Entropy, Gibbs Energy & Spontaneity
Why some reactions run on their own and others never do — and the single equation that decides.
An ice cube melts in your hand even though melting <em>absorbs</em> heat — an endothermic change happening all on its own. If energy release were the whole story, that couldn't happen. Something besides enthalpy is pulling the strings: entropy.
Entropy: nature's tendency to spread out
Entropy (S) measures how spread out the energy and matter of a system are — loosely, its disorder. A tidy crystal has low entropy; the same substance as a gas, molecules flying everywhere, has high entropy. Nature overwhelmingly drifts toward higher entropy, simply because there are vastly more spread-out arrangements than tidy ones.
Entropy generally increases when a solid melts to a liquid, a liquid boils to a gas, a solid dissolves, or a reaction produces more gas molecules than it consumes. Those changes have ΔS > 0.
Two drives, one decision
Reactions are pulled by two tendencies: toward lower enthalpy (releasing energy, ΔH < 0) and toward higher entropy (more dispersal, ΔS > 0). Sometimes they agree; often they conflict. Melting ice is uphill in enthalpy (it absorbs heat) but strongly downhill in entropy (liquid is more disordered than ice) — and above 0 °C the entropy drive wins.
Gibbs free energy (G) combines both drives into one number whose sign settles the matter:
How the signs combine
Because ΔG = ΔH − TΔS, the four combinations of signs tell a clean story:
- ΔH < 0, ΔS > 0 → ΔG < 0 always: spontaneous at all temperatures (both drives agree).
- ΔH > 0, ΔS < 0 → ΔG > 0 always: never spontaneous (both drives oppose).
- ΔH < 0, ΔS < 0 → spontaneous only at low T (enthalpy wins when T is small).
- ΔH > 0, ΔS > 0 → spontaneous only at high T (the TΔS term wins when T is large — this is melting ice).
- Both ΔH and ΔS are already in kJ, and T = 298 K — good, no unit surprises.
- ΔG = ΔH − TΔS = (−92.0) − (298)(−0.199).
- Compute TΔS: (298)(−0.199) = −59.3 kJ, so −TΔS = +59.3 kJ.
- ΔG = −92.0 + 59.3 = −32.7 kJ.
- ΔG = ΔH − TΔS = (+178) − (298)(0.161).
- TΔS = 298 × 0.161 = 47.98 kJ.
- ΔG = 178 − 47.98 = +130.0 kJ.
- ΔG > 0, so at 298 K this decomposition is non-spontaneous (limestone is stable at room temperature).
- At the crossover, ΔG = 0, so ΔH − TΔS = 0, which rearranges to T = ΔH ÷ ΔS.
- T = 178 ÷ 0.161.
- T ≈ 1106 K — above this temperature TΔS outweighs ΔH and the decomposition becomes spontaneous (why kilns run so hot).
Check your understanding
- Entropy (S) measures the dispersal of energy and matter; nature drifts toward higher entropy.
- ΔS > 0 for melting, boiling, dissolving, and reactions that make more gas.
- Gibbs free energy: ΔG = ΔH − TΔS, with T in kelvin.
- ΔG < 0 spontaneous; ΔG > 0 non-spontaneous; ΔG = 0 equilibrium.
- The ΔH and ΔS signs together set whether — and at what temperatures — a reaction runs; a more negative ΔG points further toward products.