This page is a workout. We take the machinery from the parent note and run it through every kind of mechanism problem an exam can hand you . Before we start, one promise: every symbol is earned. Let me re-anchor the two ideas you actually need.
Intuition What "rate" means, pictured
Imagine a corridor of people trying to get through a series of doors. The rate of the whole crowd getting out is set by the narrowest door — the slowest step. That narrow door is the rate-determining step (RDS) . Everything on this page is: find the narrow door, and describe the crowd waiting at it in terms of things we can actually count.
Two symbols we reuse constantly:
[ X ] and the constant k
[ X ] means "how much of species X is floating around ", measured in moles per litre (mol L − 1 , written M ). Picture a jar: more dots inside = bigger [ X ] .
k is a rate constant — a fixed number for a given step at a given temperature that says "how eager is this collision to succeed?" Big k = fast door; small k = stuck peanut-butter jar.
For an elementary step aA + bB → products , the rate is k [ A ] a [ B ] b . The exponents are the number of each molecule that must collide at once — because probability of a simultaneous meeting multiplies.
Every mechanism problem is one (or a blend) of these cells. Our 9 examples below cover all of them — including a standalone Cell Z that stress-tests the formulas at their edges.
Cell
Scenario class
What makes it tricky
Example
A
Slow step first , no intermediate in it
The "easy" case — read the rate off directly
Ex 1
B
Slow step later , fed by a fast pre-equilibrium
Must eliminate an intermediate via K
Ex 2
C
Intermediate is a reactant that was already used (denominator appears)
Fast equilibrium consuming a reactant, so it lands in the denominator
Ex 3
D
Unimolecular RDS (molecularity 1)
Degenerate "collision" — a single molecule falls apart
Ex 4
E
Termolecular / 3-body apparent order
Order can reach 3; is a true 3-body step realistic?
Ex 5
F
No obvious slow step to Steady-State Approximation
Rate set by build-up/drain balance, not one door
Ex 6
G
Real-world word problem (atmospheric / catalysis)
Translate prose to steps to law
Ex 7
H
Exam twist : given the observed order, pick the valid mechanism
Reverse direction; test candidates
Ex 8
Z
Degenerate/limiting checks : zero concentration, huge/tiny k ratios
Do the formulas stay sane at the edges?
Ex 9
Worked example Example 1 — the clean case
Overall: NO 2 + CO → NO + CO 2
Mechanism:
Step 1 (slow ): NO 2 + NO 2 → NO 3 + NO , rate = k 1 [ NO 2 ] 2
Step 2 (fast): NO 3 + CO → NO 2 + CO 2
Forecast: guess the overall rate law. Tempting answer from stoichiometry: k [ NO 2 ] [ CO ] . Is that right?
Step 1 — Find the narrow door. Step 1 is labelled slow , so it is the RDS.
Why this step? The whole crowd can only leave as fast as the narrowest door lets it. Step 2 is fast, so it never holds anyone up.
Step 2 — Write the RDS rate from its own stoichiometry. Two NO 2 molecules collide, so
Rate = k 1 [ NO 2 ] 2 .
Why this step? Step 1 is elementary, so exponents = number of colliding molecules = 2.
Step 3 — Check for intermediates in the law. NO 3 is an intermediate, but it does not appear in k 1 [ NO 2 ] 2 . Nothing to eliminate.
Why this step? A finished rate law may only contain species we can measure — reactants/products.
Result: Rate = k 1 [ NO 2 ] 2 . Second order in NO 2 , zero order in CO — CO doesn't appear at all!
Verify: Sum the steps: 2 NO 2 + NO 3 + CO → NO 3 + NO + NO 2 + CO 2 . Cancel NO 3 and one NO 2 : NO 2 + CO → NO + CO 2 ✓ matches the overall. Units of k 1 : rate is M s − 1 , [ NO 2 ] 2 is M 2 , so k 1 has M − 1 s − 1 ✓ (a bimolecular constant).
