Hess's Law
Enthalpy doesn't care how you got there — so you can build any reaction's ΔH out of steps you already know.
You can't burn carbon and stop cleanly at carbon monoxide — some always races on to carbon dioxide. So how does anyone know the ΔH of that half-finished reaction? You never measure it. You assemble it from two reactions you <em>can</em> measure. That trick is Hess's law.
Why the path doesn't matter
Recall from the first lesson that enthalpy is a state function: it depends only on the current state, like altitude on a mountain. Whether you drive up the gentle road or scramble straight up the cliff, the summit is the same height above where you started.
Hess's law is exactly this idea applied to reactions: the total enthalpy change of a reaction is the same whether it happens in one step or many. So if a target reaction can be written as a sum of other reactions, its ΔH is the sum of their ΔH values.
- The target needs 1 S and 1 SO₃. Reaction (1) already gives S → SO₂ with the right direction and amount — keep it as is: ΔH = −296.8 kJ.
- Reaction (2) makes 2 SO₃; we only want 1, so halve it: SO₂ + 1⁄2 O₂ → SO₃, ΔH = −197.8 ÷ 2 = −98.9 kJ.
- Add the two steps. The SO₂ produced in (1) is consumed in the halved (2), so it cancels.
- ΔH = (−296.8) + (−98.9) = −395.7 kJ.
- Target has CO as a product, but in (2) CO is a reactant — so reverse (2): CO₂ → CO + 1⁄2 O₂, ΔH = +283.0 kJ.
- Keep (1) as is: C + O₂ → CO₂, ΔH = −393.5 kJ.
- Add them: the CO₂ cancels (product of (1), reactant of the reversed (2)), leaving C + 1⁄2 O₂ → CO.
- ΔH = (−393.5) + (+283.0) = −110.5 kJ.
- Both reactions are already pointed the right way and correctly scaled — just add them.
- The 2 NO produced in (1) is consumed in (2), so NO cancels.
- Overall: N₂ + 2 O₂ → 2 NO₂.
- ΔH = (+180.5) + (−114.1) = +66.4 kJ — endothermic overall.
Check your understanding
- Hess's law: because enthalpy is a state function, ΔH is path-independent.
- A target reaction's ΔH = the sum of the ΔH values of the steps that build it.
- Reverse a reaction → flip the sign of ΔH.
- Scale a reaction → multiply ΔH by the same factor.
- Manipulate the given reactions so species cancel, then add the ΔH values.