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Chemical Equilibrium Chapter 16
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Equilibrium: the extent of a reaction
In stoichiometry we talk about theoretical yields, and the many reasons actual yields may be lower. Another critical reason actual yields may be lower is the reversibility of chemical reactions: some reactions may produce only 70% of the product you may calculate they ought to produce. Equilibrium looks at the extent of a chemical reaction.
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Physical equilibrium Chemical equilibrium
Equilibrium is a state in which two opposing processes are occurring at the same rate so there are no observable changes as time goes by. Chemical equilibrium is achieved when: the rates of the forward and reverse reactions are equal and the concentrations of the reactants and products remain constant Physical equilibrium H2O (l) H2O (g) Chemical equilibrium N2O4 (g) 2NO2 (g) 14.1
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The Concept of Equilibrium
Consider colorless frozen N2O4. At room temperature, it decomposes to brown NO2: N2O4(g) 2NO2(g). At some time, the color stops changing and we have a mixture of N2O4 and NO2. Chemical equilibrium is the point at which the rate of the forward reaction is equal to the rate of the reverse reaction. At that point, the concentrations of all species are constant. Using the collision model: as the amount of NO2 builds up, there is a chance that two NO2 molecules will collide to form N2O4. At the beginning of the reaction, there is no NO2 so the reverse reaction (2NO2(g) N2O4(g)) does not occur.
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The Concept of Equilibrium
As the substance warms it begins to decompose: N2O4(g) 2NO2(g) When enough NO2 is formed, it can react to form N2O4: 2NO2(g) N2O4(g). At equilibrium, as much N2O4 reacts to form NO2 as NO2 reacts to re-form N2O4 The double arrow implies the process is dynamic.
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The Concept of Equilibrium
As the reaction progresses [A] decreases to a constant, [B] increases from zero to a constant. When [A] and [B] are constant, equilibrium is achieved.
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N2O4 (g) 2NO2 (g) equilibrium equilibrium equilibrium Start with NO2
Start with NO2 & N2O4 14.1
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constant 14.1
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The Equilibrium Constant
No matter the starting composition of reactants and products, the same ratio of concentrations is achieved at equilibrium. For a general reaction the equilibrium constant expression is where Kc is the equilibrium constant.
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Equilibrium Will N2O4 (g) 2NO2 (g) K = [NO2]2 [N2O4] = 4.63 x 10-3
aA + bB cC + dD K = [C]c[D]d [A]a[B]b Law of Mass Action Equilibrium Will K >> 1 Lie to the right Favor products K << 1 Lie to the left Favor reactants 14.1
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Homogenous equilibrium applies to reactions in which all reacting species are in the same phase.
N2O4 (g) NO2 (g) Kp = NO2 P2 N2O4 P Kc = [NO2]2 [N2O4] In most cases Kc Kp aA (g) + bB (g) cC (g) + dD (g) Kp = Kc(RT)Dn Dn = moles of gaseous products – moles of gaseous reactants = (c + d) – (a + b) 14.2
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Homogeneous Equilibrium
CH3COOH (aq) + H2O (l) CH3COO- (aq) + H3O+ (aq) [CH3COO-][H3O+] [CH3COOH][H2O] Kc = ‘ [H2O] = constant [CH3COO-][H3O+] [CH3COOH] = Kc [H2O] ‘ Kc = General practice not to include units for the equilibrium constant. 14.2
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The Equilibrium Expression
Write the equilibrium expression for the following reaction:
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The equilibrium concentrations for the reaction between carbon monoxide and molecular chlorine to form COCl2 (g) at 740C are [CO] = M, [Cl2] = M, and [COCl2] = 0.14 M. Calculate the equilibrium constants Kc and Kp. CO (g) + Cl2 (g) COCl2 (g) [COCl2] [CO][Cl2] = 0.14 0.012 x 0.054 Kc = = 220 Kp = Kc(RT)Dn Dn = 1 – 2 = -1 R = T = = 347 K Kp = 220 x ( x 347)-1 = 7.7 14.2
