Pre-Equilibrium Approximation

Nitric oxide reacts with oxygen to form NO₂ faster when you cool the mixture down. That is backwards from almost every reaction you meet in introductory kinetics, and it is a clue about mechanism. The trick is a fast, reversible step that builds up an intermediate, followed by a slow step that consumes it. This pattern—rapid pre-equilibrium followed by a rate-limiting step—shows up constantly in organic, inorganic, and biochemical mechanisms. It lets chemists convert a messy multi-step mechanism into one clean, testable rate law, and it explains why some reactions have negative or unusual apparent activation energies. This article builds the pre-equilibrium approximation from the reversible-reaction framework you already know. You will see the key assumption stated precisely. Then the composite rate constant is derived step by step. Finally, two worked numerical examples show how to extract elementary rate constants from bulk kinetic data.

Key takeaways
  • Pre-equilibrium applies when a reversible first step is much faster than a subsequent slow step.
  • The fast step is treated as if at equilibrium, so K1=k1/k−1K_1 = k_1/k_{-1} fixes the intermediate's concentration.
  • Substituting into the slow step's rate law gives an observed rate constant that is a composite, kobs=k2K1k_{\text{obs}} = k_2 K_1.
  • The apparent activation energy becomes Ea,obs=Ea,2+ΔH1⊖E_{a,\text{obs}} = E_{a,2} + \Delta H_1^{\ominus}, which can be negative.
  • The approximation is a special, algebraically simpler case of the steady-state approximation.
  • Key idea: when a reversible step re-equilibrates much faster than it is drained by a slow step, its equilibrium constant—not its forward rate constant—controls the overall rate.
The core insight

When an intermediate is formed and destroyed by a fast, reversible step, and consumed only slowly by a subsequent step, the fast step stays essentially at equilibrium throughout the reaction, so the intermediate's concentration is set by K1K_1 rather than by the kinetics of its formation, and the observed rate law is obtained by substituting this equilibrium concentration into the rate expression for the slow, rate-determining step.

The physical picture

Consider a mechanism with an intermediate II formed reversibly from reactants and then consumed to give products:

A+BI→k2P\text{A} + \text{B} \underset{k_{-1}}{\overset{k_1}{\rightleftharpoons}} \text{I} \xrightarrow{k_2} \text{P}

If k−1≫k2k_{-1} \gg k_2, then II reacts back to A + B many times for every one time it proceeds forward to products. The first step effectively equilibrates on a timescale much shorter than the timescale over which P accumulates. Picture two people passing a ball back and forth rapidly (the fast equilibrium) while, only occasionally, someone in the crowd steals it away permanently (the slow step). The stealing rate depends on how many people are holding the ball at any instant—but that population is set by the fast game, not by the thief. This is different from the more general steady-state approximation, which only requires that II's concentration change slowly (small d[I]/dtd[I]/dt), a weaker and broader condition. Pre-equilibrium is the special case where the forward and reverse steps of the first reaction are individually fast compared with the drain step, so equilibrium—not merely a constant low concentration—is achieved. The practical payoff: instead of solving coupled differential equations, you can write K1=[I]/([A][B])K_1 = [\text{I}]/([\text{A}][\text{B}]) directly, because equilibrium algebra replaces kinetic algebra for that step.

Figure
Energy profile: fast reversible step feeding a slow rate-determining step
A + B I (intermediate) TS2 (slow) P TS1 (fast, low barrier) k1, k-1 large k2 small, high barrier
Figure
Concentration vs time: I equilibrates quickly, P grows slowly
time concentration [I], equilibrated fast (flat plateau) [P], grows slowly [A],[B] deplete slowly

The core relations

K1=k1k−1=[I][A][B]K_1 = \frac{k_1}{k_{-1}} = \frac{[\text{I}]}{[\text{A}][\text{B}]}

where K1K_1 is the equilibrium constant of the fast reversible step.

rate=k2[I]=k2K1[A][B]\text{rate} = k_2[\text{I}] = k_2 K_1 [\text{A}][\text{B}]

where k2k_2 is the rate constant of the slow, rate-determining step.

kobs=k2K1=k2k1k−1k_{\text{obs}} = k_2 K_1 = \frac{k_2 k_1}{k_{-1}}

where kobsk_{\text{obs}} is the single composite rate constant seen in an experimental rate law.

