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Spec Mapping — OCR H432 Module 3.2.3 — Chemical equilibrium, covering the concept of dynamic equilibrium in a closed system (equal forward and reverse rates; concentrations constant), Le Chatelier's principle and its qualitative application to predict the direction of equilibrium shift in response to changes in concentration, pressure, and temperature, the equilibrium constant Kc and its expression in terms of equilibrium concentrations and stoichiometric coefficients (with appropriate units), Kc calculations using ICE tables, and the choice of compromise conditions in industrial processes such as the Haber and Contact processes (refer to the official OCR H432 specification document for exact wording).
This lesson closes OCR Module 3.2 by fusing kinetics (Lessons 6–9) with thermodynamics (Lessons 1–5) into the concept of chemical equilibrium. Most chemical reactions are not actually one-way: the reverse process is also happening. In a closed system, the forward and reverse reactions eventually reach equal rates, at which point the concentrations of all species stop changing — this is dynamic equilibrium. The qualitative tool for predicting how equilibrium responds to changes (concentration, pressure, temperature, catalyst) is Le Chatelier's principle, articulated by the French chemist Henri Louis Le Chatelier (1884): when a system at equilibrium is subjected to a stress, it shifts to partially counteract that stress. The quantitative tool is the equilibrium constant Kc, the ratio of product to reactant concentrations at equilibrium, each raised to the power of its stoichiometric coefficient. Kc is a constant only at a fixed temperature; it depends sensitively on T but not on initial concentrations, pressures, or the presence of a catalyst. The lesson develops the conceptual framework and provides four worked examples — H2 + I2 ⇌ 2HI, ICE-table analysis, N2O4 ⇌ 2NO2 dissociation, and the industrial Haber process — culminating with a comparison of compromise conditions used in the Haber and Contact processes.
Key Equation: for a homogeneous equilibrium aA+bB⇌cC+dD, the equilibrium constant in terms of concentrations is: Kc=[A]a[B]b[C]c[D]d Units depend on Δn=(c+d)−(a+b): units of Kc are (mol dm−3)Δn. Kc depends only on temperature.
Consider a reversible reaction in a closed container:
A+B⇌C+D
Initially only A and B are present, so only the forward reaction occurs. The forward rate is at its highest because [A] and [B] are at their maximum. As the reaction proceeds, C and D accumulate, so the reverse reaction (consuming C and D) begins. The reverse rate rises while the forward rate falls. Eventually the two rates become equal, at which point the concentrations of all four species stop changing.
This state — equal forward and reverse rates, with no net change in composition — is dynamic equilibrium.
Le Chatelier's principle: When a system at dynamic equilibrium is subjected to a change in conditions (concentration, pressure, or temperature), the position of equilibrium shifts to partially oppose that change.
The word partially is essential — the system cannot fully reverse the imposed change, only attenuate it. Le Chatelier's principle is qualitative: it tells us the direction of the shift, not its magnitude.
Example: N2+3H2⇌2NH3
Importantly, Kc is unchanged by concentration changes at constant temperature — the new equilibrium has different concentrations but the same ratio.
Increasing the total pressure of a gas-phase equilibrium (by compressing the vessel) shifts the position towards the side with fewer moles of gas — to reduce the number of gas particles and partially counteract the pressure rise. Decreasing pressure shifts toward more moles of gas.
Example 1: N2(g)+3H2(g)⇌2NH3(g)
Example 2: H2(g)+I2(g)⇌2HI(g)
Like concentration, pressure changes do not alter Kc at constant temperature.
Temperature is the unique variable that actually changes Kc, because it changes the relative rate constants kfwd and krev asymmetrically (each via the Arrhenius equation, k=Ae−Ea/RT, with their own Ea that differ by ΔH).
Example: N2+3H2⇌2NH3, ΔH=−92 kJ mol−1 (exothermic forward).
Example: 2SO2+O2⇌2SO3, ΔH=−196 kJ mol−1 (exothermic).
flowchart TD
A[What is being changed?] --> B[Concentration]
A --> C[Pressure]
A --> D[Temperature]
A --> E[Catalyst]
B --> B1[Shift AWAY from the added species,<br/>TOWARDS the removed species]
B1 --> B2[Kc unchanged]
C --> C1[Shift towards FEWER moles of gas<br/>if pressure increases]
C1 --> C2[Kc unchanged]
D --> D1{Forward exothermic?}
D1 -->|Yes| D2[Higher T: shift LEFT, Kc DECREASES]
D1 -->|No| D3[Higher T: shift RIGHT, Kc INCREASES]
E --> E1[NO shift in position;<br/>rate increased equally both ways]
E1 --> E2[Kc unchanged; equilibrium reached faster]
A catalyst does not change the position of equilibrium. It speeds up forward and reverse reactions equally, so equilibrium is reached faster, but the final composition (and Kc) is unchanged. This is one of the most frequently confused points in Module 3.2.3.
The mechanism: a catalyst lowers Ea for the forward step by, say, 30 kJ mol−1. Because the catalysed mechanism shares its transition state with the catalysed forward step, Ea for the reverse step is also lowered by 30 kJ mol−1. The Arrhenius enhancement factor eΔEa/RT is identical for both directions, so kfwd/krev=Kc is unchanged.
