IB Chemistry HL Topic 4 — Entropy & Spontaneity Paper 1 & 2 Core idea ~11 min read

Gibbs Free Energy

Enthalpy says one thing. Entropy says another. When they disagree, who wins? Gibbs free energy is the referee: one number that takes both sides into account and tells you straight out whether a reaction can happen on its own.

📚 What you need to know

Two forces, one number

Picture a tug of war. On one side, enthalpy: reactions like giving out heat, so a negative ΔH pulls towards “yes, go”. On the other side, entropy: things like spreading out, so a positive ΔS also pulls towards “yes, go”.

Sometimes both pull the same way and the reaction is a certainty. Sometimes they fight, and then the winner depends on the temperature. Gibbs free energy adds the two pulls together into a single score.

The Gibbs equation ΔG° = ΔH°reactionTΔS°system
What each part of the Gibbs equation is doing ΔG = ΔH TΔS the energy term negative when heat is given out units: kJ mol⁻¹ the spreading term grows as temperature rises ΔS is in J, so ÷ 1000 first The reaction can go on its own when the whole right side is negative. Enthalpy pulls one way, entropy the other, and temperature decides who wins.
Notice the minus sign in front of the entropy term. A positive ΔS makes ΔG more negative, which is why spreading out helps a reaction go.
Read the equation out loud as a sentence: “the energy I can actually use equals the heat I release, minus what entropy takes as its fee.” That fee is TΔS, and it gets more expensive as things heat up.

The units trap

This is the single biggest source of lost marks in the whole topic, and it is not chemistry — it is arithmetic. ΔH comes in kilojoules. ΔS comes in joules. You cannot subtract one from the other until they match.

Convert the entropy value before you subtract ΔH is in kilojoules, ΔS is in joules. Match them up first. ΔS from the booklet convert the units use in the equation −199 J K⁻¹ mol⁻¹ ÷ 1000 −0.199 kJ K⁻¹ mol⁻¹ Joules and kilojoules cannot be subtracted from one another. If your ΔG comes out in the tens of thousands, you forgot to divide.
Do the division on its own line, before it goes anywhere near the Gibbs equation. Trying to do it inside the brackets is how the 1000 gets lost.

🧩 Route 1: from ΔH° and ΔS°

  1. Write down ΔH° in kJ mol−1 exactly as given.
  2. Divide ΔS° by 1000 to get kJ K−1 mol−1. Write the converted value down.
  3. Check T is in kelvin. If the question says 25 °C, that is 298 K.
  4. Substitute into ΔG° = ΔH° − TΔS°, keeping the signs in brackets.
  5. Answer in kJ mol−1, then say what the sign means.
Signs inside brackets. If ΔS° is negative, −TΔS° becomes a plus. Write it as −92 − (298 × −0.199) and let the brackets do the thinking, rather than trying to work out the sign in your head.

Route 2: adding up ΔG°f values

Standard free energies of formation behave exactly like enthalpies of formation. If the question hands you a table of ΔG°f values, you never need the Gibbs equation at all.

The Hess-style route ΔG° = ΣΔG°f(products) − ΣΔG°f(reactants)

Here elements in their standard states are zero, just like with enthalpy: ΔG°f for O2(g) is 0. That is the one place where entropy and free energy behave differently, and it catches people out both ways.

SymbolWhat it isUnitsWatch out for
ΔG°Free energy change: your verdict on the reactionkJ mol−1Negative means it can go
ΔH°Enthalpy change: heat taken in or given outkJ mol−1Already in kJ, leave it alone
ΔS°Entropy change: how much things spread outJ K−1 mol−1Must be divided by 1000
TTemperature of the reactionKAdd 273 if given in °C
ΔG°fFree energy of formation of one substancekJ mol−1Zero for elements, unlike S°

Worked examples

WORKED EXAMPLE

For N2(g) + 3H2(g) → 2NH3(g), ΔH° = −92 kJ mol−1 and ΔS° = −199 J K−1 mol−1. Calculate ΔG° at 298 K.

Step 1: convert the entropy value −199 ÷ 1000 = −0.199 kJ K⁻¹ mol⁻¹ Step 2: substitute, keeping the signs in brackets ΔG° = −92 − (298 × −0.199) Step 3: the bracket first 298 × −0.199 = −59.3, and −92 − (−59.3) = −92 + 59.3 ΔG° = −32.7 kJ mol⁻¹, so it can happen at 298 K Both terms fought: enthalpy said yes, entropy said no. Enthalpy won, but only by 33 kJ — hold that thought for the next page.
WORKED EXAMPLE

For MgCO3(s) → MgO(s) + CO2(g), ΔH° = +100 kJ mol−1 and ΔS° = +175 J K−1 mol−1. Calculate ΔG° at 298 K and comment.

Step 1: convert +175 ÷ 1000 = +0.175 kJ K⁻¹ mol⁻¹ Step 2: substitute ΔG° = +100 − (298 × 0.175) Step 3: work it out 298 × 0.175 = 52.15, so 100 − 52.15 = +47.85 ΔG° = +47.9 kJ mol⁻¹, so it will not go at room temperature And that is right: you have to heat a carbonate in a Bunsen flame to decompose it. Entropy is helping, just not enough yet.
WORKED EXAMPLE

Use ΔG°f values to find ΔG° for CH4(g) + 2O2(g) → CO2(g) + 2H2O(l). Values in kJ mol−1: CH4 −51, O2 0, CO2 −394, H2O(l) −237.

Step 1: products, with balancing numbers −394 + (2 × −237) = −394 − 474 = −868 Step 2: reactants (oxygen is an element, so zero) −51 + (2 × 0) = −51 Step 3: products − reactants −868 − (−51) = −868 + 51 ΔG° = −817 kJ mol⁻¹ Hugely negative, which is why methane burns the instant you give it a spark. No temperature or entropy data needed for this route.

💡 Exam tip

⚠ Common mix-up

You can now get a number for ΔG at one temperature. The really useful question is what happens when you change that temperature — and which reactions can be switched on with a Bunsen burner. Up next: Spontaneous Reactions.

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