Chemical Equilibria
Revise Chemical Equilibria for Chemistry (IAL) — revision notes and instant AI marking. Free to start.
Chemical Equilibria
Big idea: when a reversible reaction reaches equilibrium, there's a fixed "scorecard" ratio of products to reactants — called the equilibrium constant — and that number only changes if you change the temperature. Everything else (concentration, pressure, catalysts) can shift the equilibrium's *position*, but never the constant itself.
Summary — What This Chapter Covers
- Kc — the equilibrium constant written in terms of concentrations (mol dm⁻³), used for reactions in solution.
- Kp — the equilibrium constant written in terms of partial pressures (Pa or kPa), used for gaseous reactions.
- Solids (and liquids, for Kp) are left out of equilibrium expressions entirely.
- Calculating Kc or Kp often needs an ICE table (Initial, Change, Equilibrium) to find missing quantities.
- Kp calculations sometimes require converting moles → mole fraction → partial pressure first.
- Only a change in temperature changes the value of Kc or Kp. Concentration, pressure, and catalysts shift the position of equilibrium but leave K unchanged.
- Entropy links to equilibrium through
ΔStotal = R ln K— a big K means the reaction is strongly product-favoured entropically.
1. The Equilibrium Constant, Kc
1.1 Writing the Kc Expression
For any reversible reaction that has settled into equilibrium, we can write an expression that links the equilibrium constant to how much of each substance is hanging around. For a general reaction:
the equilibrium constant expression is:
Think of it like a recipe ratio at the finish line: once the reaction stops changing overall (even though forward and backward reactions are still happening — it's dynamic equilibrium), you measure how much of everything is present and plug it into this fraction.
Write the Kc expression for: Ag⁺(aq) + Fe²⁺(aq) ⇌ Ag(s) + Fe³⁺(aq)
Answer:
Notice Ag(s) is completely missing — it's a solid, so it never appears in the expression at all, not even as a "1".
1.2 Calculating Kc from Moles and Volume
Exam questions rarely hand you concentrations directly — instead they usually give you the number of moles of each substance at equilibrium plus the total volume of the mixture. You need to convert moles into concentration first:
CH₃COOH(l) + C₂H₅OH(l) ⇌ CH₃COOC₂H₅(l) + H₂O(l)
500 cm³ of the equilibrium mixture contains 0.235 mol ethanoic acid, 0.035 mol ethanol, 0.182 mol ethyl ethanoate, and 0.182 mol water. Find Kc.
Step 1 — concentrations (divide each by 0.500 dm³):
- [CH₃COOH] = 0.235 / 0.500 = 0.470 mol dm⁻³
- [C₂H₅OH] = 0.035 / 0.500 = 0.070 mol dm⁻³
- [CH₃COOC₂H₅] = 0.182 / 0.500 = 0.364 mol dm⁻³
- [H₂O] = 0.182 / 0.500 = 0.364 mol dm⁻³
Step 2 — expression: Kc = [H₂O][CH₃COOC₂H₅] ÷ ([C₂H₅OH][CH₃COOH])
Step 3 — substitute: Kc = (0.364 × 0.364) ÷ (0.070 × 0.470) = 4.03
Step 4 — units: every unit is mol dm⁻³, two on top and two on bottom, so they all cancel — Kc has no units here.
CH₃COOC₂H₅(l) + H₂O(l) ⇌ CH₃COOH(l) + C₂H₅OH(l)
0.1000 mol ethyl ethanoate + 0.1000 mol water, made up to 1.00 dm³. At equilibrium, 0.0654 mol water remains.
| CH₃COOC₂H₅ | H₂O | CH₃COOH | C₂H₅OH | |
|---|---|---|---|---|
| Initial | 0.1000 | 0.1000 | 0 | 0 |
| Change | −0.0346 | −0.0346 | +0.0346 | +0.0346 |
| Equilibrium | 0.0654 | 0.0654 | 0.0346 | 0.0346 |
Water dropped from 0.1000 to 0.0654, a change of −0.0346 mol. Because the ratio is 1:1:1:1, every other species changes by the same amount (0.0346), just in the direction the equation dictates.