Here we meet the trick that carries the rest of the page: an intermediate sits inside the RDS and we must trade it away.
Figure s01 — a diagram of Example 2. On the left a box holds the reactants NO + Br2 ; a magenta arrow (labelled k 1 , fast) and a violet arrow (labelled k − 1 , fast) of equal length connect it to a middle box holding the intermediate NOBr2 . Equal arrow lengths are the picture of "forward rate = reverse rate", i.e. equilibrium. A thin dotted orange arrow (labelled k 2 , SLOW — the narrow door) leaks NOBr2 + NO onward to the product box 2 NOBr.
Worked example Example 2 — pre-equilibrium elimination
Overall: 2 NO + Br 2 → 2 NOBr
Mechanism:
Step 1 (fast equilibrium ): NO + Br 2 ⇌ NOBr 2 , with k 1 forward, k − 1 reverse
Step 2 (slow ): NOBr 2 + NO → 2 NOBr , rate = k 2 [ NOBr 2 ] [ NO ]
Forecast: what will the order in NO be — 1 or 2? Guess before reading on; we answer it explicitly at the Result.
Step 1 — RDS rate. Step 2 is slow:
Rate = k 2 [ NOBr 2 ] [ NO ] .
Why: the slowest door sets the pace.
Step 2 — Spot the intermediate. NOBr 2 is produced then consumed — we can't buy a bottle of it. It must go.
Why: rate laws may only contain measurable reactants.
Step 3 — Use the fast equilibrium. "Fast forward and reverse" means Step 1 balances itself: forward rate = reverse rate — this is exactly the equal-length arrows in figure s01.
k 1 [ NO ] [ Br 2 ] = k − 1 [ NOBr 2 ] .
Why this tool and not another? Because Step 1 is fast in both directions , it reaches equilibrium long before the slow step drains it — so the equilibrium condition (in-rate = out-rate) holds.
Step 4 — Solve for the intermediate.
[ NOBr 2 ] = k − 1 k 1 [ NO ] [ Br 2 ] .
Why this step? The rate we want (k 2 [ NOBr 2 ] [ NO ] ) still contains the un-measurable [ NOBr 2 ] . We rearrange the equilibrium equation to make [ NOBr 2 ] the subject — that gives us a formula for it built entirely from measurable reactants.
Step 5 — Substitute.
Rate = k 2 ⋅ k − 1 k 1 [ NO ] [ Br 2 ] ⋅ [ NO ] = k − 1 k 1 k 2 [ NO ] 2 [ Br 2 ] .
Why this step? We drop the Step-4 expression into the RDS rate in place of [ NOBr 2 ] , evicting the intermediate. What remains contains only NO and Br 2 — things a lab can measure. Let k obs = k 1 k 2 / k − 1 :
Rate = k obs [ NO ] 2 [ Br 2 ] .
Result: the forecast is answered — second order in NO , not first, because two NO molecules feed the path (one enters the equilibrium, one enters the slow step). Total order 2 + 1 = 3 .
Verify: Sum: NO + Br 2 + NOBr 2 + NO → NOBr 2 + 2 NOBr . Cancel NOBr 2 : 2 NO + Br 2 → 2 NOBr ✓. Units of k obs : rate is M s − 1 and [ NO ] 2 [ Br 2 ] is M 3 , so k obs has M − 2 s − 1 ✓ (consistent with k 1 k 2 / k − 1 : units M − 1 s − 1 ⋅ M − 1 s − 1 / s − 1 = M − 2 s − 1 ✓). Numeric spot-check: if k 1 = 2 , k − 1 = 4 , k 2 = 3 then k obs = 2 ⋅ 3/4 = 1.5 ; with [ NO ] = 0.1 , [ Br 2 ] = 0.2 , Rate = 1.5 ⋅ 0.01 ⋅ 0.2 = 0.003 M s − 1 .