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The equilibrium constant Kp for the reaction
is 158 at 1000K. What is the equilibrium pressure of O2 if the PNO = atm and PNO = atm? 2NO2 (g) NO (g) + O2 (g) 2 Kp = 2 PNO PO PNO PO 2 = Kp PNO PO 2 = 158 x (0.400)2/(0.270)2 = 347 atm 14.2
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Heterogenous equilibrium applies to reactions in which reactants and products are in different phases. CaCO3 (s) CaO (s) + CO2 (g) Kc = ‘ [CaO][CO2] [CaCO3] [CaCO3] = constant [CaO] = constant Kc x ‘ [CaCO3] [CaO] Kc = [CO2] = Kp = PCO 2 The concentration of solids and pure liquids are not included in the expression for the equilibrium constant. 14.2
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does not depend on the amount of CaCO3 or CaO
CaCO3 (s) CaO (s) + CO2 (g) PCO 2 = Kp PCO 2 does not depend on the amount of CaCO3 or CaO 14.2
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Writing Equilibrium Constant Expressions
The concentrations of the reacting species in the condensed phase are expressed in M. In the gaseous phase, the concentrations can be expressed in M or in atm. The concentrations of pure solids, pure liquids and solvents do not appear in the equilibrium constant expressions. The equilibrium constant is a dimensionless quantity. In quoting a value for the equilibrium constant, you must specify the balanced equation and the temperature. If a reaction can be expressed as a sum of two or more reactions, the equilibrium constant for the overall reaction is given by the product of the equilibrium constants of the individual reactions. 14.2
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Calculating Equilibrium Concentrations
Express the equilibrium concentrations of all species in terms of the initial concentrations and a single unknown x, which represents the change in concentration. Write the equilibrium constant expression in terms of the equilibrium concentrations. Knowing the value of the equilibrium constant, solve for x. Having solved for x, calculate the equilibrium concentrations of all species. 14.4
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ICE At 12800C the equilibrium constant (Kc) for the reaction
Is 1.1 x If the initial concentrations are [Br2] = M and [Br] = M, calculate the concentrations of these species at equilibrium. Br2 (g) Br (g) Let x be the change in concentration of Br2 Br2 (g) Br (g) Initial (M) 0.063 0.012 ICE Change (M) -x +2x Equilibrium (M) x x [Br]2 [Br2] Kc = Kc = ( x)2 x = 1.1 x 10-3 Solve for x 14.4
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Kc = ( x)2 x = 1.1 x 10-3 4x x = – x 4x x = 0 -b ± b2 – 4ac 2a x = ax2 + bx + c =0 x = x = Br2 (g) Br (g) Initial (M) Change (M) Equilibrium (M) 0.063 0.012 -x +2x x x At equilibrium, [Br] = x = M or M At equilibrium, [Br2] = – x = M 14.4
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Example Problem: Calculate Concentration
Note the moles into a L vessel stuff ... calculate molarity. Starting concentration of HI: 2.5 mol/10.32 L = M 2 HI H I2 Initial: Change: Equil: 0.242 M 0 0 -2x +x +x x x x What we are asked for here is the equilibrium concentration of H2 ... ... otherwise known as x. So, we need to solve this beast for x.
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Example Problem: Calculate Concentration
And yes, it’s a quadratic equation. Doing a bit of rearranging: x = or – Since we are using this to model a real, physical system, we reject the negative root. The [H2] at equil. is M.
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Example Problem: Calculate Keq
This type of problem is typically tackled using the “three line” approach: 2 NO + O2 2 NO2 Initial: Change: Equilibrium:
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Approximating If Keq is really small the reaction will not proceed to the right very far, meaning the equilibrium concentrations will be nearly the same as the initial concentrations of your reactants. 0.20 – x is just about 0.20 is x is really dinky. If the difference between Keq and initial concentrations is around 3 orders of magnitude or more, go for it. Otherwise, you have to use the quadratic.
