Overview
Chemical equilibrium occurs when the rates of forward and reverse reactions are equal, resulting in constant concentrations of reactants and products. The equilibrium constant (K) quantifies the position of equilibrium.
Dynamic Equilibrium
At equilibrium:
Forward rate = Reverse rate
Concentrations are constant (not equal)
Reactions continue at molecular level
No net change in concentrations
Equilibrium Constant Expression
For a general reaction:
a A + b B ⇌ c C + d D a\text{A} + b\text{B} \rightleftharpoons c\text{C} + d\text{D} a A + b B ⇌ c C + d D
Concentration Constant (K c K_c K c )
K c = [ C ] c [ D ] d [ A ] a [ B ] b K_c = \frac{[\text{C}]^c[\text{D}]^d}{[\text{A}]^a[\text{B}]^b} K c = [ A ] a [ B ] b [ C ] c [ D ] d
Pressure Constant (K p K_p K p ) - for gases
K p = ( P C ) c ( P D ) d ( P A ) a ( P B ) b K_p = \frac{(P_C)^c(P_D)^d}{(P_A)^a(P_B)^b} K p = ( P A ) a ( P B ) b ( P C ) c ( P D ) d
Rules for Writing K Expressions
Products over reactants
Coefficients become exponents
Only include gases and aqueous species
Omit pure solids and liquids (concentration = 1)
Examples
N 2 ( g ) + 3 H 2 ( g ) ⇌ 2 NH 3 ( g ) \text{N}_2(g) + 3\text{H}_2(g) \rightleftharpoons 2\text{NH}_3(g) N 2 ( g ) + 3 H 2 ( g ) ⇌ 2 NH 3 ( g )
K c = [ NH 3 ] 2 [ N 2 ] [ H 2 ] 3 K_c = \frac{[\text{NH}_3]^2}{[\text{N}_2][\text{H}_2]^3} K c = [ N 2 ] [ H 2 ] 3 [ NH 3 ] 2
CaCO 3 ( s ) ⇌ CaO ( s ) + CO 2 ( g ) \text{CaCO}_3(s) \rightleftharpoons \text{CaO}(s) + \text{CO}_2(g) CaCO 3 ( s ) ⇌ CaO ( s ) + CO 2 ( g )
K c = [ CO 2 ] (solids omitted) K_c = [\text{CO}_2] \quad \text{(solids omitted)} K c = [ CO 2 ] (solids omitted)
AgCl ( s ) ⇌ Ag + ( a q ) + Cl − ( a q ) \text{AgCl}(s) \rightleftharpoons \text{Ag}^+(aq) + \text{Cl}^-(aq) AgCl ( s ) ⇌ Ag + ( a q ) + Cl − ( a q )
K s p = [ Ag + ] [ Cl − ] (solid omitted) K_{sp} = [\text{Ag}^+][\text{Cl}^-] \quad \text{(solid omitted)} K s p = [ Ag + ] [ Cl − ] (solid omitted)
Relationship Between K c K_c K c and K p K_p K p
K p = K c ( R T ) Δ n K_p = K_c(RT)^{\Delta n} K p = K c ( RT ) Δ n
Where:
R R R = 0.0821 L·atm/(mol·K)
T T T = temperature (K)
Δ n \Delta n Δ n = (moles gas products) - (moles gas reactants)
Example
For N 2 ( g ) + 3 H 2 ( g ) ⇌ 2 NH 3 ( g ) \text{N}_2(g) + 3\text{H}_2(g) \rightleftharpoons 2\text{NH}_3(g) N 2 ( g ) + 3 H 2 ( g ) ⇌ 2 NH 3 ( g ) , Δ n = 2 − 4 = − 2 \Delta n = 2 - 4 = -2 Δ n = 2 − 4 = − 2
K p = K c ( R T ) − 2 = K c ( R T ) 2 K_p = K_c(RT)^{-2} = \frac{K_c}{(RT)^2} K p = K c ( RT ) − 2 = ( RT ) 2 K c
Magnitude of K
K Value Position Meaning K ≫ 1 K \gg 1 K ≫ 1 Right Products favored K ≈ 1 K \approx 1 K ≈ 1 Middle Significant amounts of both K ≪ 1 K \ll 1 K ≪ 1 Left Reactants favored
Manipulating Equilibrium Constants
Reversing Reaction
K reverse = 1 K forward K_{\text{reverse}} = \frac{1}{K_{\text{forward}}} K reverse = K forward 1
Multiplying Coefficients
K new = K n K_{\text{new}} = K^n K new = K n
Adding Reactions
K overall = K 1 × K 2 × K 3 ⋯ K_{\text{overall}} = K_1 \times K_2 \times K_3 \cdots K overall = K 1 × K 2 × K 3 ⋯
Example
If: A ⇌ B \text{A} \rightleftharpoons \text{B} A ⇌ B , K 1 = 2.0 K_1 = 2.0 K 1 = 2.0
B ⇌ C \text{B} \rightleftharpoons \text{C} B ⇌ C , K 2 = 3.0 K_2 = 3.0 K 2 = 3.0
Then: A ⇌ C \text{A} \rightleftharpoons \text{C} A ⇌ C , K = K 1 × K 2 = 6.0 K = K_1 \times K_2 = 6.0 K = K 1 × K 2 = 6.0
Reaction Quotient (Q)
Q has the same form as K but uses current (not equilibrium) concentrations.
