Thermodynamics
Hess's Law
The enthalpy bookkeeping rule that lets you measure reactions you can't run
Hess's law states that the enthalpy change of a reaction depends only on the initial and final states, not the path taken. Sum the ΔH of any sequence of steps that connects reactants to products and you get the same number — even if the route is hypothetical.
- DiscoveredGermain Hess, 1840
- Underlying principleH is a state function
- Standard temperature298.15 K
- Standard pressure1 bar (100 kPa)
- Sign conventionΔH < 0 = exothermic
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The state-function argument
Hess's law sounds almost too convenient: pick any chain of reactions linking your starting materials to your products, add up the enthalpies, and the answer is the right one. The justification is one sentence of thermodynamics. Enthalpy is a state function — it depends only on the current state of the system, not on what the system did to get there. Therefore the difference between two states is fixed.
To see why this must be true, imagine that a different route gave a smaller ΔH. You could combine the cheap route forward with the expensive route in reverse, finishing where you started but having released net energy from nothing. That violates the first law of thermodynamics. So all paths must agree.
The law was published by the Swiss-Russian chemist Germain Hess in 1840 — half a century before the first law was rigorously formulated. Hess noticed empirically that the heats of neutralization of strong acid–base pairs were consistent regardless of the order in which the acid and base were added. The thermodynamic vocabulary came later; the bookkeeping rule was already there.
The three rules of enthalpy arithmetic
- Reverse a reaction → flip the sign of ΔH. If A → B has ΔH = +100 kJ/mol, then B → A has ΔH = −100 kJ/mol.
- Multiply by a coefficient → multiply ΔH by the same coefficient. If ½ N₂ + ½ O₂ → NO has ΔH = +90 kJ/mol, then N₂ + O₂ → 2 NO has ΔH = +180 kJ/mol.
- Add reactions → add ΔH. If you can write the target reaction as a linear combination of known steps, the target ΔH is the same linear combination of known ΔHs.
That is the entire toolkit. Every Hess's law problem reduces to picking which steps to flip and which to scale so that the spectator species cancel, leaving exactly the target equation.
Worked example: combustion of methane
Suppose we want the standard enthalpy of combustion of methane:
CH₄(g) + 2 O₂(g) → CO₂(g) + 2 H₂O(l) ΔH_combustion = ?
We don't have a calorimeter handy. But we have these tabulated formation enthalpies (each is the energy released when the compound is built from its elements in their standard states):
(1) C(graphite) + O₂(g) → CO₂(g) ΔH₁ = −393.5 kJ/mol
(2) H₂(g) + ½ O₂(g) → H₂O(l) ΔH₂ = −285.8 kJ/mol
(3) C(graphite) + 2 H₂(g) → CH₄(g) ΔH₃ = −74.8 kJ/mol
To produce the target equation, we need CH₄ on the left, so reaction (3) must be reversed. We need 1 CO₂ on the right, so reaction (1) is used as-is. We need 2 H₂O on the right, so reaction (2) is doubled.
−(3): CH₄(g) → C(graphite) + 2 H₂(g) ΔH = +74.8 kJ/mol
(1): C(graphite) + O₂(g) → CO₂(g) ΔH = −393.5 kJ/mol
2(2): 2 H₂(g) + O₂(g) → 2 H₂O(l) ΔH = 2 × (−285.8) = −571.6 kJ/mol
─────────────────────────────────────────────────────────────
Sum: CH₄(g) + 2 O₂(g) → CO₂(g) + 2 H₂O(l) ΔH = −890.3 kJ/mol
The carbon atom and the two H₂ molecules cancel between the steps; what remains is exactly the combustion equation. The number, −890.3 kJ/mol, matches what bomb calorimetry on actual methane gives to within 0.1 %.
Shortcut: the formation-enthalpy method
The most common Hess's law application has a closed-form shortcut. For any reaction whose participants all appear in a table of standard formation enthalpies ΔH°f:
ΔH°_rxn = Σ (ν · ΔH°_f) products − Σ (ν · ΔH°_f) reactants
where ν is the stoichiometric coefficient. Elements in their standard state have ΔH°f = 0 by definition. Re-running the methane combustion this way:
ΔH° = [1·(−393.5) + 2·(−285.8)] − [1·(−74.8) + 2·(0)]
= [−393.5 − 571.6] − [−74.8]
= −965.1 + 74.8
= −890.3 kJ/mol ✓
Same answer, less paperwork. The formation method is Hess's law in its tidiest disguise: every reaction is decomposed via the elements, and the elements cancel between the reactant and product columns.
Hess's law vs direct measurement
| Direct calorimetry | Hess's law (path summation) | |
|---|---|---|
| What you actually do | Run the reaction, measure heat | Look up known ΔHs and add |
| Works on slow reactions | No — heat leaks before completion | Yes — uses tabulated values |
| Works on side-product-prone reactions | No — heat is for the mixture | Yes — chooses clean steps |
| Works on hypothetical reactions | No | Yes — only needs a paper path |
| Accuracy | ±0.1–1 % for clean systems | Limited by tabulated input |
| Equipment | Bomb or solution calorimeter | Pencil and a table |
| Best for | Establishing reference values | Predicting new reactions |
The two are complementary. Calorimetry produces the entries in the formation-enthalpy table; Hess's law leverages those entries to predict reactions nobody has run. Modern thermochemical databases (NIST, NASA Glenn, JANAF) are essentially curated, cross-checked Hess-law inputs.
