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7.4 Chemical Equilibrium, Heats of Reaction, and Mixing

Key Takeaways

  • The equilibrium constant Keq is calculated from standard Gibbs free energy of reaction: delta G_rxn_dec = -R * T * ln(Keq).

  • The van 't Hoff equation describes temperature effects on Keq; increasing temperature shifts endothermic reactions forward and exothermic reactions backward.

  • Kirchhoff's Law corrects the standard enthalpy of reaction for temperature deviations using delta Cp values.

  • Ideal mixtures have zero enthalpy of mixing and volume change, whereas non-ideal solutions have non-zero excess properties.

  • Partial molar properties represent the molar contribution of a species to a mixture, related through the Gibbs-Duhem equation.

Last updated: July 2026

Chemical Reaction Equilibrium

Chemical reaction equilibrium calculations determine the maximum possible conversion (thermodynamic limit) of a chemical reaction at given operating conditions. The fundamental criterion for chemical equilibrium is that the total Gibbs free energy of the system is minimized at constant temperature and pressure. For a general reaction ∑νiAi=0\sum \nu_i A_i = 0 (where stoichiometric coefficients νi\nu_i are positive for products and negative for reactants), the standard Gibbs free energy change of reaction (ΔGrxn∘\Delta G_{rxn}^\circ) is calculated from the standard Gibbs free energies of formation (ΔGf,i∘\Delta G_{f,i}^\circ) found in reference tables:

ΔGrxn∘=∑νiΔGf,i∘\Delta G_{rxn}^\circ = \sum \nu_i \Delta G_{f,i}^\circ

The equilibrium constant (KeqK_{eq}) is directly related to the standard Gibbs free energy change by:

ΔGrxn∘=−RTln⁡Keq  ⟹  Keq=exp⁡(−ΔGrxn∘RT)\Delta G_{rxn}^\circ = -RT \ln K_{eq} \implies K_{eq} = \exp\left(-\frac{\Delta G_{rxn}^\circ}{RT}\right)

where RR is the universal gas constant and TT is the absolute temperature. The equilibrium constant is defined in terms of the activities (aia_i) of the reacting species:

Keq=∏(ai)νiK_{eq} = \prod (a_i)^{\nu_i}

For an ideal gas mixture, the activity of species ii is ai=yiP/P∘a_i = y_i P / P^\circ, where P∘P^\circ is the standard-state pressure (1 bar1 \text{ bar} or 100 kPa100 \text{ kPa}). This gives:

Keq=(PP∘)∑νi∏(yi)νi=(PP∘)ΔνKyK_{eq} = \left(\frac{P}{P^\circ}\right)^{\sum \nu_i} \prod (y_i)^{\nu_i} = \left(\frac{P}{P^\circ}\right)^{\Delta \nu} K_y

where Δν=∑νi\Delta \nu = \sum \nu_i is the change in the total number of moles of gas. Note that if Δν>0\Delta \nu > 0, increasing the system pressure PP will decrease the equilibrium mole fraction constant KyK_y, thereby decreasing the equilibrium conversion (Le Chatelier's Principle).

Temperature Effects: The van 't Hoff Equation

The standard Gibbs free energy change, and therefore KeqK_{eq}, is a function of temperature. The effect of temperature on the equilibrium constant is quantitatively described by the van 't Hoff equation:

d(ln⁡Keq)dT=ΔHrxn∘RT2\frac{d(\ln K_{eq})}{dT} = \frac{\Delta H_{rxn}^\circ}{R T^2}

where ΔHrxn∘\Delta H_{rxn}^\circ is the standard enthalpy of reaction. Assuming ΔHrxn∘\Delta H_{rxn}^\circ is approximately constant over a moderate temperature range, integrating the van 't Hoff equation from T1T_1 to T2T_2 yields:

ln⁡(Keq(T2)Keq(T1))=−ΔHrxn∘R(1T2−1T1)\ln\left(\frac{K_{eq}(T_2)}{K_{eq}(T_1)}\right) = -\frac{\Delta H_{rxn}^\circ}{R} \left(\frac{1}{T_2} - \frac{1}{T_1}\right)

This relationship reveals that:

  • For endothermic reactions (ΔHrxn∘>0\Delta H_{rxn}^\circ > 0), KeqK_{eq} increases as temperature increases, shifting the equilibrium toward the products.
  • For exothermic reactions (ΔHrxn∘<0\Delta H_{rxn}^\circ < 0), KeqK_{eq} decreases as temperature increases, shifting the equilibrium toward the reactants.