Q = [ C ] c [ D ] d [ A ] a [ B ] b (at any time) Q = \frac{[\text{C}]^c[\text{D}]^d}{[\text{A}]^a[\text{B}]^b} \quad \text{(at any time)} Q = [ A ] a [ B ] b [ C ] c [ D ] d (at any time)
Comparing Q to K
Condition Direction Action Q < K Q < K Q < K Right (→) More products form Q = K Q = K Q = K Equilibrium No net change Q > K Q > K Q > K Left (←) More reactants form
Equilibrium Calculations
ICE Table Method
I = Initial concentration
C = Change in concentration
E = Equilibrium concentration
Example Problem
For: H 2 ( g ) + I 2 ( g ) ⇌ 2 HI ( g ) \text{H}_2(g) + \text{I}_2(g) \rightleftharpoons 2\text{HI}(g) H 2 ( g ) + I 2 ( g ) ⇌ 2 HI ( g ) , K c = 54.3 K_c = 54.3 K c = 54.3 at 430°C
Initial: [ H 2 ] = 0.50 [\text{H}_2] = 0.50 [ H 2 ] = 0.50 M, [ I 2 ] = 0.50 [\text{I}_2] = 0.50 [ I 2 ] = 0.50 M, [ HI ] = 0 [\text{HI}] = 0 [ HI ] = 0
H₂ I₂ 2HI I 0.50 0.50 0 C − x -x − x − x -x − x + 2 x +2x + 2 x E 0.50 − x 0.50-x 0.50 − x 0.50 − x 0.50-x 0.50 − x 2 x 2x 2 x
K c = [ HI ] 2 [ H 2 ] [ I 2 ] K_c = \frac{[\text{HI}]^2}{[\text{H}_2][\text{I}_2]} K c = [ H 2 ] [ I 2 ] [ HI ] 2
54.3 = ( 2 x ) 2 ( 0.50 − x ) ( 0.50 − x ) = 4 x 2 ( 0.50 − x ) 2 54.3 = \frac{(2x)^2}{(0.50-x)(0.50-x)} = \frac{4x^2}{(0.50-x)^2} 54.3 = ( 0.50 − x ) ( 0.50 − x ) ( 2 x ) 2 = ( 0.50 − x ) 2 4 x 2
54.3 = 2 x 0.50 − x \sqrt{54.3} = \frac{2x}{0.50-x} 54.3 = 0.50 − x 2 x
7.37 ( 0.50 − x ) = 2 x 7.37(0.50-x) = 2x 7.37 ( 0.50 − x ) = 2 x
3.69 − 7.37 x = 2 x 3.69 - 7.37x = 2x 3.69 − 7.37 x = 2 x
x = 0.39 M x = 0.39 \text{ M} x = 0.39 M
[ H 2 ] = [ I 2 ] = 0.11 M , [ HI ] = 0.78 M [\text{H}_2] = [\text{I}_2] = 0.11 \text{ M}, \quad [\text{HI}] = 0.78 \text{ M} [ H 2 ] = [ I 2 ] = 0.11 M , [ HI ] = 0.78 M
Special Equilibrium Constants
K w K_w K w (Water)
H 2 O ( l ) ⇌ H + ( a q ) + OH − ( a q ) \text{H}_2\text{O}(l) \rightleftharpoons \text{H}^+(aq) + \text{OH}^-(aq) H 2 O ( l ) ⇌ H + ( a q ) + OH − ( a q )
K w = [ H + ] [ OH − ] = 1.0 × 10 − 14 at 25°C K_w = [\text{H}^+][\text{OH}^-] = 1.0 \times 10^{-14} \text{ at 25°C} K w = [ H + ] [ OH − ] = 1.0 × 1 0 − 14 at 25°C
K a K_a K a (Acid Dissociation)
HA ( a q ) ⇌ H + ( a q ) + A − ( a q ) \text{HA}(aq) \rightleftharpoons \text{H}^+(aq) + \text{A}^-(aq) HA ( a q ) ⇌ H + ( a q ) + A − ( a q )
K a = [ H + ] [ A − ] [ HA ] K_a = \frac{[\text{H}^+][\text{A}^-]}{[\text{HA}]} K a = [ HA ] [ H + ] [ A − ]
K b K_b K b (Base Dissociation)
B ( a q ) + H 2 O ( l ) ⇌ BH + ( a q ) + OH − ( a q ) \text{B}(aq) + \text{H}_2\text{O}(l) \rightleftharpoons \text{BH}^+(aq) + \text{OH}^-(aq) B ( a q ) + H 2 O ( l ) ⇌ BH + ( a q ) + OH − ( a q )
K b = [ BH + ] [ OH − ] [ B ] K_b = \frac{[\text{BH}^+][\text{OH}^-]}{[\text{B}]} K b = [ B ] [ BH + ] [ OH − ]
K s p K_{sp} K s p (Solubility Product)
AgCl ( s ) ⇌ Ag + ( a q ) + Cl − ( a q ) \text{AgCl}(s) \rightleftharpoons \text{Ag}^+(aq) + \text{Cl}^-(aq) AgCl ( s ) ⇌ Ag + ( a q ) + Cl − ( a q )
K s p = [ Ag + ] [ Cl − ] K_{sp} = [\text{Ag}^+][\text{Cl}^-] K s p = [ Ag + ] [ Cl − ]
Temperature Dependence
K changes with temperature:
Exothermic: K decreases as T increases
Endothermic: K increases as T increases
Van't Hoff Equation
ln ( K 2 K 1 ) = − Δ H ° R ( 1 T 2 − 1 T 1 ) \ln\left(\frac{K_2}{K_1}\right) = -\frac{\Delta H°}{R}\left(\frac{1}{T_2} - \frac{1}{T_1}\right) ln ( K 1 K 2 ) = − R Δ H ° ( T 2 1 − T 1 1 )