#1\right|}\) \(\newcommand{\bbar}{\overline{\bvec}}\) \(\newcommand{\bhat}{\widehat{\bvec}}\) \(\newcommand{\bperp}{\bvec^\perp}\) \(\newcommand{\xhat}{\widehat{\xvec}}\) \(\newcommand{\vhat}{\widehat{\vvec}}\) \(\newcommand{\uhat}{\widehat{\uvec}}\) \(\newcommand{\what}{\widehat{\wvec}}\) \(\newcommand{\Sighat}{\widehat{\Sigma}}\) \(\newcommand{\lt}{<}\) \(\newcommand{\gt}{>}\) \(\newcommand{\amp}{&}\) \(\definecolor{fillinmathshade}{gray}{0.9}\)
    Learning Objectives
    • To know the relationship between the equilibrium constant and the rate constants for the forward and reverse reactions.
    • To write an equilibrium constant expression for any reaction.

    Whenever gases are involved in a reaction, the partial pressure of each gas can be used instead of its concentration in the equation for the reaction quotient because the partial pressure of a gas is directly proportional to its concentration at constant temperature.

    Equilibrium Constant Expressions for Systems that Contain Gases

    For reactions that involve species in solution, the concentrations used in equilibrium calculations are usually expressed in moles/liter. For gases, however, the concentrations are usually expressed in terms of partial pressures rather than molarity, where the standard state is 1 atm of pressure. The symbol \(K_p\) is used to denote equilibrium constants calculated from partial pressures. For the general reaction \(aA+bB \rightleftharpoons cC+dD\), in which all the components are gases, the equilibrium constant expression can be written as the ratio of the partial pressures of the products and reactants (each raised to its coefficient in the chemical equation):

    \[K_p=\dfrac{(P_C)^c(P_D)^d}{(P_A)^a(P_B)^b} \label{Eq16}\]

    Thus \(K_p\) for the decomposition of \(N_2O_4\) (Equation 15.1) is as follows:

    \[K_p=\dfrac{(P_{NO_2})^2}{P_{N_2O_4}} \label{Eq17}\]

    Like \(K\), \(K_p\) is a unitless quantity because the quantity that is actually used to calculate it is an “effective pressure,” the ratio of the measured pressure to a standard state of 1 bar (approximately 1 atm), which produces a unitless quantity. The “effective pressure” is called the fugacity, just as activity is the effective concentration.

    This relationship between KC and KP can be derived from the ideal gas equation, where M is the molar concentration of gas, \(\dfrac{n}{V}\).

    \[\begin{align} PV&=nRT \label{13.3.16} \\[4pt] P &=\left(\dfrac{n}{V}\right)RT \label{13.3.17} \\[4pt] &=MRT \label{13.3.18} \end{align}\]

    Thus, at constant temperature, the pressure of a gas is directly proportional to its concentration. Using the partial pressures of the gases, we can write the reaction quotient for the system

    \[\ce{C2H6}(g) \rightleftharpoons \ce{C2H4}(g)+\ce{H2}(g) \label{13.3.19}\]

    by following the same guidelines for deriving concentration-based expressions:

    \[Q_P=\dfrac{P_{\ce{C2H4}}P_{\ce{H2}}}{P_{\ce{C2H6}}} \label{13.3.20}\]

    In this equation we use QP to indicate a reaction quotient written with partial pressures: \(P_{\ce{C2H6}}\) is the partial pressure of C2H6; \(P_{\ce{H2}}\), the partial pressure of H2; and \(P_{\ce{C2H6}}\), the partial pressure of C2H4. At equilibrium:

    \[K_P=Q_P=\dfrac{P_{\ce{C2H4}}P_{\ce{H2}}}{P_{\ce{C2H6}}} \label{13.3.21}\]

    The subscript \(P\) in the symbol \(K_P\) designates an equilibrium constant derived using partial pressures instead of concentrations. The equilibrium constant, KP, is still a constant, but its numeric value may differ from the equilibrium constant found for the same reaction by using concentrations.

    Conversion between a value for \(K_c\), an equilibrium constant expressed in terms of concentrations, and a value for \(K_P\), an equilibrium constant expressed in terms of pressures, is straightforward (a K or Q without a subscript could be either concentration or pressure).

    The equation relating \(K_c\) and \(K_P\) is derived as follows. For the gas-phase reaction:

    \[m\ce{A}+n\ce{B} \rightleftharpoons x\ce{C}+y\ce{D} \label{13.3.22}\]

    with

    \[ \begin{align} K_P &=\dfrac{(P_C)^x(P_D)^y}{(P_A)^m(P_B)^n} \label{13.3.23} \\[4pt] &=\dfrac{([\ce C]×RT)^x([\ce D]×RT)^y}{([\ce A]×RT)^m([\ce B]×RT)^n} \label{13.3.24} \\[4pt] &=\dfrac{[\ce C]^x[\ce D]^y}{[\ce A]^m[\ce B]^n}×\dfrac{(RT)^{x+y}}{(RT)^{m+n}} \label{13.3.25} \\[4pt] &=K_c(RT)^{(x+y)−(m+n)} \label{13.3.26} \\[4pt] &=K_c(RT)^{Δn} \label{13.3.27} \end{align}\]

    The relationship between \(K_c\) and \(K_P\) is

    \[ \K_P=K_c(RT)^{Δn} \label{13.3.28}\]