Heats of Reaction and Temperature Dependence

The standard heat of reaction (ΔHrxn∘\Delta H_{rxn}^\circ) is calculated from standard heats of formation (ΔHf,i∘\Delta H_{f,i}^\circ):

ΔHrxn∘=∑νiΔHf,i∘\Delta H_{rxn}^\circ = \sum \nu_i \Delta H_{f,i}^\circ

To determine the heat of reaction at a temperature other than the standard state temperature (T∘=298.15 KT^\circ = 298.15 \text{ K}), we apply Kirchhoff's Law:

ΔHrxn∘(T)=ΔHrxn∘(T∘)+∫T∘TΔCpdT\Delta H_{rxn}^\circ(T) = \Delta H_{rxn}^\circ(T^\circ) + \int_{T^\circ}^T \Delta C_p dT

where ΔCp=∑νiCp,i(T)\Delta C_p = \sum \nu_i C_{p,i}(T) is the change in heat capacity upon reaction. If the heat capacities are functions of temperature (typically expressed as polynomials Cp,i=ai+biT+ciT2+diT3C_{p,i} = a_i + b_i T + c_i T^2 + d_i T^3), ΔCp\Delta C_p must be integrated accordingly.

Thermodynamics of Mixing

When pure substances are mixed to form a solution, the thermodynamic properties change. For an ideal solution, the molecules of different species are similar in size and chemical nature, resulting in zero heat of mixing (ΔHmix=0\Delta H_{mix} = 0) and zero volume change on mixing (ΔVmix=0\Delta V_{mix} = 0). The entropy and Gibbs free energy of mixing for an ideal solution are:

ΔSmixideal=−R∑xiln⁡xi>0\Delta S_{mix}^{\text{ideal}} = -R \sum x_i \ln x_i > 0 ΔGmixideal=RT∑xiln⁡xi<0\Delta G_{mix}^{\text{ideal}} = RT \sum x_i \ln x_i < 0

For non-ideal solutions, we define excess properties (MEM^E) as the difference between the actual solution property (MM) and that of an ideal solution (MidealM^{\text{ideal}}) at the same temperature, pressure, and composition. The heat of mixing is equal to the excess enthalpy of the solution:

ΔHmix=HE=H−∑xiHi\Delta H_{mix} = H^E = H - \sum x_i H_i

Partial Molar Properties

In a mixture, the contribution of a single mole of component ii to the total property MM (such as volume, enthalpy, or Gibbs free energy) is described by its partial molar property (Mˉi\bar{M}_i):

Mˉi=(∂(nM)∂ni)T,P,nj≠i\bar{M}_i = \left(\frac{\partial (n M)}{\partial n_i}\right)_{T, P, n_{j \ne i}}

The chemical potential μi\mu_i is simply the partial molar Gibbs free energy (Gˉi\bar{G}_i).

The total property of a solution is calculated from the partial molar properties via the summability relation:

nM=∑niMˉi  ⟹  M=∑xiMˉinM = \sum n_i \bar{M}_i \implies M = \sum x_i \bar{M}_i

The changes in partial molar properties are constrained by the Gibbs-Duhem equation. At constant temperature and pressure, the Gibbs-Duhem relation is:

∑xidMˉi=0\sum x_i d\bar{M}_i = 0

For a binary mixture, this simplifies to:

x1dMˉ1+x2dMˉ2=0  ⟹  x1dMˉ1dx1+x2dMˉ2dx1=0x_1 d\bar{M}_1 + x_2 d\bar{M}_2 = 0 \implies x_1 \frac{d\bar{M}_1}{dx_1} + x_2 \frac{d\bar{M}_2}{dx_1} = 0

This relationship shows that the partial molar properties of components in a mixture cannot change independently; if one increases, the other must decrease.