Worked example Example 3 — a reactant hides in the denominator
Ozone decomposition, 2 O 3 → 3 O 2 :
Step 1 (fast equilibrium ): O 3 ⇌ O 2 + O , k 1 , k − 1
Step 2 (slow ): O + O 3 → 2 O 2 , rate = k 2 [ O ] [ O 3 ]
Forecast: the reverse of Step 1 eats O 2 . Will [ O 2 ] end up on top or bottom of the rate law?
Step 1 — RDS rate: Rate = k 2 [ O ] [ O 3 ] .
Step 2 — Intermediate is atomic O . Eliminate it.
Step 3 — Equilibrium condition. Forward = reverse:
k 1 [ O 3 ] = k − 1 [ O 2 ] [ O ] .
Why: the reverse reaction is bimolecular (O 2 meets O ), so its rate carries a [ O 2 ] factor — that is the whole point of this cell.
Step 4 — Solve.
[ O ] = k − 1 [ O 2 ] k 1 [ O 3 ] .
Why this step? The RDS rate still hides the intermediate [ O ] . We rearrange the equilibrium equation to isolate [ O ] ; because [ O 2 ] sat on the reverse side, it is now divided out — it slides into the denominator. That is precisely how a product ends up inhibiting the rate.
Step 5 — Substitute.
Rate = k 2 ⋅ k − 1 [ O 2 ] k 1 [ O 3 ] ⋅ [ O 3 ] = k − 1 k 1 k 2 [ O 2 ] [ O 3 ] 2 .
Why this step? Dropping the Step-4 expression into the RDS rate evicts [ O ] , leaving only measurable O 3 and O 2 . Let k obs = k 1 k 2 / k − 1 :
Rate = k obs [ O 3 ] 2 [ O 2 ] − 1 .
Result: order + 2 in O 3 , order − 1 in O 2 . A negative order — the product O 2 inhibits the reaction, exactly what experiment shows for ozone.
Verify: Sum: O 3 + O + O 3 → O 2 + O + 2 O 2 . Cancel O : 2 O 3 → 3 O 2 ✓. Units of k obs : rate M s − 1 = k obs ⋅ M 2 / M = k obs ⋅ M , so k obs has s − 1 ✓ (matching k 1 k 2 / k − 1 : s − 1 ⋅ M − 1 s − 1 / M − 1 s − 1 = s − 1 ✓). Numeric: k 1 = 6 , k − 1 = 3 , k 2 = 2 ⇒ k obs = 4 ; with [ O 3 ] = 0.1 , [ O 2 ] = 0.5 : Rate = 4 ⋅ 0.01/0.5 = 0.08 M s − 1 .
Worked example Example 4 — a single molecule falls apart
Overall: N 2 O 5 → 2 NO 2 + 2 1 O 2 (simplified). Slow step is unimolecular :
Step 1 (slow ): N 2 O 5 → NO 2 + NO 3 , rate = k 1 [ N 2 O 5 ]
Step 2 (fast): NO 2 + NO 3 → NO 2 + O 2 + NO … (fast follow-ups)
Forecast: "molecularity 1" means how many molecules must meet? What's the order?
Step 1 — RDS rate. Molecularity = 1 : no partner needed, the molecule just shakes itself apart.
Rate = k 1 [ N 2 O 5 ] .
Why this is the degenerate case: a "collision" with zero partners is one molecule reaching enough vibrational energy to break — see Activation Energy and Catalysts . The exponent is 1 , not 0 : doubling [ N 2 O 5 ] doubles the number of molecules that can break per second.
Result: Rate = k 1 [ N 2 O 5 ] — first order .
Verify: Units — rate M s − 1 = k 1 ⋅ M , so k 1 has units s − 1 ✓ (the hallmark of a unimolecular constant). Sanity: at [ N 2 O 5 ] = 0 , Rate = 0 ✓ — nothing to decompose. (Cell Z pushes such edge tests further in Ex 9.)
