Michael S. answered 08/05/26
B.S. in Chemistry, Indiana University; Organic Chem Teaching Intern
Kp = 1.18
Step 1 — ICE table in partial pressures
2 SO2(g) + O2(g) ⇌ 2 SO3(g)
SO2 O2 SO3
I: 4.57 1.50 0
C: −2x −x +2x
E: 4.57−2x 1.50−x 2x
You can work directly in atm — Kp is defined in partial pressures, so there is no need to convert to concentrations and back.
Step 2 — find x from the one equilibrium value you were given
2x = 1.99 atm → x = 0.995 atm
Step 3 — fill in the rest
P(SO2) = 4.57 − 2(0.995) = 4.57 − 1.99 = 2.58 atm
P(O2) = 1.50 − 0.995 = 0.505 atm
P(SO3) = 1.99 atm
A shortcut worth seeing: SO2 and SO3 both carry a coefficient of 2, so the SO2 consumed equals the SO3 formed exactly — 1.99 atm. Oxygen, with coefficient 1, changes by half that. You can often skip solving for x entirely once you notice this.
Step 4 — the Kp expression
Kp = P(SO3)2 / [ P(SO2)2 × P(O2) ]
Kp = (1.99)2 / [ (2.58)2(0.505) ] = 3.96 / [ (6.66)(0.505) ] = 3.96 / 3.36 = 1.18
Two things to get right
1. Exponents come from coefficients. Both SO3 and SO2 are squared; O2 is to the first power. Forgetting to square the SO2 term gives 3.05 — a plausible-looking number that is simply wrong.
2. Use equilibrium pressures, not initial ones. Substituting the starting 4.57 and 1.50 into the expression is the other frequent slip. That calculation gives Q at t = 0, which is 0 here since no product existed yet.
Interpreting the result: Kp ≈ 1 means neither side dominates — at 1090 K this reaction sits with substantial amounts of both reactants and products, which the numbers show directly (2.58 atm SO2 alongside 1.99 atm SO3). Industrially this is exactly the problem the contact process has to solve: SO3 formation is favoured at lower temperatures, so plants run cooler with a catalyst rather than hotter.
(Formally Kp here carries units of atm−1, since Δn = 2 − 3 = −1, but most courses report equilibrium constants unitless. Follow whichever convention your instructor uses.)