Ea,obs=Ea,2+ΔH1⊖E_{a,\text{obs}} = E_{a,2} + \Delta H_1^{\ominus}

where ΔH1⊖=Ea,1−Ea,−1\Delta H_1^{\ominus} = E_{a,1} - E_{a,-1} is the standard reaction enthalpy of the fast pre-equilibrium step.

The core relations — validity condition

k−1≫k2[other reactant]k_{-1} \gg k_2[\text{other reactant}]

where this inequality must hold for the equilibrium assumption to be self-consistent.

Derivation AFrom coupled rate laws to a single composite rate constant

Goal. Starting from the full mass-action rate equations for A + B ⇌ I → P, derive the observed rate law and show it reduces to kobs=k2K1k_{\text{obs}} = k_2 K_1 under the pre-equilibrium condition.

Step 1. Write the exact rate equations. The intermediate I is formed and consumed by three elementary steps, so

d[I]dt=k1[A][B]−k−1[I]−k2[I]\frac{d[\text{I}]}{dt} = k_1[\text{A}][\text{B}] - k_{-1}[\text{I}] - k_2[\text{I}]

This is exact; no approximation has been made yet.

Step 2. Compare the two loss channels for I. The intermediate disappears either by reverting to A + B (rate constant k−1k_{-1}) or by moving on to product (rate constant k2k_2). The pre-equilibrium condition is precisely the statement

k−1≫k2k_{-1} \gg k_2

so that reversion back to reactants happens vastly more often than conversion to product. Physically, I samples the fast equilibrium many times before it "leaks" toward P.

Step 3. Impose quasi-equilibrium on the fast step. Because loss through k−1k_{-1} dominates the right-hand side, the fast forward and reverse fluxes very nearly cancel at every instant:

k1[A][B]≈k−1[I]k_1[\text{A}][\text{B}] \approx k_{-1}[\text{I}]

This is stronger than steady state (d[I]/dt≈0d[\text{I}]/dt \approx 0 overall); here the two large terms cancel each other while the small k2[I]k_2[\text{I}] term is neglected in comparison, consistent with Step 2.

Step 4. Solve for the intermediate's concentration. Rearranging Step 3,

[I]≈k1k−1[A][B]=K1[A][B][\text{I}] \approx \frac{k_1}{k_{-1}}[\text{A}][\text{B}] = K_1[\text{A}][\text{B}]

This says [I] tracks the instantaneous concentrations of A and B exactly as an equilibrium constant would predict, even while A and B are slowly being consumed overall.

Step 5. Insert into the rate law for product formation. The rate of appearance of P is controlled only by the slow step,

d[P]dt=k2[I]=k2K1[A][B]\frac{d[\text{P}]}{dt} = k_2[\text{I}] = k_2 K_1 [\text{A}][\text{B}]

Step 6. Identify the composite rate constant. Comparing with an experimental second-order rate law, rate =kobs[A][B]= k_{\text{obs}}[\text{A}][\text{B}], gives directly

kobs=k2K1=k2k1k−1\boxed{k_{\text{obs}} = k_2 K_1 = \dfrac{k_2 k_1}{k_{-1}}}

Step 7. Translate into activation energies. Writing each rate constant in Arrhenius form, ki=Aie−Ea,i/RTk_i = A_i e^{-E_{a,i}/RT}, and K1=e−ΔG1⊖/RTK_1 = e^{-\Delta G_1^{\ominus}/RT} with ΔG1⊖≈ΔH1⊖−TΔS1⊖\Delta G_1^{\ominus} \approx \Delta H_1^{\ominus} - T\Delta S_1^{\ominus}, taking d(ln⁡kobs)/dTd(\ln k_{\text{obs}})/dT term by term yields

