Thermodynamics
Gibbs energy and equilibrium
Calculate ∆G and use it with K.
Working out ∆S of the surroundings every time is awkward. Gibbs energy, G, combines enthalpy and entropy in one quantity about the system alone: G = H – TS. At constant temperature and pressure:
∆G = ∆H – T∆S.
- If ∆G < 0, the process is spontaneous.
- If ∆G = 0, the system is at equilibrium.
- If ∆G > 0, it is not spontaneous (the reverse process is).
The signs of ∆H and ∆S decide how temperature matters:
| ∆H | ∆S | Spontaneous? |
|---|---|---|
| – | + | at all temperatures |
| + | – | never |
| + | + | only at high temperature, above T = ∆H/∆S |
| – | – | only at low temperature |
Gibbs energy is linked to the equilibrium constant:
∆rG⊖ = –RT ln K = –2.303 RT log K.
A large K (mostly products at equilibrium) means a negative ∆G⊖. So K can be found from ∆G⊖ (log K = –∆G⊖ / 2.303RT), and ∆G⊖ from a measured K. For example, a reaction with K = 100 at 298 K has ∆G⊖ = –2.303 × 8.314 × 298 × log 100 = –11.4 kJ mol⁻¹.
∆G also has a practical meaning: it is the maximum useful work a system can do (other than expansion work). A reaction with a large positive ∆G⊖ hardly goes at all on its own.
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