Study Guides
Reaction Kinetics: Rate Equations and Catalysis
Rate equations, orders of reaction, rate constants, reaction mechanisms, and homogeneous and heterogeneous catalysis, for Cambridge International AS & A Level Chemistry 9701.
- Subject
- Chemistry
- Level
- A LEVEL
- Topic
- Reaction kinetics
- Author
- Marlbridge Academic Team
- Updated
This guide covers subtopics 26.1, Simple rate equations, orders of reaction and rate constants, and 26.2, Homogeneous and heterogeneous catalysts, from Topic 26, Reaction kinetics, of Cambridge International AS & A Level Chemistry 9701, 2025–2027 series. This is A Level content.
Before studying this
This resource assumes collision theory, the Boltzmann distribution and activation energy from Reaction Kinetics: Collision Theory and Catalysis — that AS resource explains why rate changes with conditions; this one adds the quantitative rate equation and mechanism-deduction tools AS explicitly excludes.
Syllabus coverage
CAMBRIDGE INTERNATIONAL AS & A LEVEL CHEMISTRY 9701 — A Level, Topic 26
26.1 Simple rate equations, orders of reaction and rate constants — explaining and using rate equation, order of reaction, overall order, rate constant, half-life, rate-determining step and intermediate; using rate equations of the form rate = k[A]ᵐ[B]ⁿ; deducing order from concentration-time graphs or experimental data; interpreting graphical data; calculating an initial rate; constructing a rate equation; using that a first-order half-life is independent of concentration; calculating a rate constant from initial rates or from half-life; for a multi-step reaction, suggesting a mechanism consistent with the rate equation, predicting order from a mechanism, deducing a rate equation from a mechanism, identifying an intermediate or catalyst, and identifying the rate-determining step; describing qualitatively the effect of temperature on the rate constant.
26.2 Homogeneous and heterogeneous catalysts — explaining that catalysts can be homogeneous or heterogeneous; describing the mode of action of a heterogeneous catalyst (adsorption, bond weakening, desorption), exemplified by iron in the Haber process and Pd/Pt/Rh in catalytic converters; describing the mode of action of a homogeneous catalyst (used in one step, reformed in a later step), exemplified by atmospheric NOₓ catalysing SO₂ oxidation and Fe²⁺/Fe³⁺ in the I⁻/S₂O₈²⁻ reaction.
Rate equations and orders of reaction
A rate equation expresses how reaction rate depends on the concentration of each reactant:
rate = k[A]ᵐ[B]ⁿ
where k is the rate constant, and m and n are the orders of reaction with respect to A and B (each 0, 1 or 2 at this level) — found only from experimental data, never from the stoichiometric equation. The overall order is m + n.
- Zero order (m = 0): changing [A] has no effect on rate; a concentration-time graph for A is a straight line (constant rate of loss).
- First order (m = 1): rate is directly proportional to [A]; doubling [A] doubles the rate.
- Second order (m = 2): rate is proportional to [A]²; doubling [A] quadruples the rate.
Deducing order from initial-rates data.
Worked example. The following initial rates were measured for A + B → products:
| Experiment | [A] / mol dm⁻³ | [B] / mol dm⁻³ | Initial rate / mol dm⁻³ s⁻¹ |
|---|---|---|---|
| 1 | 0.10 | 0.10 | 2.0 × 10⁻³ |
| 2 | 0.20 | 0.10 | 4.0 × 10⁻³ |
| 3 | 0.20 | 0.20 | 1.6 × 10⁻² |
Comparing experiments 1 and 2: [A] doubles, [B] constant, rate doubles (2.0 → 4.0 × 10⁻³) — first order with respect to A.
Comparing experiments 2 and 3: [B] doubles, [A] constant, rate quadruples (4.0 → 16 × 10⁻³) — second order with respect to B.
Rate equation: rate = k[A][B]²; overall order = 1 + 2 = 3.
Using experiment 1 to find k: 2.0 × 10⁻³ = k(0.10)(0.10)², so k = 2.0 × 10⁻³ / (0.10 × 0.010) = 2.0 × 10⁻³ / 1.0 × 10⁻³ = 2.0 mol⁻² dm⁶ s⁻¹
Half-life of a first-order reaction. For a first-order reaction, the time for the concentration to halve (t½) is constant, independent of the starting concentration — a distinctive test for first order directly from a concentration-time graph (equal time intervals for each successive halving). This links to the rate constant by:
k = 0.693 / t½
Worked example. A first-order reaction has t½ = 24 s. Calculate k.
k = 0.693 / 24 = 0.0289 s⁻¹
Effect of temperature on k. Increasing temperature increases the rate constant itself (not just the rate, which can also change with concentration) — this is the quantitative counterpart to the AS-level Boltzmann-distribution explanation: more particles have energy ≥ the activation energy at a higher temperature, which is reflected in a larger k.
Deducing mechanisms from rate equations
For a multi-step reaction, the overall rate equation is determined only by the rate-determining step (the slowest step) and any steps before it — species produced after the rate-determining step don’t appear in the rate equation.
