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Entropy Gibbs energy notes and lesson for A Level chemistry (free PDF download)

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Entropy Gibbs energy notes and lesson for A Level chemistry (free PDF download)

This chemistry grades 11-12 lesson on entropy Gibbs energy notes gives the key ideas first, then worked examples and diagrams. After that, practise with the worksheet on entropy Gibbs energy and check yourself with the quiz.

Quick answer: Entropy measures how many ways particles and energy can be arranged; it rises from solid to liquid to gas. The Gibbs energy change, ΔG = ΔH − TΔS, decides feasibility: a reaction is spontaneous when ΔG is negative. It becomes spontaneous above T = ΔH/ΔS when both ΔH and ΔS are positive.

Level: Chemistry grades 11-12 (A Level · IB · Class 11-12) · Curriculum: IB R1.4

Entropy Gibbs energy notes: the key ideas

What is entropy?

Entropy, symbol S, measures how widely the energy of a system is spread over its particles. A system with more ways to arrange its particles and share energy has higher entropy. It is often described as disorder, but the real idea is the number of possible arrangements.

Definition

Entropy S is a measure of the number of ways in which particles and their energy can be arranged. Standard molar entropy S° is measured in J K⁻¹ mol⁻¹ at 298 K and 100 kPa. Entropy is never zero for a substance above absolute zero.

Three boxes of water particles: ordered ice with entropy 44.8, close but disordered liquid water with 69.9 and widely spread steam with 188.8 joules per kelvin per moleStandard molar entropy of water in three statesice, H₂O(s)44.8 J K⁻¹ mol⁻¹water, H₂O(l)69.9 J K⁻¹ mol⁻¹steam, H₂O(g)188.8 J K⁻¹ mol⁻¹more freedom of movement and energy storage: entropy rises
Entropy rises sharply from solid to liquid to gas.

These rules help you predict the sign of an entropy change without a calculator.

  • Gases have much higher entropy than liquids, and liquids higher than solids.
  • More moles of gas on the product side means ΔS is positive.
  • Dissolving a solid, or heating any substance, raises entropy.
  • Larger and more complex molecules have higher entropy than small ones.
SubstanceS° (J K⁻¹ mol⁻¹)
H₂(g)130.7
N₂(g)191.6
NH₃(g)192.5
H₂O(l)69.9
CaCO₃(s)92.9
Diamond, C(s)2.4

How do you calculate the entropy change of a reaction?

Formula

ΔS° = ΣS°(products) − ΣS°(reactants)
Each S° is multiplied by its coefficient in the balanced equation. ΔS° is in J K⁻¹ mol⁻¹ of reaction.

Worked example 1

Find ΔS° for N₂(g) + 3H₂(g) → 2NH₃(g).
Products: 2 × 192.5 = 385.0. Reactants: 191.6 + 3 × 130.7 = 583.7.
ΔS° = 385.0 − 583.7 = −198.7 J K⁻¹ mol⁻¹
Four moles of gas become two, so a decrease in entropy is expected.

Why can endothermic changes happen by themselves?

The second law of thermodynamics says that the total entropy of the system plus its surroundings must increase in any spontaneous change. An exothermic reaction releases heat that spreads the surroundings’ energy over more particles, raising their entropy.

Formulae

ΔS(surroundings) = −ΔH / T
ΔS(total) = ΔS(system) + ΔS(surroundings)
ΔH in J/mol, T in kelvin, so ΔS is in J K⁻¹ mol⁻¹.

What is Gibbs free energy and how does it predict feasibility?

Multiplying ΔS(total) by −T gives a quantity that depends only on the system: the Gibbs free energy change.

Gibbs equation

ΔG = ΔH − TΔS
ΔG = Gibbs energy change (kJ/mol), ΔH = enthalpy change (kJ/mol), T = temperature (K), ΔS = entropy change of the system (kJ K⁻¹ mol⁻¹). A reaction is spontaneous when ΔG < 0 and at equilibrium when ΔG = 0.

