Why some reactions happen on their own and others do not — measured by entropy and decided by Gibbs energy.
This whole sub-topic is Higher Level only. Enthalpy alone does not decide whether a reaction happens — some endothermic reactions are spontaneous. The missing ingredient is entropy, and the two combine in the Gibbs energy, ΔG, which is the real test of spontaneity.
Entropy (S) measures how dispersed the matter and energy of a system are — the more ways the particles and their energy can be arranged, the higher the entropy. Units are J K⁻¹ mol⁻¹. Entropy rises going solid → liquid → gas, when a solid or liquid produces a gas, when the number of moles of gas increases, and when a solid dissolves. Predict the sign of ΔS:
Every substance has an absolute standard entropy S° (unlike enthalpy, entropy has a true zero — a perfect crystal at 0 K). For a reaction:
ΔS°reaction = Σ S°(products) − Σ S°(reactants)
The Gibbs energy change combines enthalpy and entropy at a temperature T (in kelvin):
ΔG° = ΔH° − TΔS°
Watch the units. ΔH° is usually in kJ mol⁻¹ but S° (and ΔS°) is in J K⁻¹ mol⁻¹ — you must convert ΔS° to kJ (÷1000) before multiplying by T, or you will be out by a factor of 1000. Try the calculator:
A reaction is spontaneous (thermodynamically feasible) when ΔG < 0. If ΔG = 0 the system is at equilibrium; if ΔG > 0 the forward reaction is not spontaneous. Because ΔG° = ΔH° − TΔS°, the signs of ΔH and ΔS give four cases — click each:
When ΔH and ΔS have the same sign, spontaneity depends on temperature. Since ΔG° = ΔH° − TΔS° is a straight line in T (slope −ΔS°, intercept ΔH°), it crosses ΔG = 0 at the changeover temperature:
T = ΔH° ÷ ΔS° (setting ΔG° = 0)
Drag the temperature slider: the plot shows ΔG against T for the CaCO₃ decomposition (ΔH° = +178 kJ, ΔS° = +161 J K⁻¹). It only becomes spontaneous above about 1106 K (≈ 833 °C) — which is why a lime kiln must be so hot.
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