Lesson 4 · 30 min

Reaction mechanisms

An overall equation tells you only the start and the finish; the mechanism is the step-by-step story in between. Integrate every elementary step in the simulator and see how the rate-determining step, the steady state and pre-equilibrium turn a mechanism into a testable rate law.

In this lesson

  • Distinguish elementary steps from the overall reaction and write an elementary step’s rate law from its molecularity
  • Identify intermediates and catalysts in a mechanism and pick out the rate-determining step
  • Derive rate laws from mechanisms with the steady-state and pre-equilibrium approximations
  • Judge whether a mechanism is consistent with the observed rate law

Nitric oxide turns red-brown in air as it becomes nitrogen dioxide: 2 NO+OX2→2 NOX2\ce{2NO} + \ce{O2} \mathrel{\ce{->}} \ce{2NO2}. The measured rate law is r=k[NO]2[OX2]r = k[\ce{NO}]^2[\ce{O2}], which looks like three molecules colliding at once — and three-body collisions are extremely rare. Stranger still, this reaction slows down when heated. The answer lies in its mechanism: the overall equation records only the start and the finish, while in between lie a few simple steps.

Predict first

Below 225 °C the rate law of NOX2+CO→NO+COX2\ce{NO2} + \ce{CO} \mathrel{\ce{->}} \ce{NO} + \ce{CO2} is r=k[NOX2]2r = k[\ce{NO2}]^2, independent of CO. This tells you that:

Pick an answer and lock it in before you look. A wrong guess teaches more than no guess.

Elementary steps and molecularity

An elementary step is a single molecular event. The number of particles that collide in it is its molecularity: unimolecular (one molecule falls apart or rearranges), bimolecular (two particles collide — by far the most common) and termolecular (rare). Only for an elementary step can the rate law be read off the equation — its order equals its molecularity: r=k[A]r = k[\mathrm{A}] for A→P\ce{A} \mathrel{\ce{->}} \ce{P}, r=k[A][B]r = k[\mathrm{A}][\mathrm{B}] for A+B→P\ce{A} + \ce{B} \mathrel{\ce{->}} \ce{P}.

A mechanism is a set of elementary steps that must add up to the overall reaction. A species formed in one step and used up in a later one is an intermediate (such as NOX3\ce{NO3}); one used up at the start and regenerated at the end is a catalyst. The slowest step acts as a bottleneck on the overall rate: the rate-determining step.

d[I]dt≈0  (SS)2 NO⇌kX−1kX1NX2OX2: [NX2OX2]=K1[NO]2 ⇒ r=k2K1[NO]2[OX2]\frac{d[\mathrm{I}]}{dt} \approx 0\ \ \text{(SS)}\qquad\qquad \ce{2NO <=>[k_1][k_{-1}] N2O2}:\ [\ce{N2O2}] = K_1[\ce{NO}]^2 \ \Rightarrow\ r = k_2K_1[\ce{NO}]^2[\ce{O2}]
Left: the steady-state approximation (SS) — a reactive intermediate is consumed as fast as it forms, so its concentration stays low and nearly constant. Right: the pre-equilibrium approximation — a fast, reversible first step stays at equilibrium while a slow second step drains it.
[I][\mathrm{I}]
concentration of the intermediate
K1=k1/k−1K_1 = k_1/k_{-1}
equilibrium constant of the first step
k2k_2
rate constant of the slow step NX2OX2+OX2→2 NOX2\ce{N2O2} + \ce{O2} \mathrel{\ce{->}} \ce{2NO2}

Worked example

2NO + O₂: the rate law from the mechanism

Mechanism: ① 2 NO⇌NX2OX2\ce{2NO} \mathrel{\ce{<=>}} \ce{N2O2} (fast and reversible, k1k_1, k−1k_{-1}); ② NX2OX2+OX2→2 NOX2\ce{N2O2} + \ce{O2} \mathrel{\ce{->}} \ce{2NO2} (slow, k2k_2). Derive the rate law and explain why heating slows the reaction.