Worked example Example 5 — how high can order go?
Overall: 2 NO + O 2 → 2 NO 2 . Suppose (hypothetically) a single termolecular step:
Step 1 (slow , 3-body): NO + NO + O 2 → 2 NO 2 , rate = k 1 [ NO ] 2 [ O 2 ]
Forecast: what's the overall order (sum of exponents)? And is a genuine 3-body collision physically likely?
Step 1 — Read the rate. Elementary, molecularity 3:
Rate = k 1 [ NO ] 2 [ O 2 ] , order = 2 + 1 = 3.
Step 2 — Sanity on the physics. Three molecules meeting at the same instant is rare — recall from Collision Theory that even 2-body collisions are the norm and 3-body ones are roughly a thousand times less frequent. So although this gives the right law , chemists prefer the pre-equilibrium route of Example 2 (same law, no improbable triple collision).
Why mention this? An exam may accept either mechanism if both reproduce the observed order-3 law — but asks you to flag which is more realistic .
Result: Rate = k 1 [ NO ] 2 [ O 2 ] , order 3.
Verify: This is exactly the k obs [ NO ] 2 [ O 2 ] form from the parent note's Example 2 — two different mechanisms, same rate law , confirming a rate law can't uniquely prove a mechanism. Units of k 1 : rate M s − 1 = k 1 ⋅ M 3 , so k 1 has M − 2 s − 1 ✓ (a termolecular constant). Numeric: k 1 = 5 , [ NO ] = 0.2 , [ O 2 ] = 0.3 : Rate = 5 ⋅ 0.04 ⋅ 0.3 = 0.06 M s − 1 .
When no step is flagged "slow," the funnel has two similar doors . We use the Steady-State Approximation : a reactive intermediate is made and destroyed so fast that its amount barely changes, so its net rate of change is about zero .
Figure s02 — a graph of the intermediate concentration [ O ] (magenta curve) against time. It climbs steeply from zero, then flattens onto a violet dashed plateau. On the rising part (orange arrow) it is made faster than it is destroyed; on the flat top (navy arrow) making balances destroying, so the slope d [ O ] / d t is essentially zero — that flat top is the steady-state assumption we exploit.
Worked example Example 6 — steady-state derivation
Overall: 2 O 3 → 3 O 2 , but now nothing is labelled slow:
Step 1: O 3 k 1 O 2 + O
Step − 1 : O 2 + O k − 1 O 3
Step 2: O + O 3 k 2 2 O 2
Forecast: what happens to the answer when k 2 [ O 3 ] is tiny compared with k − 1 [ O 2 ] ? Should it collapse to Example 3's answer?
Step 1 — Write the net rate of the intermediate O . It is made by Step 1, destroyed by Steps − 1 and 2 :
d t d [ O ] = k 1 [ O 3 ] − k − 1 [ O 2 ] [ O ] − k 2 [ O ] [ O 3 ] .
Why this tool? No single door is narrow, so we can't just read off one step. Instead we track the flat top of the [ O ] curve in figure s02: it rises, then levels — on that plateau its slope is about zero.
Step 2 — Set it to zero (steady state).
k 1 [ O 3 ] = [ O ] ( k − 1 [ O 2 ] + k 2 [ O 3 ] ) ⇒ [ O ] = k − 1 [ O 2 ] + k 2 [ O 3 ] k 1 [ O 3 ] .
Why this step? The plateau means "made = destroyed", i.e. the whole right-hand side sums to zero. Setting it to zero turns a hard differential equation into a plain algebraic one, which we then rearrange to isolate the un-measurable [ O ] .
Step 3 — Rate of product (via Step 2).
Rate = k 2 [ O ] [ O 3 ] = k − 1 [ O 2 ] + k 2 [ O 3 ] k 1 k 2 [ O 3 ] 2 .