Kc = (0.346 × 0.346) ÷ (0.654 × 0.654) = 0.28 (no units — they all cancel)
2. The Equilibrium Constant, Kp
Kp is basically Kc's twin for gas-phase reactions — instead of concentrations, we use partial pressures (the pressure each individual gas would exert if it alone filled the container).
CaCO₃(s) ⇌ CaO(s) + CO₂(g), the whole expression collapses down to just
Kp = pCO₂.
2SO₂(g) + O₂(g) ⇌ 2SO₃(g), with p(SO₂) = 1.0×10⁶ Pa, p(O₂) = 7.0×10⁶ Pa, p(SO₃) = 8.0×10⁶ Pa.
Kp = p²(SO₃) ÷ [p²(SO₂) × p(O₂)] = (8.0×10⁶)² ÷ [(1.0×10⁶)² × (7.0×10⁶)]
Kp = 9.1 × 10⁻⁶ Pa⁻¹
Units: Pa² ÷ (Pa² × Pa) = Pa⁻¹ — always work these out from the raw expression, don't guess.
2.1 When You're Only Given Moles and Total Pressure
Sometimes you don't get partial pressures directly — instead you're given the number of moles of each gas at equilibrium and the total pressure of the container. You need two extra steps first:
- Mole fraction of each gas = (moles of that gas) ÷ (total moles of all gases)
- Partial pressure of each gas = (mole fraction) × (total pressure)
H₂(g) + I₂(g) ⇌ 2HI(g) at 600 K. Moles at equilibrium: H₂ = 1.71×10⁻³, I₂ = 2.91×10⁻³, HI = 1.65×10⁻². Total pressure = 100 kPa.
Step 1 — total moles: 1.71×10⁻³ + 2.91×10⁻³ + 1.65×10⁻² = 2.112×10⁻²
Step 2 — mole fractions: H₂ = 0.0810, I₂ = 0.1378, HI = 0.7813
Step 3 — partial pressures (× 100 kPa): H₂ = 8.10 kPa, I₂ = 13.78 kPa, HI = 78.13 kPa
Step 4 — Kp expression: Kp = p²(HI) ÷ [p(H₂) × p(I₂)]
Step 5 — substitute: Kp = 78.13² ÷ (8.10 × 13.78) = 54.7
Step 6 — units: Pa² ÷ (Pa × Pa) — all units cancel, so Kp has no units here.
3. Equilibrium Constant & Changing Conditions
This is the section students trip up on most, so let's be crystal clear about the difference between two things that sound similar but aren't:
- Position of equilibrium — which side (reactants or products) currently has more "stuff" in it. This shifts around with concentration, pressure, and temperature changes (think Le Chatelier).
- Equilibrium constant (K) — the actual numerical value of that products-over-reactants ratio. This is a fixed number for a given reaction at a given temperature, and only temperature can change it.
3.1 Effect of Temperature
| Change | How the equilibrium shifts |
|---|---|
| Increase in temperature | Shifts in the endothermic direction, to absorb the extra heat and reverse the change |
| Decrease in temperature | Shifts in the exothermic direction, to release heat and reverse the change |
For a reaction that's exothermic in the forward direction: raising the temperature pushes the equilibrium from right back to left (favouring reactants), so the ratio [products]/[reactants] gets smaller — meaning K decreases.
For an endothermic forward reaction: raising the temperature pushes equilibrium further right (favouring products), so [products]/[reactants] gets bigger — meaning K increases.
3.2 Effect of Pressure
Pressure changes only matter for reactions involving gases.
| Change | How the equilibrium shifts |
|---|---|
| Increase in pressure | Shifts towards the side with the smaller number of gas moles (to reduce pressure again) |
| Decrease in pressure | Shifts towards the side with the larger number of gas moles (to increase pressure again) |
Crucially: neither Kc nor Kp is affected by pressure changes. The system shifts to a brand new equilibrium position, but when you recalculate K from the new concentrations or partial pressures, you get the exact same number as before. It's the same idea as adding more of one reactant to a Kc equilibrium in solution — the position moves, but K stays put.
