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IMAT Chemistry · Equilibrium, Kinetics and Energetics

Entropy, Gibbs Free Energy and Spontaneous Change

Whether a reaction can happen by itself depends on both its enthalpy change and its entropy change, combined in the Gibbs free energy ΔG = ΔH − TΔS.

Why this matters

No past IMAT question has been set on this page yet, but entropy and free energy are in the official syllabus. Expect a qualitative question: the sign of an entropy change, or whether a reaction is spontaneous at high or low temperature.

Concept 1 of 2: Entropy: a measure of the spreading of matter and energy

A drop of ink spreads through water and never gathers back into a drop by itself. There are vastly more ways for the particles to be spread out than gathered up, so spreading is overwhelmingly likely. Entropy measures how many ways the particles and their energy can be arranged: the more spread out, the higher the entropy.

Definition

  • Entropy SS measures the dispersal (often called the disorder) of particles and energy. Units: J/(K mol).
  • Entropy increases from solid to liquid to gas, with a big jump on forming a gas.
  • A reaction that increases the number of moles of gas usually has ΔS>0\Delta S > 0. Dissolving, mixing and heating also increase entropy.
  • The second law of thermodynamics: in a spontaneous change, the total entropy of the system plus surroundings increases. The entropy of the system alone can fall, if enough heat is released to the surroundings.
ChangeEntropy of the systemWhy
Ice meltingIncreasesParticles become free to move
Steam condensingDecreasesGas becomes liquid
CaCO3(s)→CaO(s)+CO2(g)\mathrm{CaCO_3(s) \rightarrow CaO(s) + CO_2(g)}IncreasesA gas is produced from a solid
N2(g)+3H2(g)→2NH3(g)\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)}Decreases4 mol of gas become 2 mol
Salt dissolving in waterUsually increasesIons spread through the solution
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The entropy of the system can fall in a spontaneous change

Water freezes spontaneously below 0 °C although its entropy falls. The heat released raises the entropy of the surroundings by more. The second law is about the total entropy, not the system alone.

Concept 2 of 2: Gibbs free energy and whether a reaction is spontaneous

Two tendencies drive chemical change: to release energy (negative ΔH) and to spread out (positive ΔS). The Gibbs free energy weighs them against each other, with temperature deciding how much the entropy term counts. When ΔG is negative the reaction can go by itself.

Definition

  • ΔG=ΔH−TΔS\Delta G = \Delta H - T\Delta S, with TT in kelvin. Convert ΔS\Delta S from J to kJ before combining it with ΔH\Delta H in kJ.
  • ΔG<0\Delta G < 0: the reaction is spontaneous (feasible). ΔG>0\Delta G > 0: not spontaneous; the reverse reaction is. ΔG=0\Delta G = 0: at equilibrium.
  • ΔH<0\Delta H < 0 and ΔS>0\Delta S > 0: spontaneous at all temperatures.
  • ΔH>0\Delta H > 0 and ΔS<0\Delta S < 0: never spontaneous.
  • ΔH<0\Delta H < 0 and ΔS<0\Delta S < 0: spontaneous only at low temperature. ΔH>0\Delta H > 0 and ΔS>0\Delta S > 0: only at high temperature. The switch happens at T=ΔH/ΔST = \Delta H / \Delta S.
  • Spontaneous says nothing about speed: diamond turning into graphite has ΔG<0\Delta G < 0 but is far too slow to see.

Gibbs free energy

ΔG=ΔH−TΔS\Delta G = \Delta H - T\Delta S
  • ΔG\Delta Gfree energy change, in kJ/mol
  • ΔH\Delta Henthalpy change, in kJ/mol
  • TTabsolute temperature, in K
  • ΔS\Delta Sentropy change, in kJ/(K mol) when combined with ΔH in kJ

Worked example

For CaCO3(s)→CaO(s)+CO2(g)\mathrm{CaCO_3(s) \rightarrow CaO(s) + CO_2(g)}, ΔH=+178 kJ/mol\Delta H = +178\ \text{kJ/mol} and ΔS=+161 J K−1mol−1\Delta S = +161\ \text{J K}^{-1}\text{mol}^{-1}. Is it spontaneous at 298 K? Above what temperature does it become spontaneous?
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Endothermic reactions can be spontaneous

Ice melting above 0 °C and ammonium nitrate dissolving are endothermic yet happen by themselves, because their entropy increase is large enough. A positive ΔH alone does not rule out a spontaneous change.

Spontaneous does not mean fast

ΔG tells you whether a reaction can go, not how quickly. A mixture of hydrogen and oxygen has a very negative ΔG for forming water, yet it can sit unchanged for years until a spark supplies the activation energy.

Summary — formulas & gotchas at a glance

A revision cheat-sheet for the formulas and gotchas above. Click any concept name to jump back to its full explanation.

Formulas (1)

Reference tables (1)

Entropy: a measure of the spreading of matter and energy5 rows
ChangeEntropy of the systemWhy
Ice meltingIncreasesParticles become free to move
Steam condensingDecreasesGas becomes liquid
CaCO3(s)→CaO(s)+CO2(g)\mathrm{CaCO_3(s) \rightarrow CaO(s) + CO_2(g)}IncreasesA gas is produced from a solid
N2(g)+3H2(g)→2NH3(g)\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)}Decreases4 mol of gas become 2 mol
Salt dissolving in waterUsually increasesIons spread through the solution

Watch out for (3)

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