A two by two grid: negative ΔH with positive ΔS is spontaneous at all temperatures, negative ΔH with negative ΔS at low temperature only, positive ΔH with positive ΔS at high temperature only, positive ΔH with negative ΔS neverSigns of ΔH and ΔS decide when a reaction is spontaneousΔS positiveΔS negativeΔH negativeΔH positivespontaneous atall temperaturesspontaneous atlow T onlyspontaneous athigh T onlynever spontaneous
Four sign combinations of ΔH and ΔS.
Worked example 2

An instant cold pack contains ammonium nitrate, which dissolves with ΔH = +25.7 kJ/mol and ΔS = +108.7 J K⁻¹ mol⁻¹. Is dissolving spontaneous at 298 K?
ΔS = 0.1087 kJ K⁻¹ mol⁻¹.
ΔG = 25.7 − 298 × 0.1087 = 25.7 − 32.4 = −6.7 kJ/mol, so yes. The entropy gain outweighs the energy absorbed, so the pack gets cold.

Worked example 3

Limestone decomposes: CaCO₃(s) → CaO(s) + CO₂(g), ΔH = +178 kJ/mol, ΔS = +160.6 J K⁻¹ mol⁻¹. Find the minimum temperature for spontaneity.
At the changeover ΔG = 0, so T = ΔH / ΔS = 178 000 ÷ 160.6 = 1108 K (835 °C).

Graph of Gibbs energy change against temperature for the decomposition of calcium carbonate: a straight line falling from +178 kJ/mol at 0 K and crossing zero at 1108 K040080012001600−1000100200Temperature T (K)ΔG (kJ/mol)ΔG > 0: not spontaneousΔG < 0: spontaneous1108 K
ΔG = ΔH − TΔS for CaCO₃ → CaO + CO₂: the reaction becomes spontaneous above 1108 K.

How is ΔG related to the equilibrium constant?

Formula

ΔG° = −RT ln K
R = 8.31 J K⁻¹ mol⁻¹, T in K, K = equilibrium constant. Negative ΔG° gives K greater than 1; positive ΔG° gives K less than 1.

Worked example 4

A reaction has ΔG° = −28.6 kJ/mol at 298 K. Find K.
ln K = 28 600 ÷ (8.31 × 298) = 11.55
K = e11.55 = 1.04 × 10⁵

Common mistake

ΔH is normally given in kJ/mol but ΔS in J K⁻¹ mol⁻¹. If you subtract TΔS directly from ΔH, your answer is wrong by a factor of 1000. Convert ΔS to kJ K⁻¹ mol⁻¹, and always use kelvin, not °C.

Lina’s tip

To find the temperature at which a reaction switches from non-spontaneous to spontaneous (or the reverse), set ΔG = 0 and solve T = ΔH / ΔS. Check the answer lies in the sensible range for the reaction.

Key points to remember
  • ΔS° = ΣS°(products) − ΣS°(reactants), in J K⁻¹ mol⁻¹.
  • Gases have higher entropy than liquids; liquids higher than solids; more gas moles means ΔS positive.
  • ΔG = ΔH − TΔS; spontaneous if ΔG is negative, at equilibrium if ΔG = 0.
  • Convert ΔS to kJ K⁻¹ mol⁻¹ and T to kelvin before using the Gibbs equation.
  • ΔG° = −RT ln K links thermodynamics to the equilibrium constant.

Entropy, Gibbs energy and reaction feasibility: frequently asked questions

What does a positive entropy change mean?

It means the system has more ways of arranging its particles and energy after the change, for example when a solid melts, a liquid boils or a reaction produces more gas moles. It does not by itself prove the change is spontaneous.

How do you know if a reaction is spontaneous?

Calculate ΔG = ΔH − TΔS in consistent units. If ΔG is negative the reaction is thermodynamically feasible at that temperature. A feasible reaction may still be very slow if its activation energy is high.

Why are some endothermic reactions spontaneous?

If the entropy of the system increases enough, the −TΔS term makes ΔG negative even when ΔH is positive. Dissolving ammonium nitrate and the decomposition of limestone at high temperature are examples.

What is the link between ΔG and the equilibrium constant?

ΔG° = −RT ln K. A large negative ΔG° gives a very large K, so products dominate at equilibrium. A large positive ΔG° gives a very small K.

Why must temperature be in kelvin?

The equation ΔG = ΔH − TΔS uses absolute temperature, since T multiplies ΔS. Using °C would give zero or negative values at the wrong points and make predictions meaningless.

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