A first-order phase transition has a discontinuous first derivative of the equilibrium free energy, such as entropy or volume, and latent heat. A second-order transition has continuous first derivatives but a discontinuous or divergent second derivative.
At fixed temperature, volume, and particle number, spontaneous changes satisfy because accounts for heat exchanged with the reservoir. Equilibrium therefore minimizes the Helmholtz free energy.
Minimization gives for and below. ThusUsing and , entropy is continuous but the low-temperature heat capacity has the additional . The jump is , so the transition is second order.
Writing , nonzero equilibria satisfy . For , coexistence occurs at and , so magnetization jumps and the transition is first order.
For , above and below: this is the tricritical continuous case. Below ,so the extra heat capacity is and diverges on approach from below; above it is absent.
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