Where Hess's law shows up
- Engine and rocket design. Specific energy of fuels (kJ/kg) is computed from formation enthalpies of products and reactants. The hydrazine + N₂O₄ pair used in the Apollo Lunar Module gives 5.7 MJ/kg by Hess summation, which then sets the achievable specific impulse.
- Bond-energy estimation. Average bond enthalpies are extracted from Hess cycles over many compounds. Breaking and re-forming bonds in a target reaction lets you estimate ΔH within ~10 %.
- Lattice energy via the Born–Haber cycle. The lattice energy of NaCl can't be measured directly. The Born–Haber cycle assembles ionization energy, electron affinity, sublimation, dissociation and formation enthalpies into a closed loop; Hess's law forces the lattice energy to take the value that closes it.
- Biochemical pathway analysis. Glycolysis turns glucose into pyruvate over ten enzymatic steps. The total ΔG (and ΔH) is the sum of the ten step values, even though no enzyme runs the whole thing in one shot.
- Climate radiative forcing. CO₂'s contribution to atmospheric energy balance starts with its formation enthalpy from C and O₂; combustion budgets for fossil fuels are Hess sums over thousands of compounds.
Estimating ΔH from average bond enthalpies
If you don't have formation enthalpies but you do have average bond strengths, Hess's law gives a rougher but still useful estimate. The hypothetical path is: break every bond in the reactants (cost ΣBE_reactants), then form every bond in the products (release ΣBE_products):
ΔH_rxn ≈ Σ BE(bonds broken) − Σ BE(bonds formed)
For the methane combustion: break 4 C–H bonds (+4·412 = +1648 kJ) and 2 O=O bonds (+2·498 = +996 kJ); form 2 C=O bonds (−2·799 = −1598 kJ) and 4 O–H bonds (−4·463 = −1852 kJ). Sum: +1648 + 996 − 1598 − 1852 = −806 kJ/mol. The true value is −890 kJ/mol; the bond-energy estimate is in the ballpark but coarse because bond strengths are averages over many compounds.
Common pitfalls
- Forgetting to flip the sign on a reversed step. The single most common Hess error. Write the reversed reaction explicitly before you scale it.
- Mismatched physical states. H₂O(l) and H₂O(g) differ by 44 kJ/mol — the heat of vaporization. Always check that the state in your tabulated value matches the state in your target equation.
- Mixing standard and non-standard data. Tabulated ΔH°f assumes 1 bar, 298.15 K, and (for solutions) 1 M. Mixing those with values measured at 500 K or 10 atm gives nonsense.
- Wrong sign convention. Some older sources report heats of combustion as positive numbers. Modern thermochemistry takes ΔH < 0 for exothermic. Pick a convention and stick to it.
- Treating bond-energy estimates as exact. Average bond enthalpies are population averages — the C–H in methane (435 kJ/mol) is not the same as the C–H in chloroform (377 kJ/mol). Use formation enthalpies whenever they exist.
Variants and extensions
- Born–Haber cycle. Hess applied to ionic-solid formation. Closes the loop: element → atoms → ions → solid versus element → solid directly.
- Kirchhoff's law. Extends Hess to other temperatures: ΔH(T₂) = ΔH(T₁) + ∫(ΔCp) dT. Same path-independence argument applied across a temperature axis.
- Hess's law for entropy and Gibbs energy. S and G are also state functions. ΔS°rxn and ΔG°rxn are computed by identical summation rules.
- Group contribution methods (Benson, Joback). Functional groups carry tabulated incremental ΔH°f values; molecular formation enthalpies are estimated by adding group contributions. A practical Hess shortcut for compounds without published data.
Frequently asked questions
Why does Hess's law work?
Enthalpy H is a state function — its value depends only on the current pressure, temperature and composition, not on history. Therefore the difference ΔH between two states is fixed regardless of route. If a different path gave a different ΔH, you could run one direction up and another down to create or destroy energy in a closed loop, violating the first law of thermodynamics.
Can Hess's law be applied to reactions that have never been measured?
Yes — that is the whole point. Many target reactions are too slow, too dangerous, or produce too many side-products to calorimeter directly. As long as you can string together known steps whose enthalpies are tabulated, the sum gives you the unknown ΔH. The combustion enthalpy of solid carbon to CO is a textbook example: direct measurement is impossible because you always get some CO₂.
What is the difference between Hess's law and the formation-enthalpy method?
The formation-enthalpy method (ΔH_rxn = ΣΔH_f products − ΣΔH_f reactants) is a special case of Hess's law in which every step goes through the elements in their standard states. Both give the same number; the formation method is just a tidier table lookup.
Do I have to use kJ per mole, or can I use kcal?
Any consistent energy unit works as long as you don't mix them. kJ/mol is the SI convention; kcal/mol is still common in biochemistry. 1 kcal/mol ≈ 4.184 kJ/mol. The signs and stoichiometric coefficients matter far more than the unit.
Does Hess's law apply at any temperature, or only 298 K?
It applies at any single temperature. Tabulated values are usually at 298.15 K (standard state), so if you sum standard enthalpies you get ΔH at 298 K. To get ΔH at a different temperature, use Kirchhoff's law: ΔH(T₂) = ΔH(T₁) + ∫ΔCp dT between the two temperatures.
Does the same trick work for entropy and Gibbs energy?
Yes. S, G, U and any other state function obey the path-independence rule. ΔG_rxn = ΣΔG_f products − ΣΔG_f reactants is the direct analogue. Heat q and work w, however, are path functions — Hess's law does not apply to them individually, only to their sum at constant pressure (which is ΔH).