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Chemistry · Ch 8 — Physical and Chemical Equilibrium

Equilibrium constants for heterogeneous equilibrium

8.6.3

Equilibrium constants for heterogeneous equilibrium

For a heterogeneous equilibrium, the equilibrium-constant expression can be simplified further, because a pure solid or pure liquid does not have a variable concentration the way a gas or a dissolved species does.

Consider CaCO3(s)⇌CaO(s)+CO2(g)CaCO_3(s) \rightleftharpoons CaO(s) + CO_2(g). Writing the equilibrium constant in the usual way would give KC=[CaO(s)][CO2(g)][CaCO3(s)]K_C = \dfrac{[CaO(s)][CO_2(g)]}{[CaCO_3(s)]}. But a pure solid, unlike a gas, does not expand to fill its container -- it always has the same number of moles per litre of its own volume at a given temperature, so its concentration (active mass) is itself a constant. Since both [CaCO3(s)][CaCO_3(s)] and [CaO(s)][CaO(s)] are constants, they can be absorbed into the equilibrium constant itself, leaving

KC=[CO2(g)]orKP=pCO2K_C = [CO_2(g)] \qquad \text{or} \qquad K_P = p_{CO_2}

So the equilibrium constant for this reaction depends only on the concentration (or partial pressure) of the gaseous carbon dioxide, not at all on how much solid calcium carbonate or calcium oxide happens to be present. The same reasoning applies to a pure liquid, whose active mass likewise stays constant at a given temperature -- so pure-liquid concentration terms can also be dropped from an equilibrium-constant expression. For example, in

CO2(g)+H2O(l)⇌H+(aq)+HCO3−(aq)CO_2(g) + H_2O(l) \rightleftharpoons H^+(aq) + HCO_3^-(aq)

since H2O(l)H_2O(l) is a pure liquid, its concentration is excluded and KCK_C is written

KC=[H+(aq)][HCO3−(aq)][CO2(g)]K_C = \frac{[H^+(aq)][HCO_3^-(aq)]}{[CO_2(g)]}

Worked example: writing Kp and Kc for three reactions.

  1. 2SO2(g)+O2(g)⇌2SO3(g)2SO_2(g) + O_2(g) \rightleftharpoons 2SO_3(g): both sides fully gaseous, so KC=[SO3]2[SO2]2[O2]K_C = \dfrac{[SO_3]^2}{[SO_2]^2[O_2]} and KP=pSO32pSO22 pO2K_P = \dfrac{p_{SO_3}^2}{p_{SO_2}^2\,p_{O_2}}.

  2. 2CO(g)⇌CO2(g)+C(s)2CO(g) \rightleftharpoons CO_2(g) + C(s): heterogeneous, with pure solid carbon dropped from the expression, so KC=[CO2][CO]2K_C = \dfrac{[CO_2]}{[CO]^2} and KP=pCO2pCO2K_P = \dfrac{p_{CO_2}}{p_{CO}^2}.

  3. Ag2O(s)+2NH3(aq)⇌2AgNO3(aq)+H2O(l)Ag_2O(s) + 2NH_3(aq) \rightleftharpoons 2AgNO_3(aq) + H_2O(l): with both the pure solid Ag2O(s)Ag_2O(s) and the pure liquid H2O(l)H_2O(l) dropped, KC=[AgNO3]2[NH3]2K_C = \dfrac{[AgNO_3]^2}{[NH_3]^2}. …

Misc 8.6.3-worked-kpkc-threeWorked example: writing Kp and Kc for three reactions

Worked out. For (1) 2SO2(g)+O2(g)⇌2SO3(g)2SO_2(g) + O_2(g) \rightleftharpoons 2SO_3(g): KC=[SO3]2[SO2]2[O2]K_C = \dfrac{[SO_3]^2}{[SO_2]^2[O_2]} and KP=pSO32pSO22 pO2K_P = \dfrac{p_{SO_3}^2}{p_{SO_2}^2\,p_{O_2}}. For (2) 2CO(g)⇌CO2(g)+C(s)2CO(g) \rightleftharpoons CO_2(g) + C(s) (heterogeneous, C(s) dropped): KC=[CO2][CO]2K_C = \dfrac{[CO_2]}{[CO]^2} and KP=pCO2pCO2K_P = \dfrac{p_{CO_2}}{p_{CO}^2}. For (3) Ag2O(s)+2NH3(aq)⇌2AgNO3(aq)+H2O(l)Ag_2O(s) + 2NH_3(aq) \rightleftharpoons 2AgNO_3(aq) + H_2O(l) (both Ag2_2O(s) and H2_2O(l) dropped): KC=[AgNO3]2[NH3]2K_C = \dfrac{[AgNO_3]^2}{[NH_3]^2}. …

Misc 8.6.3-evaluate-yourselfEvaluate Yourself: two self-check Kc/Kp calculations

Worked out. (1) Fe3+(aq)+SCN−(aq)⇌[Fe(SCN)]2+(aq)Fe^{3+}(aq) + SCN^-(aq) \rightleftharpoons [Fe(SCN)]^{2+}(aq): starting [Fe3+]=1×10−3[Fe^{3+}] = 1\times10^{-3} M, [SCN−]=8×10−4[SCN^-] = 8\times10^{-4} M; at equilibrium [Fe(SCN)2+]=2×10−4[Fe(SCN)^{2+}] = 2\times10^{-4} M -- find KCK_C. (2) 2NO(g)+O2(g)⇌2NO2(g)2NO(g) + O_2(g) \rightleftharpoons 2NO_2(g) studied with initial 1 atm NO and 1 atm O2O_2; at equilibrium pO2=0.52p_{O_2} = 0.52 atm -- find KPK_P. …