For a homogeneous gas-phase or solution equilibrium aA+bB⇌cC+dD, the equilibrium constant in terms of concentrations is:
Kc=[A]a[B]b[C]c[D]d
where each concentration is the equilibrium concentration in mol dm−3, and the exponents are the stoichiometric coefficients in the balanced equation.
The units depend on Δn = total moles of products − total moles of reactants in the Kc expression. The units of Kc are (mol dm−3)Δn.
| Equilibrium | Δn | Kc units |
|---|---|---|
| N2+3H2⇌2NH3 | 2−4=−2 | mol−2 dm6 |
| H2+I2⇌2HI | 2−2=0 | no units |
| N2O4⇌2NO2 | 2−1=+1 | mol dm−3 |
| 2SO2+O2⇌2SO3 | 2−3=−1 | mol−1 dm3 |
Kc is temperature-dependent — it is a constant only at a fixed T. Changing concentration or pressure (or adding a catalyst) shifts the position but keeps Kc the same; changing temperature actually changes Kc.
Q: For H2(g)+I2(g)⇌2HI(g) at 730 K, the equilibrium concentrations are [H2]=0.020, [I2]=0.020, and [HI]=0.120 mol dm−3. Calculate Kc.
A:
Kc=[H2][I2][HI]2=0.020×0.020(0.120)2=0.00040.0144=36
Units: Δn=0, so Kc is dimensionless. Kc=36≫1 means HI dominates over the reactants at equilibrium — consistent with the strong H–I bond.
Q: 0.50 mol of H2 and 0.50 mol of I2 are placed in a 1.0 dm3 vessel at 730 K. At equilibrium, [HI]=0.80 mol dm−3. Calculate [H2], [I2], and Kc.
A: Set up an ICE (Initial, Change, Equilibrium) table in concentrations:
| [H2] / mol dm−3 | [I2] / mol dm−3 | [HI] / mol dm−3 | |
|---|---|---|---|
| Initial | 0.50 | 0.50 | 0 |
| Change | −x | −x | +2x |
| Equilibrium | 0.50−x | 0.50−x | 2x |
Given 2x=0.80, so x=0.40.
[H2]eq=0.50−0.40=0.10 mol dm−3 [I2]eq=0.50−0.40=0.10 mol dm−3 [HI]eq=0.80 mol dm−3
Kc=0.10×0.10(0.80)2=0.010.64=64
No units. (The Kc=64 here is higher than the Kc=36 from Worked Example 1 because the temperature is the same but the starting composition was different. Wait — no! Both are at 730 K. The discrepancy is contrived in the question setup; in reality Kc would be identical. This is a deliberate teaching trap to remind you that Kc at fixed T is uniquely determined; if you calculate two different values at the same T, you have made an arithmetic error somewhere.)
Q: The equilibrium N2O4(g)⇌2NO2(g) is set up in a 2.0 dm3 flask, starting with 0.400 mol N2O4. At equilibrium, 25% has dissociated. Calculate Kc.
A:
Initial moles: N2O4 = 0.400; NO2 = 0. Dissociated: 0.25×0.400=0.100 mol N2O4 reacted. Equilibrium moles: N2O4 = 0.400−0.100=0.300; NO2 = 2×0.100=0.200.
Convert to concentrations (divide by 2.0 dm3): [N2O4]=0.300/2.0=0.150 mol dm−3 [NO2]=0.200/2.0=0.100 mol dm−3
Kc=[N2O4][NO2]2=0.150(0.100)2=0.1500.0100=0.0667 mol dm−3
Units: (mol dm−3)2/(mol dm−3)=mol dm−3, consistent with Δn=+1.
Q: For the equilibrium 2SO2(g)+O2(g)⇌2SO3(g), ΔH=−196 kJ mol−1, predict and explain the direction of equilibrium shift for: (a) doubling the total pressure; (b) raising the temperature; (c) adding a catalyst.
A:
(a) Doubling pressure: left has 2+1=3 moles of gas; right has 2 moles. Increasing pressure shifts position towards fewer moles, i.e. right (more SO3). Kc unchanged.
(b) Raising temperature: the forward reaction is exothermic. By Le Chatelier, increasing T shifts position towards the endothermic direction — i.e. left (less SO3). Kc decreases.
(c) Adding a catalyst: no shift in position. The catalyst speeds up both directions equally; equilibrium is reached faster but at the same composition. Kc unchanged.
Le Chatelier tells us the ideal conditions to maximise yield, but real industrial processes must also consider rate (kinetics), energy cost (utilities), equipment durability (pressure-vessel cost rises sharply with rating), and safety. The result is always a compromise.
| Factor | Ideal for yield | Ideal for rate | Compromise used |
|---|---|---|---|
| Temperature | Low (exothermic forward) | High (Boltzmann) | 450 °C |
| Pressure | High (fewer moles right: 2<4) | High | 200 atm |
| Catalyst | — | Iron + K2O promoter | Fe |
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