Worked Example: van 't Hoff Temperature Correction

For the water-gas shift reaction (CO+H2O⇌CO2+H2CO + H_2O \rightleftharpoons CO_2 + H_2), the equilibrium constant is Keq=22.4K_{eq} = 22.4 at 600 K600\text{ K}. The standard enthalpy of reaction is constant over the temperature range at ΔHrxn∘=−41.2 kJ/mol=−41200 J/mol\Delta H_{rxn}^\circ = -41.2\text{ kJ/mol} = -41200\text{ J/mol}. Calculate the equilibrium constant at 800 K800\text{ K}. The universal gas constant is R=8.314 J/(mol⋅K)R = 8.314\text{ J/(mol}\cdot\text{K)}.

Step 1: Write down the integrated van 't Hoff equation.

ln⁡(Keq(T2)Keq(T1))=−ΔHrxn∘R(1T2−1T1)\ln\left(\frac{K_{eq}(T_2)}{K_{eq}(T_1)}\right) = -\frac{\Delta H_{rxn}^\circ}{R} \left(\frac{1}{T_2} - \frac{1}{T_1}\right)

Step 2: Substitute the known values.

T1=600 K,Keq(T1)=22.4T_1 = 600 \text{ K}, \quad K_{eq}(T_1) = 22.4 T2=800 KT_2 = 800 \text{ K} ln⁡(Keq(800 K)22.4)=−−41200 J/mol8.314 J/(mol⋅K)(1800 K−1600 K)\ln\left(\frac{K_{eq}(800\text{ K})}{22.4}\right) = -\frac{-41200 \text{ J/mol}}{8.314 \text{ J/(mol}\cdot\text{K)}} \left(\frac{1}{800 \text{ K}} - \frac{1}{600 \text{ K}}\right)

Step 3: Solve the arithmetic.

1800−1600=0.00125−0.001667=−0.0004167 K−1\frac{1}{800} - \frac{1}{600} = 0.00125 - 0.001667 = -0.0004167 \text{ K}^{-1} ln⁡(Keq(800 K)22.4)=4955.5×(−0.0004167)≈−2.065\ln\left(\frac{K_{eq}(800\text{ K})}{22.4}\right) = 4955.5 \times (-0.0004167) \approx -2.065

Step 4: Exponentiate to find Keq(800 K)K_{eq}(800\text{ K}).

Keq(800 K)22.4=exp⁡(−2.065)≈0.1268\frac{K_{eq}(800\text{ K})}{22.4} = \exp(-2.065) \approx 0.1268 Keq(800 K)=22.4×0.1268≈2.84K_{eq}(800\text{ K}) = 22.4 \times 0.1268 \approx 2.84

As expected for an exothermic reaction, raising the temperature from 600 K600\text{ K} to 800 K800\text{ K} significantly reduces the equilibrium constant from 22.422.4 to 2.842.84, meaning that the equilibrium composition shifts toward the reactants, reducing the maximum conversion of carbon monoxide.

Test Your Knowledge

For a certain endothermic reaction, the equilibrium constant is Keq = 1.0 * 10^3 at 300 K. If the heat of reaction is 50.0 kJ/mol and is assumed constant, what is the equilibrium constant at 350 K?

A

5.3 * 10^1

B

1.9 * 10^4

C

8.5 * 10^2

D

1.0 * 10^3

Test Your Knowledge

The standard heats of formation of carbon monoxide, water vapor, carbon dioxide, and hydrogen gas at 298.15 K are -110.5 kJ/mol, -241.8 kJ/mol, -393.5 kJ/mol, and 0 kJ/mol, respectively. What is the standard heat of the water-gas shift reaction (CO + H2O <-> CO2 + H2) at 298.15 K?

A

41.2 kJ/mol

B

-745.8 kJ/mol

C

-635.3 kJ/mol

D

-41.2 kJ/mol

Test Your Knowledge

At constant temperature and pressure, the Gibbs-Duhem equation relates the changes in chemical potentials of the components in a mixture. For a binary system, which of the following expressions is correct?

A

x1 * d(mu1) + x2 * d(mu2) = 0

B

d(mu1) + d(mu2) = 0

C

x1 * d(mu1) - x2 * d(mu2) = 0

D

x2 * d(mu1) + x1 * d(mu2) = 0

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