Ea,obs=Ea,2+ΔH1⊖E_{a,\text{obs}} = E_{a,2} + \Delta H_1^{\ominus}

If the pre-equilibrium is exothermic enough (ΔH1⊖\Delta H_1^{\ominus} sufficiently negative), Ea,obsE_{a,\text{obs}} can even become negative, so the overall reaction slows down as temperature rises—exactly the anomaly seen in 2NO+O2→2NO22\text{NO} + \text{O}_2 \rightarrow 2\text{NO}_2.

Worked examples

Example 1 — Extracting kobsk_{\text{obs}} from elementary constants (foundational). The gas-phase reaction 2NO+O2→2NO22\text{NO} + \text{O}_2 \rightarrow 2\text{NO}_2 is believed to proceed by

NO+NON2O2,N2O2+O2→k22NO2\text{NO} + \text{NO} \underset{k_{-1}}{\overset{k_1}{\rightleftharpoons}} \text{N}_2\text{O}_2, \qquad \text{N}_2\text{O}_2 + \text{O}_2 \xrightarrow{k_2} 2\text{NO}_2

Suppose at 300 K the elementary rate constants are k1=1.2×109 dm3mol−1s−1k_1 = 1.2\times10^{9}\ \text{dm}^3\text{mol}^{-1}\text{s}^{-1}, k−1=4.0×109 s−1k_{-1} = 4.0\times10^{9}\ \text{s}^{-1}, and k2=3.0×106 dm3mol−1s−1k_2 = 3.0\times10^{6}\ \text{dm}^3\text{mol}^{-1}\text{s}^{-1}. Step 1: check the pre-equilibrium condition. We need k−1≫k2×k_{-1} \gg k_2 \times (typical [O₂]). With [O₂] ~ 1 mol dm⁻³ or less under normal lab conditions, k2[O2]≤3.0×106 s−1k_2[\text{O}_2] \le 3.0\times10^{6}\ \text{s}^{-1}, which is indeed far smaller than k−1=4.0×109 s−1k_{-1} = 4.0\times10^{9}\ \text{s}^{-1} (ratio ~1300). The approximation is well justified. Step 2: compute K1K_1.

K1=k1k−1=1.2×1094.0×109=0.30 dm3mol−1K_1 = \frac{k_1}{k_{-1}} = \frac{1.2\times10^{9}}{4.0\times10^{9}} = 0.30\ \text{dm}^3\text{mol}^{-1}

Step 3: compute kobsk_{\text{obs}}.

kobs=k2K1=(3.0×106 dm3mol−1s−1)(0.30 dm3mol−1)=9.0×105 dm6mol−2s−1k_{\text{obs}} = k_2 K_1 = (3.0\times10^{6}\ \text{dm}^3\text{mol}^{-1}\text{s}^{-1})(0.30\ \text{dm}^3\text{mol}^{-1}) = 9.0\times10^{5}\ \text{dm}^6\text{mol}^{-2}\text{s}^{-1}

Step 4: sanity check units. The overall rate law is rate =kobs[NO]2[O2]= k_{\text{obs}}[\text{NO}]^2[\text{O}_2], third order overall, so kobsk_{\text{obs}} must carry units of dm6mol−2s−1\text{dm}^6\text{mol}^{-2}\text{s}^{-1}—consistent with what we obtained. This matches the experimentally observed third-order rate law for this reaction (second order in NO, first order in O₂), and the magnitude ∼106 dm6mol−2s−1\sim10^{6}\ \text{dm}^6\text{mol}^{-2}\text{s}^{-1} is the right order for a termolecular-looking gas reaction proceeding through a bound intermediate.