Integrating every elementary step · testing the approximations

Mechanism simulator

Overall reaction: 2 NO+OX2→2 NOX2\ce{2NO} + \ce{O2} \mathrel{\ce{->}} \ce{2NO2}

  1. 2 NO⇌kX−1kX1NX2OX2\ce{2NO} \mathrel{\ce{<=>[k_1][k_{-1}]}} \ce{N2O2} bimolecular fast
  2. NX2OX2+OX2→kX22 NOX2\ce{N2O2} + \ce{O2} \mathrel{\ce{->[k_2]}} \ce{2NO2} bimolecular slow

All species (solid = full mechanism; dashed = approximate rate law)

020406080100Time t / s00.20.40.60.81Concentration / M
  • NO
  • O₂
  • N₂O₂
  • NO₂
  • Product from the approximation

The intermediate, magnified (dashed = approximation) — N₂O₂

020406080100Time t / s00.0020.004Concentration / M
Pre-equilibrium approximation r=k2K1[NO]2[OX2],K1=k1k−1r = k_2K_1[\ce{NO}]^2[\ce{O2}],\qquad K_1 = \dfrac{k_1}{k_{-1}}

Condition for the approximation: ratio ≫ 1; now 40

Largest gap between the full mechanism and the approximation: 0.9 %

Step rates at t = 10.0 s
  • 2NO → N₂O₂ 0.502 M s⁻¹
  • N₂O₂ → 2NO 0.494 M s⁻¹
  • N₂O₂ + O₂ → 2NO₂ 0.0088 M s⁻¹

The first step is fast and reversible, the second slow: N₂O₂ stays in equilibrium with NO, [N₂O₂] = K₁[NO]². The overall rate is second order in NO and first order in O₂ — it looks like a three-body collision but is two bimolecular steps. Once k₋₁ is no longer much larger than k₂[O₂], the approximation fails.

No curve here is drawn by hand: each elementary step’s rate is k times its reactant concentrations raised to their molecularity, and all concentrations are integrated with the adaptive Dormand–Prince method (relative error 10⁻⁷). Dashed curves integrate the rate law derived from the steady-state, pre-equilibrium or rate-determining-step approximation on its own. Rate constants are model values chosen for viewing — only their ratios matter. For the real 2NO + O₂ reaction the measured rate constant falls as temperature rises, the signature of a pre-equilibrium mechanism.
Start with the defaults: the dashed curve (pre-equilibrium) sits almost on the solid one, and “Measure the order” gives about 2 for NO and 1 for O₂. Now lower k₋₁ and raise k₂ until the ratio is no longer much greater than 1 — the approximation drifts away. Then switch to “Consecutive steps” and watch the intermediate I rise and fall.

Concept check

Iodide-catalysed decomposition of hydrogen peroxide: ① HX2OX2+IX−→HX2O+IOX−\ce{H2O2} + \ce{I-} \mathrel{\ce{->}} \ce{H2O} + \ce{IO-} (slow); ② HX2OX2+IOX−→HX2O+OX2+IX−\ce{H2O2} + \ce{IO-} \mathrel{\ce{->}} \ce{H2O} + \ce{O2} + \ce{I-} (fast). Here:

Try the calculation

For consecutive steps A→I→P\ce{A} \mathrel{\ce{->}} \ce{I} \mathrel{\ce{->}} \ce{P} with k1=0.50 s−1k_1 = 0.50\ \mathrm{s^{-1}} and k2=5.0 s−1k_2 = 5.0\ \mathrm{s^{-1}}, starting from A only, when does the intermediate I peak? (You can check in the simulator.)

s

Key takeaways

  • For an elementary step, order equals molecularity; an overall rate law must come from experiment or a mechanism.
  • The steps of a mechanism add up to the overall reaction; intermediates are made then used, catalysts used then regenerated.
  • The slowest step is rate-determining; a fast pre-equilibrium brings the species before it into the rate law.
  • Steady-state and pre-equilibrium approximations turn mechanisms into testable rate laws, each within its own limits.
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Data and references

  1. R. Atkinson et al., “Evaluated kinetic and photochemical data for atmospheric chemistry: Volume I”, Atmos. Chem. Phys. 4, 1461–1738 (2004) (NO + NO + O₂).
  2. P. Atkins, J. de Paula, J. Keeler, Atkins’ Physical Chemistry, 11th ed. (2018), Topic 17E–17F (reaction mechanisms, steady state, pre-equilibria).
  3. Chemistry LibreTexts, “Ea and catalysts” (H₂O₂ + I⁻ mechanism and barriers).