General Chemistry I · Thermochemistry

Hess's Law

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On this page 7 sections
  1. In 30 seconds
  2. Why this matters
  3. The college version
  4. Eli explains
  5. Key takeaway
  6. Study tools
  7. Sources & references

In 30 seconds

Hess's law states that the enthalpy change of an overall reaction is the sum of the enthalpy changes of the individual steps into which it can be divided — regardless of the path taken. Because enthalpy is a state function, ΔH depends only on the initial reactants and final products, not on how you get from one to the other. This lets chemists determine ΔH for reactions that are difficult or impossible to measure directly by combining reactions whose ΔH values are already known.

Why this matters

Many important enthalpies cannot be measured directly. Some reactions are too slow, some produce side products, and some (like forming CO from its elements) are experimentally messy. Hess's law lets chemists compute these values from well-behaved reactions. It is also the conceptual bridge to the next topic — standard enthalpies of formation — which is Hess's law applied to a universal set of "building block" reactions. Energetics of fuels, metabolic pathways, and industrial syntheses are all computed this way.

The college version

Key Ideas

  • State-function consequence: ΔH_total = ΔH_1 + ΔH_2 + ΔH_3 + … for any valid sequence of steps.
  • Reverse a reaction → flip the sign of ΔH. If A → B has ΔH = +x, then B → A has ΔH = −x.
  • Multiply a reaction by a factor → multiply ΔH by the same factor. ΔH scales with the amount of substance.
  • Add reactions → add their ΔH values. Intermediates that appear on both sides cancel out.
  • Goal: arrange the given equations so that, after cancellation, only the target reaction's reactants and products remain.
  • Common target reactions: forming CO from C and O₂ (partial oxidation), forming a compound from its elements, or an overall multi-step synthesis.

Equations and Variables

SymbolMeaning
ΔH₁, ΔH₂, …Enthalpy change of each step
ΔH_rxnEnthalpy change of the overall reaction
ΔH°fStandard enthalpy of formation (used in the next note)
  • ΔH_rxn = Σ ΔH_steps
  • Reverse: ΔH → −ΔH
  • Multiply by n: ΔH → n·ΔH
  • Add: ΔH_sum = ΔH_A + ΔH_B

How It Works

Think of enthalpy like altitude: the change in altitude from the base of a mountain to its peak is the same whether you climb the direct trail, take a winding road, or fly a helicopter. Only the start and end points matter. Hess's law applies the same logic to chemical reactions — you may "route" a reaction through any intermediate compounds as long as you end at the correct products.

Procedure:

  1. Write the target equation.
  2. List the given equations with their ΔH values.
  3. Reverse any equation whose reactant/product appears on the "wrong" side of the target; flip its ΔH sign.
  4. Multiply any equation so its coefficients match the target; scale its ΔH.
  5. Add the equations, canceling identical species on opposite sides.
  6. Add the ΔH values to get ΔH_rxn.

Worked Example

Find ΔH for C(s) + ½O₂(g) → CO(g), given:

(1) C(s) + O₂(g) → CO₂(g), ΔH = −393.5 kJ (2) CO(g) + ½O₂(g) → CO₂(g), ΔH = −283.0 kJ

Step 1 — Target has C(s) and ½O₂ as reactants, CO(g) as the sole product. CO₂ must cancel.

Step 2 — Keep equation (1) as written (C on the reactant side, correct):

C(s) + O₂(g) → CO₂(g), ΔH = −393.5 kJ

Step 3 — Equation (2) has CO(g) as a reactant, but we need CO(g) as a product. Reverse it and flip the sign:

CO₂(g) → CO(g) + ½O₂(g), ΔH = +283.0 kJ

Step 4 — Add the two equations:

C(s) + O₂(g) + CO₂(g) → CO₂(g) + CO(g) + ½O₂(g)

CO₂ cancels (one on each side); O₂ on the left minus ½O₂ on the right leaves ½O₂ on the left:

C(s) + ½O₂(g) → CO(g)

Step 5 — Add the enthalpies:

ΔH = (−393.5 kJ) + (+283.0 kJ) = −110.5 kJ

This is exactly the standard enthalpy of formation of carbon monoxide, −110.5 kJ/mol — a value that is hard to measure directly because burning carbon tends to over-oxidize to CO₂, so Hess's law is how it is determined.

Common Confusions

  • Forgetting to flip the sign when reversing. This is the most frequent error. Reversed reaction = reversed sign, always.
  • Forgetting to scale ΔH when changing coefficients. If you double an equation to balance it, you must double its ΔH.
  • Canceling incorrectly. Only cancel species that are identical and on opposite sides. If one side has 2O₂ and the other has ½O₂, they don't fully cancel.
  • Treating ΔH as temperature. ΔH is a heat quantity with a sign; don't confuse "adding equations" with arithmetic on temperatures.
  • Assuming the direct reaction can't be measured. Hess's law is often introduced with measurable steps but is most useful for unmeasurable targets (like CO formation).
Eli, the EliExplains learning guide

Eli explains

The same idea, in plain words

Explain it like I’m 10

Imagine you're counting how much money you spent on a trip from your house to the beach. You could drive straight there, or drive to your friend's house first, then to the beach. The total gas money might differ if the roads are different — but here's the twist: enthalpy is not like gas money, it's like your altitude. Whether you hike straight up the mountain or take the long zigzag trail, when you reach the top you're at the same height. Hess's law says reactions are like that: the total heat change only depends on where you started (reactants) and where you ended (products), not the path. So if you can't measure a reaction directly, you can "hike around it" using reactions you can measure, add up their heat changes, and get the answer.

Key takeaways

  • ΔH is a state function → path-independent → Hess's law holds.
  • Reverse: flip sign. Multiply: scale ΔH. Add: add ΔH.
  • Species that appear on both sides of the summed equations cancel.
  • Coefficients must match the target exactly before adding.
  • Hess's law is why ΔH°f values (next note) can be used to find any ΔH°rxn.
  • State Hess's law in one sentence.
  • If a reaction with ΔH = −250 kJ is reversed and then doubled, what is the new ΔH?
  • Given A → B (ΔH = +40 kJ) and B → C (ΔH = −15 kJ), find ΔH for A → C.
  • Why does Hess's law work? (What property of enthalpy guarantees it?)
  • Answers: (1) the ΔH of an overall reaction is the sum of the ΔH of its steps; (2) +500 kJ (reverse → +250, double → +500); (3) +25 kJ; (4) enthalpy is a state function, so ΔH is path-independent.

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Practice General Chemistry I

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Study tools & related lessonsYou’ll learn to · Related

You’ll learn to

  • State Hess's law and explain why it follows from enthalpy being a state function.
  • Manipulate thermochemical equations: reverse, multiply, and add them.
  • Calculate the enthalpy change of an overall reaction from a set of known reactions.

Sources & references

  1. OpenStax, *Chemistry 2e*, §5.3 Enthalpy (Hess's law).
  2. NIST Chemistry WebBook — standard enthalpy of formation of CO and CO₂.
  3. IUPAC "Gold Book" — Hess's law definition.

This lesson was adapted from the open educational references above; their licenses and attributions are preserved. See Copyright & Licensing.

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