Example 2 — Working backward: apparent activation energy (applied, harder). For the same mechanism, experiments give the elementary Arrhenius parameters: Ea,1=0 kJ mol−1E_{a,1} = 0\ \text{kJ mol}^{-1} (barrierless radical-radical association), Ea,−1=21 kJ mol−1E_{a,-1} = 21\ \text{kJ mol}^{-1} (N₂O₂ bond dissociation), and Ea,2=25 kJ mol−1E_{a,2} = 25\ \text{kJ mol}^{-1}. An experimentalist measures kobsk_{\text{obs}} at two temperatures and wants to predict the apparent activation energy without measuring a full Arrhenius plot. Step 1: find ΔH1⊖\Delta H_1^{\ominus}.

ΔH1⊖=Ea,1−Ea,−1=0−21 kJ mol−1=−21 kJ mol−1\Delta H_1^{\ominus} = E_{a,1} - E_{a,-1} = 0 - 21\ \text{kJ mol}^{-1} = -21\ \text{kJ mol}^{-1}

This is negative, confirming that dimerization of NO to N₂O₂ is exothermic, as expected for bond formation. Step 2: apply the composite activation energy relation.

Ea,obs=Ea,2+ΔH1⊖=25 kJ mol−1+(−21 kJ mol−1)=4 kJ mol−1E_{a,\text{obs}} = E_{a,2} + \Delta H_1^{\ominus} = 25\ \text{kJ mol}^{-1} + (-21\ \text{kJ mol}^{-1}) = 4\ \text{kJ mol}^{-1}

Step 3: interpret and cross-check against a known fact. Ea,obs=4 kJ mol−1E_{a,\text{obs}} = 4\ \text{kJ mol}^{-1} is small and positive here—but note that with only slightly more exothermic pre-equilibrium (say ΔH1⊖=−30 kJ mol−1\Delta H_1^{\ominus} = -30\ \text{kJ mol}^{-1}), Ea,obsE_{a,\text{obs}} would flip negative. This is exactly the experimentally documented behavior of 2NO+O2→2NO22\text{NO}+\text{O}_2 \rightarrow 2\text{NO}_2: its rate constant decreases modestly as temperature increases, corresponding to a small negative observed activation energy in the range −4-4 to −6 kJ mol−1-6\ \text{kJ mol}^{-1} depending on the data set used, a hallmark signature that a pre-equilibrium step lies upstream of the true rate-determining step. Step 4: quantify the temperature sensitivity. Using kobs(T2)/kobs(T1)=exp⁡[−Ea,obsR(1T2−1T1)]k_{\text{obs}}(T_2)/k_{\text{obs}}(T_1) = \exp\left[-\dfrac{E_{a,\text{obs}}}{R}\left(\dfrac{1}{T_2}-\dfrac{1}{T_1}\right)\right] with Ea,obs=4000 J mol−1E_{a,\text{obs}} = 4000\ \text{J mol}^{-1}, going from 280 K to 320 K gives

ln⁡kobs(320)kobs(280)=−40008.314(1320−1280)=−481.3×(−4.46×10−4)=0.215\ln\frac{k_{\text{obs}}(320)}{k_{\text{obs}}(280)} = -\frac{4000}{8.314}\left(\frac{1}{320}-\frac{1}{280}\right) = -481.3 \times (-4.46\times10^{-4}) = 0.215

so kobsk_{\text{obs}} increases by only about 24% over that 40 K range—a far weaker temperature dependence than a normal single-step reaction with Ea∼50E_a \sim 50–100 kJ mol−1100\ \text{kJ mol}^{-1} would show, confirming the diagnostic value of a small or negative Ea,obsE_{a,\text{obs}}.

