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Chemistry · Ch 12 — Chemical Equilibrium

Relationship between Kp and Kc

12.4.5

Relationship between Kp and Kc

Consider the general reversible gaseous reaction aA(g)+bB(g)⇌cC(g)+dD(g)aA(g)+bB(g)\rightleftharpoons cC(g)+dD(g). Substituting PA=[A]RTP_A=[A]RT, PB=[B]RTP_B=[B]RT, PC=[C]RTP_C=[C]RT and PD=[D]RTP_D=[D]RT (Section 12.4.4) into the KpK_p expression, Kp=PC cPD dPA aPB bK_p=\dfrac{P_C^{\,c}P_D^{\,d}}{P_A^{\,a}P_B^{\,b}}, gives Kp=[C]c(RT)c [D]d(RT)d[A]a(RT)a [B]b(RT)b=[C]c[D]d[A]a[B]b×(RT)(c+d)−(a+b)K_p=\dfrac{[C]^c(RT)^c\,[D]^d(RT)^d}{[A]^a(RT)^a\,[B]^b(RT)^b}=\dfrac{[C]^c[D]^d}{[A]^a[B]^b}\times(RT)^{(c+d)-(a+b)}. Since Kc=[C]c[D]d[A]a[B]bK_c=\dfrac{[C]^c[D]^d}{[A]^a[B]^b} (Section 12.4.3), this simplifies to the key relation Kp=Kc(RT)ΔnK_p=K_c(RT)^{\Delta n}, where Δn=(c+d)−(a+b)\Delta n=(c+d)-(a+b) = (total moles of gaseous products) −- (total moles of gaseous reactants) in the balanced equation, and R=8.314R=8.314 (with pressure expressed in bar, since standard pressure is defined as 1 bar; recall 1 Pa=1 N m−21\ \text{Pa}=1\ \text{N m}^{-2} and 1 bar=105 Pa1\ \text{bar}=10^5\ \text{Pa}). Problem 12.2 applies this to the Haber equilibrium N2(g)+3H2(g)⇌2NH3(g)N_2(g)+3H_2(g)\rightleftharpoons 2NH_3(g), where Δn=2−4=−2\Delta n=2-4=-2, giving Kp=Kc (RT)−2K_p=K_c\,(RT)^{-2}. Problem 12.3 applies it to $H_2(g)+I_2(g)\rightleftharpoo …

Misc Problem 12.2Kp in terms of Kc for the Haber-process equilibrium

Worked out. Worked example for N2(g) + 3H2(g) is in equilibrium with 2NH3(g). Starting from Kp = (P(NH3))^2 / [P(N2)(P(H2))^3] and substituting P = [conc]RT for each species gives Kp = [NH3]^2(RT)^2 / {N2 x [H2]^3(RT)^3}. Collecting the concentration ratio as Kc and the RT powers separately gives Kp = Kc x (RT)^(2-4) = Kc x RT^-2, since the total gas moles fall from 4 (1 N2 + 3 H2) to 2 (2 NH3), i.e. Δn = 2 - 4 …

Misc Problem 12.3Kp in terms of Kc for H2 + I2 in equilibrium with 2HI

Worked out. Worked example for H2(g) + I2(g) is in equilibrium with 2HI(g). Starting from Kp = (P(HI))^2 / [P(H2)P(I2)] and substituting P = [conc]RT for each species gives Kp = [HI]^2(RT)^2 / {H2 x I2}. The (RT) terms in the denominator combine to (RT)^2, exactly cancelling the (RT)^2 in the numerator, leaving Kp = Kc x RT^(2-(1+1)) = Kc x RT^0 = Kc. This reflects Δn = 2 - (1+1) = 0, i.e. equal gas moles on both sides of this particular …