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Initial Concentration of I2: 0.50 mol/2.5L = 0.20 M I2 2 I
Example Initial Concentration of I2: 0.50 mol/2.5L = 0.20 M I I More than 3 orders of mag. between these numbers. The simplification will work here. Initial change equil: -x x 0.20-x x With an equilibrium constant that small, whatever x is, it’s near dink, and 0.20 minus dink is 0.20 (like a million dollars minus a nickel is still a million dollars). 0.20 – x is the same as 0.20 x = 3.83 x 10-6 M
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Initial Concentration of I2: 0.50 mol/2.5L = 0.20 M I2 2 I
Example Initial Concentration of I2: 0.50 mol/2.5L = 0.20 M I I These are too close to each other ... 0.20-x will not be trivially close to 0.20 here. Initial change equil: -x x 0.20-x x Looks like this one has to proceed through the quadratic ...
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‘ ‘ ‘ ‘ ‘ Kc = [C][D] [A][B] Kc = [E][F] [C][D] Kc A + B C + D Kc
C + D E + F [E][F] [A][B] Kc = A + B E + F Kc Kc = Kc ‘ x If a reaction can be expressed as the sum of two or more reactions, the equilibrium constant for the overall reaction is given by the product of the equilibrium constants of the individual reactions. 14.2
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‘ N2O4 (g) 2NO2 (g) 2NO2 (g) N2O4 (g) = 4.63 x 10-3 K = [NO2]2 [N2O4]
= 216 When the equation for a reversible reaction is written in the opposite direction, the equilibrium constant becomes the reciprocal of the original equilibrium constant. 14.2
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Qc > Kc system proceeds from right to left to reach equilibrium
The reaction quotient (Qc) is calculated by substituting the initial concentrations of the reactants and products into the equilibrium constant (Kc) expression. IF Qc > Kc system proceeds from right to left to reach equilibrium Qc = Kc the system is at equilibrium Qc < Kc system proceeds from left to right to reach equilibrium 14.4
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Le Châtelier’s Principle
If an external stress is applied to a system at equilibrium, the system adjusts in such a way that the stress is partially offset as the system reaches a new equilibrium position. Changes in Concentration N2 (g) + 3H2 (g) NH3 (g) Add NH3 Equilibrium shifts left to offset stress 14.5
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Le Châtelier’s Principle
Changes in Concentration continued Remove Add Add Remove aA + bB cC + dD Change Shifts the Equilibrium Increase concentration of product(s) left Decrease concentration of product(s) right Increase concentration of reactant(s) right Decrease concentration of reactant(s) left 14.5
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Le Châtelier’s Principle
Changes in Volume and Pressure A (g) + B (g) C (g) Change Shifts the Equilibrium Increase pressure Side with fewest moles of gas Decrease pressure Side with most moles of gas Increase volume Side with most moles of gas Decrease volume Side with fewest moles of gas 14.5
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Le Châtelier’s Principle
Changes in Temperature Change Exothermic Rx Endothermic Rx Increase temperature K decreases K increases Decrease temperature K increases K decreases colder hotter 14.5
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Le Châtelier’s Principle
Adding a Catalyst does not change K does not shift the position of an equilibrium system system will reach equilibrium sooner uncatalyzed catalyzed Catalyst lowers Ea for both forward and reverse reactions. Catalyst does not change equilibrium constant or shift equilibrium. 14.5
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Example
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Life at High Altitudes and Hemoglobin Production
Chemistry In Action Life at High Altitudes and Hemoglobin Production Hb (aq) + O2 (aq) HbO2 (aq) Kc = [HbO2] [Hb][O2]
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Chemistry In Action: The Haber Process
N2 (g) + 3H2 (g) NH3 (g) DH0 = kJ/mol
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Le Châtelier’s Principle
Change Equilibrium Constant Change Shift Equilibrium Concentration yes no Pressure yes no Volume yes no Temperature yes yes Catalyst no no 14.5
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