    In this equation, Δn is the difference between the sum of the coefficients of the gaseous products and the sum of the coefficients of the gaseous reactants in the reaction (the change in moles of gas between the reactants and the products). For the gas-phase reaction \(m\ce{A}+n\ce{B} \rightleftharpoons x\ce{C}+y\ce{D}\), we have

    \[Δn=(x+y)−(m+n) \label{13.3.29}\]
    Example \(\PageIndex{1}\): Calculation of KP

    Write the equations for the conversion of \(K_c\) to KP for each of the following reactions:

    1. \(\ce{C2H6}(g) \rightleftharpoons \ce{C2H4}(g)+\ce{H2}(g)\)
    2. \(\ce{CO}(g)+\ce{H2O}(g) \rightleftharpoons \ce{CO2}(g)+\ce{H2}(g)\)
    3. \(\ce{N2}(g)+\ce{3H2}(g) \rightleftharpoons \ce{2NH3}(g)\)
    4. Kc is equal to 0.28 for the following reaction at 900 °C:

    \[\ce{CS2}(g)+\ce{4H2}(g) \rightleftharpoons \ce{CH4}(g)+\ce{2H2S}(g)\]

    What is KP at this temperature?

    Solution

    (a) Δn = (2) − (1) = 1

    KP = \(K_c\) (RT)Δn = \(K_c\) (RT)1 = \(K_c\) (RT)

    (b) Δn = (2) − (2) = 0

    KP = \(K_c\) (RT)Δn = \(K_c\) (RT)0 = Kc

    (c) Δn = (2) − (1 + 3) = −2

    KP = \(K_c\) (RT)Δn = \(K_c\) (RT)−2 = \(\dfrac{K_c}{(RT)^2}\)

    d) KP = \(K_c\) (RT)Δn = (0.28)[(0.0821)(1173)]−2 = 3.0 × 10−5

    Exercise \(\PageIndex{1}\)

    Write the equations for the conversion of \(K_c\) to KP for each of the following reactions, which occur in the gas phase:

    1. \(\ce{2SO2}(g)+\ce{O2}(g) \rightleftharpoons \ce{2SO3}(g)\)
    2. \(\ce{N2O4}(g) \rightleftharpoons \ce{2NO2}(g)\)
    3. \(\ce{C3H8}(g)+\ce{5O2}(g) \rightleftharpoons \ce{3CO2}(g)+\ce{4H2O}(g)\)
    4. At 227 °C, the following reaction has \(K_c\) = 0.0952:

    \[\ce{CH3OH}(g) \rightleftharpoons \ce{CO}(g)+\ce{2H2}(g)\]

    What would be the value of KP at this temperature?

    Answer a

    KP = \(K_c\) (RT)−1

    Answer b

    KP = \(K_c\) (RT)

    Answer c

    KP = \(K_c\) (RT);

    Answer d

    160 or 1.6 × 102

    Video Discussing Converting Kc to Kp: https://youtu.be/_2WVnlqXrV4

    Heterogeneous Equilibria

    A heterogeneous equilibrium is a system in which reactants and products are found in two or more phases. The phases may be any combination of solid, liquid, or gas phases, and solutions. When dealing with these equilibria, remember that solids and pure liquids do not appear in equilibrium constant expressions (the activities of pure solids, pure liquids, and solvents are 1).

    Some heterogeneous equilibria involve chemical changes:

    Example 1

    \[\ce{PbCl2}(s) \rightleftharpoons \ce{Pb^2+}(aq)+\ce{2Cl-}(aq) \label{13.3.30a}\]

    with associated equilibrium constant

    \[K_c=\ce{[Pb^2+][Cl- ]^2} \label{13.3.30b}\]

    Example 2

    \[\ce{CaO}(s)+\ce{CO2}(g) \rightleftharpoons \ce{CaCO3}(s) \label{13.3.31a}\]

    with associated equilibrium constant

    \[K_c=\dfrac{1}{P_{\ce{CO2}}} \label{13.3.31b}\]

    Example 3

    \[\ce{C}(s)+\ce{2S}(g) \rightleftharpoons \ce{CS2}(g) \label{13.3.32a}\]

    with associated equilibrium constant

    \[K_c=\ce{\dfrac{P_{CS2}}{P_{S}^2}} \label{13.3.32b}\]

    Other heterogeneous equilibria involve phase changes, for example, the evaporation of liquid bromine, as shown in the following equation:

    \[\ce{Br2}(l) \rightleftharpoons \ce{Br2}(g) \label{13.3.33a}\]

    with associated equilibrium constant

    \[K_c=P_{\ce{Br2}} \label{13.3.33b}\]

    Summary

    For gases, the equilibrium constant expression can be written as the ratio of the partial pressures of the products to the partial pressures of the reactants, each raised to a power matching its coefficient in the chemical equation. An equilibrium constant calculated from partial pressures (\(K_p\)) is related to \(K\) by the ideal gas constant (\(R\)), the temperature (\(T\)), and the change in the number of moles of gas during the reaction. An equilibrium system that contains products and reactants in a single phase is a homogeneous equilibrium; a system whose reactants, products, or both are in more than one phase is a heterogeneous equilibrium.

    • For a system involving one or more gases, either the molar concentrations of the gases or their partial pressures can be used.
    • Equilibrium constant expression for reactions involving gases using partial pressures: \[K_p=\dfrac{(P_C)^c(P_D)^d}{(P_A)^a(P_B)^b} \]
    • Relationship between \(K_p\) and \(K\): \[K_p = K(RT)^{Δn} \]

    4.3: Gas Phase Equilibria and Heterogeneous Systems is shared under a CC BY-NC-SA 4.0 license and was authored, remixed, and/or curated by LibreTexts.