Why this step? Product O 2 is born in Step 2, so its rate is k 2 [ O ] [ O 3 ] ; we substitute the Step-2 expression for [ O ] to evict the intermediate, leaving only measurable species.
Step 4 — Limiting check. If k − 1 [ O 2 ] far exceeds k 2 [ O 3 ] (reverse fast → pre-equilibrium), drop k 2 [ O 3 ] from the denominator:
Rate → k − 1 k 1 k 2 [ O 2 ] [ O 3 ] 2 ,
exactly Example 3 — the steady state is the more general law and the pre-equilibrium is its special case.
Verify: Units: numerator k 1 k 2 [ O 3 ] 2 over denominator k − 1 [ O 2 ] gives (as in Ex 3) an overall M s − 1 ✓. Numeric, general form with k 1 = 6 , k 2 = 2 , k − 1 = 3 , [ O 3 ] = 0.1 , [ O 2 ] = 0.5 :
Rate = 3 ⋅ 0.5 + 2 ⋅ 0.1 6 ⋅ 2 ⋅ 0.01 = 1.7 0.12 ≈ 0.0706 M s − 1 , close to Example 3's 0.08 (they differ only by the extra k 2 [ O 3 ] in the denominator) — sensible ✓.
Worked example Example 7 — enzyme-style bottleneck in words
"An enzyme E grabs a substrate S to form a complex E S very quickly and reversibly; then E S slowly converts to product P , releasing E . Sketch the rate law when substrate is scarce."
Step 1 (fast eq): E + S ⇌ E S , k 1 , k − 1
Step 2 (slow): E S k 2 E + P , rate = k 2 [ E S ]
Forecast: with lots of enzyme and little substrate, do you expect first order in [ S ] ?
Step 1 — RDS rate. Rate = k 2 [ E S ] .
Step 2 — E S is the intermediate. Fast equilibrium of Step 1:
k 1 [ E ] [ S ] = k − 1 [ E S ] ⇒ [ E S ] = k − 1 k 1 [ E ] [ S ] .
Why this step? We rearrange the equilibrium to isolate the un-measurable complex [ E S ] in terms of enzyme and substrate we can actually monitor.
Step 3 — Substitute.
Rate = k − 1 k 1 k 2 [ E ] [ S ] .
Why this step? Dropping the Step-2 expression into the RDS rate evicts [ E S ] . In the scarce-substrate limit the enzyme is mostly free, so [ E ] is nearly a constant [ E ] 0 :
Rate ≈ k ′ [ S ] , k ′ = k − 1 k 1 k 2 [ E ] 0 .
Result: first order in substrate at low [ S ] — the linear low-substrate regime of Enzyme Kinetics (Michaelis–Menten). At high [ S ] the enzyme saturates and the order drops toward 0 (all enzyme busy — the door is jammed open at max flow).
Verify: Low-[ S ] order = 1 , high-[ S ] order = 0 : the two edges of the scenario matrix are captured. Numeric low limit: k 1 = 10 , k − 1 = 2 , k 2 = 5 , [ E ] 0 = 0.01 , [ S ] = 0.1 : k ′ = ( 10 ⋅ 5/2 ) ⋅ 0.01 = 0.25 , so Rate = 0.25 ⋅ 0.1 = 0.025 M s − 1 .
Worked example Example 8 — pick the mechanism that fits the data
Experiment gives Rate = k [ H 2 ] [ ICl ] for H 2 + 2 ICl → I 2 + 2 HCl . Two candidate mechanisms are offered. Which is consistent?
Candidate X: single step H 2 + 2 ICl → products (termolecular). Predicts Rate = k [ H 2 ] [ ICl ] 2 .
Candidate Y:
Step 1 (slow ): H 2 + ICl → HI + HCl , rate = k 1 [ H 2 ] [ ICl ]
Step 2 (fast): HI + ICl → I 2 + HCl
Forecast: which predicted law matches the observed k [ H 2 ] [ ICl ] ?
