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S1.1 - Introduction to the particulate nature of matter S1.2 - The nuclear atom S1.3 - Electron configurations S1.4 - Counting particles by mass - The mole S1.5 - Ideal gases S2.1 - The ionic model S2.2 - The covalent model S2.3 - The metallic model S2.4 - From models to materials S3.1 - The periodic table - Classification of elements S3.2 - Functional groups - Classification of organic compounds R1.1 - Measuring enthalpy changes R1.2 - Energy cycles in reactions R1.3 - Energy from fuels R1.4 - Entropy and spontaneity AHL R2.1 - How much? The amount of chemical change R2.2 - How fast? The rate of chemical change R2.3 - How far? The extent of chemical change R3.1 - Proton transfer reactions R3.2 - Electron transfer reactions R3.3 - Electron sharing reactions R3.4 - Electron-pair sharing reactions

R1.4 - Entropy and spontaneity AHL

1.4.1 Entropy (AHL) 1.4.2 Gibbs Free Energy and Spontaneity (AHL) 1.4.3 Interpreting ∆G and Temperature Effects (AHL) 1.4.4 ∆G, Equilibrium and Reaction Quotient (AHL)

Entropy (S) and Entropy Changes (ΔS) HL Only

Specification Reference R1.4.1

Quick Notes

  • Entropy (S) measures the dispersal of energy and matter in a system.
  • The more disorder or randomness, the higher the entropy.
  • Entropy order (same conditions): Gases > Liquids > Solids
  • Entropy increases when:
    • A solid melts or evaporates.
    • A gas is produced in a reaction.
    • A substance dissolves.
  • Entropy decreases when:
    • Gases condense or liquids freeze.
    • Fewer particles are formed from more.
  • Standard entropy change: ΔS = ΣS(products) – ΣS(reactants)
  • Entropy values (S) are given in J mol⁻¹ K⁻¹.
  • S = 0 for a perfect crystal at 0 K (Third Law of Thermodynamics).

Full Notes

What Is Entropy (S)?

Entropy is a thermodynamic quantity that describes the dispersal or distribution of matter and energy within a system.

In simpler terms – the more ways the particles or energy can be arranged, the greater the entropy.

Entropy is a state function, measured in J mol⁻¹ K⁻¹.

Change in Entropy (ΔS) measures how the disorder of a system changes for a reaction or process.

Trends in Entropy by Physical State

Under the same temperature and pressure:

Therefore: S (gas) > S (liquid) > S (solid)

Predicting Entropy Changes

We can often predict whether entropy increases or decreases in a physical or chemical process:

Changes of state

IB HL 1.4.1 Chemistry diagram showing entropy increasing from solid to liquid to gas as particle disorder increases.

Going from a solid to a liquid or a gas increases entropy because particles move more freely and can be arranged in more possible ways.

Dissolving ionic solids

IB HL 1.4.1 Chemistry diagram showing entropy increase when an ionic solid dissolves into aqueous ions.

Dissolving a crystalline solid into solution increases disorder.

More gas particles formed

IB HL 1.4.1 Chemistry diagram highlighting larger entropy increases when the number of gaseous molecules rises.

Reactions where the number of gaseous molecules increases show a big jump in entropy.

Examples:

N2(g) + 3H2(g) → 2NH3(g): Entropy decreases (fewer gas particles).

CaCO3(s) → CaO(s) + CO2(g): Entropy increases (gas formed).

The opposite is also true for all the above.

Table for Prediciting ΔS

Process Effect on Entropy
Melting / Boiling Increase
Condensation / Freezing Decrease
Dissolution of solid into liquid Increase
Gas formation Increase
Decrease in number of gas moles Decrease

Calculating Entropy Change (ΔS)

Every substance, in a given state, has a standard entropy value (S).

We can use the standard entropy values (S) for each substance in a reaction (usually given in tables in the data booklet) to determine the entropy change, ΔS, that occurs.

Formula: ΔS = ΣS(products) – ΣS(reactants)

Step-by-step:

Photo of Matt
Matt’s exam tip

Don’t forget the molar ratios of everything in the equation and keep workings very clear. Also, make sure you are using a substance’s S value for the correct state (for example, H2O(l) has a different S to H2O(g)).


Worked Example

Calculate ΔSsystem for the reaction 2H2(g) + O2(g) → 2H2O(l).

  • Given: S(H2O(l)) = 70 J mol⁻¹ K⁻¹, S(H2(g)) = 131 J mol⁻¹ K⁻¹, S(O2(g)) = 205 J mol⁻¹ K⁻¹
  • ΔS = [2 × 70] – [2 × 131 + 1 × 205]
  • ΔS = 140 – (262 + 205) = 140 – 467 = –327 J mol⁻¹ K⁻¹

Entropy decreases in this reaction.

Entropy of a Perfect Crystal at 0 K

At absolute zero (0 K), a perfect crystal has zero entropy.

This is because there is only one way to arrange the particles, giving 'complete' order. This concept is the basis of the Third Law of Thermodynamics.

Structure 1.1 – Linked Course Question

Why is the entropy of a perfect crystal at 0 K predicted to be zero?

At 0 K, the particles in a perfect crystal are in complete order with only one possible arrangement and no movement. Since entropy measures disorder (or, more correctly, the number of possible microstates), this total order means the entropy is zero.

Summary