Worked example. The reaction 2NO(g) + Br₂(g) → 2NOBr(g) is proposed to proceed by:
Step 1 (fast, reversible): NO + Br₂ ⇌ NOBr₂
Step 2 (slow): NOBr₂ + NO → 2NOBr
Deduce the rate equation implied by this mechanism, and identify the intermediate.
The rate-determining step is step 2, so the rate equation is based on its reactants: rate = k[NOBr₂][NO]. Since NOBr₂ doesn’t appear in the overall equation, it’s an intermediate, formed in step 1 and consumed in step 2 — its own concentration can be re-expressed using the fast pre-equilibrium of step 1, but at this level it’s enough to identify it and write the rate equation directly in terms of the species present in the rate-determining step and any before it.
This works in reverse too: given an experimental rate equation, a proposed mechanism is only consistent with it if the rate-determining step’s reactants (and only those) match the species in the rate equation. A species appearing in the rate equation with a lower order than its stoichiometric coefficient in the overall equation is a strong sign it’s involved before the rate-determining step, not in it directly.
Homogeneous and heterogeneous catalysts
A catalyst can be homogeneous (same physical state as the reactants, typically forming a genuine intermediate step within the reaction) or heterogeneous (different physical state, typically acting via surface adsorption).
Heterogeneous catalysis proceeds by: adsorption of reactant molecules onto active sites on the catalyst’s surface; bond weakening within the adsorbed molecules as they interact with the surface, lowering the activation energy for the reaction between them; and desorption of the product molecules, freeing the active site for further reactant molecules.
- Iron in the Haber process: N₂ and H₂ adsorb onto the iron surface, where the N≡N and H–H bonds are weakened, allowing them to react to form NH₃, which then desorbs.
- Pd, Pt and Rh in catalytic converters: NO and CO (from car exhaust) adsorb onto the precious-metal surface, where bond weakening allows the reaction 2CO + 2NO → 2CO₂ + N₂ to proceed with a much lower activation energy than the uncatalysed gas-phase reaction, before the products desorb.
Homogeneous catalysis proceeds by the catalyst being consumed in one step of the mechanism and regenerated in a later step — never appearing in the overall balanced equation, but genuinely taking part in the reaction pathway.
- Atmospheric oxides of nitrogen catalysing SO₂ oxidation: NO reacts with O₂ to form NO₂, which then oxidises SO₂ to SO₃ while being reduced back to NO — the NO is regenerated and can catalyse further SO₂ oxidation, contributing to acid rain formation.
- Fe²⁺/Fe³⁺ in the I⁻/S₂O₈²⁻ reaction: the direct reaction between I⁻ and S₂O₈²⁻ is slow, since both ions are negatively charged and repel each other. Fe²⁺ reduces S₂O₈²⁻ to give Fe³⁺ (which, being a cation, doesn’t face that repulsion problem), and Fe³⁺ then oxidises I⁻ back to Fe²⁺ — regenerating the catalyst while avoiding the slow anion-anion step entirely.
Common mistakes
Reading orders of reaction off the balanced stoichiometric equation. Orders can only be found from experimental data (initial rates, concentration-time graphs, or a given mechanism) — never assumed from stoichiometric coefficients.
Forgetting that half-life being constant is unique to first-order reactions. For zero-order or second-order reactions, successive half-lives are not equal — this is precisely why a constant half-life is used as a diagnostic test for first order.
Including a homogeneous catalyst’s formula in the overall equation. By definition, a catalyst is regenerated and cancels out — it appears in the mechanism steps but never in the final balanced equation.
Confusing a reaction intermediate with a catalyst. Both are produced in one step and consumed in another, but an intermediate is produced then consumed later in the same overall reaction sequence (forward-moving); a catalyst is consumed then regenerated, ending the reaction sequence unchanged and available to react again.
Quick revision checklist
- rate = k[A]ᵐ[B]ⁿ; orders found from data only, never from stoichiometry
- Doubling a reactant: rate ×2 (order 1), ×4 (order 2), unchanged (order 0)
- First-order half-life is constant; k = 0.693/t½
- Rate equation reflects the rate-determining step (and any step before it)
- Intermediate: made then consumed within the mechanism, absent from the overall equation
- Heterogeneous catalysis: adsorption → bond weakening → desorption (different phase from reactants)
- Homogeneous catalysis: consumed in one step, regenerated in a later step (same phase as reactants)
Related resources
- Reaction Kinetics: Collision Theory and Catalysis — the qualitative AS foundation this topic quantifies
- Transition Elements: Properties, Complexes and Redox Chemistry — the Fe²⁺/Fe³⁺ catalytic cycle in transition-metal context
- Nitrogen and Sulfur — atmospheric NOₓ chemistry and acid rain this topic’s catalysis example connects to
- Cambridge AS & A Level Chemistry hub
Written against Cambridge International AS & A Level Chemistry 9701, 2025–2027 series. Always check the current syllabus for your examination year.
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