Limiting cases & common traps

SituationWhat happens
k−1≫k2k_{-1} \gg k_2Pre-equilibrium valid; use kobs=k2K1k_{\text{obs}} = k_2K_1
k−1∼k2k_{-1} \sim k_2 or k−1≪k2k_{-1} \ll k_2Pre-equilibrium fails; use the full steady-state treatment instead
ΔH1⊖\Delta H_1^{\ominus} strongly negativeEa,obsE_{a,\text{obs}} can become negative; rate falls as TT rises
Reactant concentration very high, raising the effective drain rate k2[X]k_2[\text{X}]Can violate k−1≫k2[X]k_{-1}\gg k_2[\text{X}] even if k−1≫k2k_{-1}\gg k_2 alone looked fine
Only one elementary rate constant knownCannot get kobsk_{\text{obs}}; need k1k_1, k−1k_{-1}, and k2k_2, or K1K_1 and k2k_2

The chemist behind it

The pre-equilibrium idea grew out of early twentieth-century efforts to rationalize rate laws that did not match simple bimolecular collision pictures, particularly reactions with fractional or unusual orders and anomalous temperature dependence. Physical chemists studying nitrogen oxide chemistry and ester hydrolysis mechanisms in the 1920s–1930s needed a way to reconcile fast acid-base or association equilibria with a separate slow chemical step, and the algebraic shortcut of substituting an equilibrium constant into a rate law became a standard tool taught alongside the steady-state method developed at the same time.

Origins · 1 minVictor Henri and how this was discovered
VH
Victor Henri
1872–1940 · pioneered treating enzyme-substrate binding as a rapid pre-equilibrium, laying groundwork for Michaelis-Menten kinetics

Ask the tutor: How does the pre-equilibrium approximation simplify into the Michaelis-Menten rate law when an enzyme's substrate-binding step is fast?

How is pre-equilibrium different from the steady-state approximation?

Steady state assumes only that d[I]/dt≈0d[\text{I}]/dt \approx 0 overall—the intermediate's concentration is small and roughly constant, but the forward and reverse fluxes of the first step need not individually dominate. Pre-equilibrium is stricter: it requires k−1≫k2k_{-1} \gg k_2, so the first step's forward and reverse rates nearly cancel independently of the slow step. Every pre-equilibrium result can be derived as a limiting case of the full steady-state expression, but not every steady-state system satisfies the pre-equilibrium condition.

Why can the apparent activation energy be negative?

The composite rate constant kobs=k2K1k_{\text{obs}} = k_2K_1 combines a genuine Arrhenius rate constant k2k_2 with an equilibrium constant K1K_1, which itself falls with temperature if the pre-equilibrium step is exothermic (van 't Hoff behavior). If that fall is steeper than the rise in k2k_2, the product kobsk_{\text{obs}} decreases with temperature overall, mathematically equivalent to a negative Ea,obs=Ea,2+ΔH1⊖E_{a,\text{obs}} = E_{a,2}+\Delta H_1^{\ominus}. This is a real, measurable phenomenon, not an artifact.

Can pre-equilibrium apply to more than two steps?

Yes. If several fast, reversible steps precede one slow, rate-determining step, each fast equilibrium contributes its own equilibrium constant to the composite expression, and kobsk_{\text{obs}} becomes a product of the slow step's rate constant with all the preceding KiK_i values. This generalization is exactly how enzyme kinetics treats multi-step substrate binding before catalysis, and how acid-catalyzed mechanisms treat rapid protonation before a slow bond-breaking step.

How do I know experimentally that a mechanism follows pre-equilibrium rather than a single elementary step?

Key signatures include a rate law whose order does not match simple collision theory (for example, third order overall from formally bimolecular steps), an unusually small or negative apparent activation energy, and successful independent measurement of K1K_1 (from spectroscopy or equilibrium studies) that, combined with an independently measured k2k_2, reproduces the observed kobsk_{\text{obs}}. Isotope-exchange experiments on the proposed intermediate provide further supporting evidence.

Where does pre-equilibrium lead next in kinetics?

The same logic—fast reversible binding followed by a slow catalytic step—underlies the Michaelis-Menten treatment of enzyme kinetics, where substrate binding to the enzyme is often (though not always) fast compared with the catalytic turnover step. It also connects to transition-state theory, which treats the formation of the activated complex itself as a quasi-equilibrium with the reactants, extending the same algebraic trick to the rate-determining step itself.

Before this

Where this leads