3.3 Effect of a Catalyst
A catalyst speeds up the forward and reverse reactions by exactly the same factor. That means the system reaches equilibrium faster, but it arrives at the same position and the same value of K it would have reached anyway, just quicker. Catalysts never appear in the equilibrium expression and never change K.
AB(aq) + CD(aq) ⇌ AC(aq) + BD(aq), ΔH = +180 kJ mol⁻¹. Which factors would change the value of Kc?
Answer: Only a change in temperature. Adding a catalyst speeds up reaching equilibrium but doesn't move its position or change Kc. Changing concentration would shift the position but the system would settle back to the same Kc.
4. Equilibrium Constant & Temperature — The Mechanics
It helps to actually watch the numbers move, not just memorise the rule. Take the endothermic decomposition of hydrogen iodide:
with Kc = [H₂][I₂] ÷ [HI]². As temperature increases:
- [H₂] and [I₂] increase (more HI breaks down)
- [HI] decreases
- Top of the fraction goes up, bottom goes down → Kc increases
with Kc = [SO₃]² ÷ ([SO₂]²[O₂]). As temperature increases:
- [SO₃] decreases
- [SO₂] and [O₂] increase
- Top goes down, bottom goes up → Kc decreases
5. Equilibrium Constant & Entropy
This links back to thermodynamics: every spontaneous change has a positive total entropy change (ΔStotal > 0). The total entropy change is made of two parts:
ΔSsys barely shifts with temperature (unless a state changes), but ΔSsurr shifts a lot, because it depends directly on temperature:
CaCO₃(s) → CaO(s) + CO₂(g), ΔH = +177.9 kJ mol⁻¹, ΔSsys = +160.4 J K⁻¹ mol⁻¹.
At 293 K (20°C):
ΔSsurr = −177,900 ÷ 293 = −607.2 J K⁻¹ mol⁻¹
ΔStotal = 160.4 + (−607.2) = −446.8 J K⁻¹ mol⁻¹ → negative → NOT spontaneous
At 1173 K (900°C):
ΔSsurr = −177,900 ÷ 1173 = −151.7 J K⁻¹ mol⁻¹
ΔStotal = 160.4 + (−151.7) = +8.7 J K⁻¹ mol⁻¹ → positive → spontaneous!
This is exactly why limestone only decomposes into quicklime when you heat it strongly in a kiln.
5.1 Why Equilibrium Reactions Are Special
In a normal one-way reaction, ΔStotal just needs to be positive to go forward. But an equilibrium reaction is reversible — it can be reached from either the pure reactant side or the pure product side. That means both the forward and backward journeys towards the equilibrium mixture must have positive ΔStotal (both are spontaneous moves towards the middle).
Picture entropy plotted against the % composition of a gas mixture (like N₂O₄ ⇌ 2NO₂). The entropy curve peaks somewhere in the middle — that peak is the equilibrium mixture. Moving from pure N₂O₄ towards that peak increases entropy (spontaneous). Moving from pure NO₂ towards that peak also increases entropy (also spontaneous). But once you're sitting at the peak, moving further in either direction would actually decrease total entropy — which is why the reaction doesn't run to completion either way. It just sits at the top of the hill.
5.2 Connecting Entropy to K
At the exact equilibrium point, the forward and backward entropy changes cancel out to zero. This gives us a direct link between total entropy and the equilibrium constant:
Rearranged to calculate K directly from a known entropy change:
As a rough guide (not a strict rule): a very large K suggests the equilibrium position sits heavily towards the products (right-hand side), while a very small K suggests it sits heavily towards the reactants (left-hand side).
What to Memorise
Concepts Checklist
Exam Tips & Common Mistakes
- 3. Equilibrium Constant & Changing Conditions
- 4. Equilibrium Constant & Temperature — The Mechanics
- 5. Equilibrium Constant & Entropy
- Exam Tips & Common Mistakes
Read the full Chemical Equilibria notes free
That's the preview — create a free account to read the rest, plus flashcards and practice questions with instant AI marking. No credit card.
Unlock the full notes free →