Represent a multistep process with an overall equilibrium expression, using the constituent K expressions for each individual reaction.
Three algebraic rules, plus one clarification:
Compare to Hess's law (6.9) — the structure is the same but the operation is different:
| Operation | ΔH | K |
|---|---|---|
| Reverse | change sign | take reciprocal |
| Multiply by c | multiply by c | raise to power c |
| Add reactions | add ΔH values | multiply K values |
The pattern is that anything additive for ΔH is multiplicative for K. That is not a coincidence: ΔG° = −RT ln K, and a logarithm turns products into sums.
Where this shows up: the Ka of a polyprotic acid's overall ionization is the product of the stepwise Ka values, and Ka × Kb = Kw for a conjugate pair (8.3) is exactly this rule applied to two reactions that sum to the autoionization of water.
Given (1) 2 NO(g) ⇌ N₂(g) + O₂(g) K₁ = 1.0 × 10³⁰ (2) 2 NO(g) + O₂(g) ⇌ 2 NO₂(g) K₂ = 6.4 × 10⁹ calculate K for N₂(g) + 2 O₂(g) ⇌ 2 NO₂(g).
Target: N₂ + 2 O₂ ⇌ 2 NO₂
Place N₂: it must be a reactant, but in (1) it is a product. Reverse (1):
N₂(g) + O₂(g) ⇌ 2 NO(g) K = 1/K₁ = 1.0 × 10⁻³⁰
Place NO₂: equation (2) already has it as a product with coefficient 2. Use as is:
2 NO(g) + O₂(g) ⇌ 2 NO₂(g) K = 6.4 × 10⁹
Add the two equations:
N₂ + O₂ + 2 NO + O₂ ⇌ 2 NO + 2 NO₂
NO cancels, and the two O₂ combine:
N₂ + 2 O₂ ⇌ 2 NO₂ ✓
Multiply the constants:
K = (1.0 × 10⁻³⁰)(6.4 × 10⁹) = 6.4 × 10⁻²¹
Extremely reactant-favored — which is why the nitrogen and oxygen in the atmosphere do not spontaneously form NO₂ at room temperature.