Step 1 — Predict X's law. Elementary termolecular gives k [ H 2 ] [ ICl ] 2 . Order in ICl = 2 . Does not match (observed is 1).
Why reject: the exponent on ICl is wrong, and 3-body collisions are unlikely anyway.
Step 2 — Predict Y's law. RDS is Step 1, elementary, giving k 1 [ H 2 ] [ ICl ] . Order in ICl = 1 . Matches ✓.
Step 3 — Confirm Y sums correctly. H 2 + ICl + HI + ICl → HI + HCl + I 2 + HCl ; cancel HI : H 2 + 2 ICl → I 2 + 2 HCl ✓.
Result: Mechanism Y is accepted (fits observed law and stoichiometry; no improbable termolecular step).
Verify: Observed law order sum = 1 + 1 = 2 ; Y predicts 2 ✓, X predicts 3 ✗. Numeric with k 1 = 4 , [ H 2 ] = 0.5 , [ ICl ] = 0.2 : Rate = 4 ⋅ 0.5 ⋅ 0.2 = 0.4 M s − 1 .
Worked example Example 9 — do the formulas stay sane at the edges?
Take the pre-equilibrium law from Example 2, Rate = k obs [ NO ] 2 [ Br 2 ] with k obs = k 1 k 2 / k − 1 , and stress it at four edges.
Forecast: guess which edge makes the rate blow up rather than vanish.
Step 1 — Zero reactant. Set [ NO ] = 0 .
Rate = k obs ⋅ 0 2 ⋅ [ Br 2 ] = 0.
Why this step? If a reactant that appears in the law is absent, no path can run — the rate must be exactly zero. It is ✓.
Step 2 — Zero of a species not in the law. In Example 1, set [ CO ] = 0 : Rate = k 1 [ NO 2 ] 2 is unchanged .
Why this step? Zero-order species genuinely don't gate the RDS, so removing them can't slow Step 1. This is the counter-intuitive edge students trip on.
Step 3 — Very fast reverse (k − 1 → ∞ ). In k obs = k 1 k 2 / k − 1 ,
k obs → 0 ⇒ Rate → 0.
Why this step? A furious reverse tears the intermediate apart before the slow step can use it — the equilibrium sits far left, starving Step 2. Vanishing rate is physically right ✓.
Step 4 — Product-inhibited law near zero product. Take Example 3, Rate = k obs [ O 3 ] 2 / [ O 2 ] , and let [ O 2 ] → 0 .
Rate → + ∞.
Why this step? This is the "blow-up" edge from the forecast: a denominator heading to zero sends the rate sky-high. Physically the model breaks here (you never truly have zero O 2 , since Step 1 keeps making it) — a healthy reminder that limiting laws have a domain of validity.
Verify: Edge 1 gives 0 ✓; Edge 2 leaves k 1 [ NO 2 ] 2 untouched ✓; Edge 3 gives 0 ✓ (lim k − 1 → ∞ k 1 k 2 / k − 1 = 0 ); Edge 4 diverges ✓ (lim [ O 2 ] → 0 + k obs [ O 3 ] 2 / [ O 2 ] = + ∞ ). All four match intuition.
Recall When do I use pre-equilibrium vs steady state?
Use pre-equilibrium when a fast reversible step is followed by a clearly slow step (reverse far exceeds forward-drain). Use steady-state when no step is flagged slow, or to be safe — steady-state is the general result that contains pre-equilibrium as a limit.
Recall Which cell does a negative reaction order come from?
Cell C ::: a product (or reactant) that appears in the reverse of a fast equilibrium lands in the denominator , giving a negative order — that species inhibits the reaction.
Mnemonic The two-move dance
"Slowest sets it, intermediates get evicted." Find the RDS, write its law, then evict any intermediate using equilibrium (or steady state) until only measurable species remain.