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Thermodynamic Potentials and Equilibrium

Thermodynamic potentials (enthalpy, Helmholtz free energy, Gibbs free energy, grand potential) answer the question: which state is stable under a given set of constraints? This page is relevant for predicting phase coexistence, chemical reaction direction, battery voltage, and material stability. It unifies the first and second laws into a single minimization principle.

Authoritative sources

The fundamental potentials

PotentialDefinitionNatural variablesMinimized at equilibrium when
U(S,V,N)Internal energyS, V, N(S, V, N fixed)
H(S,P,N) = U + PVEnthalpyS, P, NConstant P, S, N (e.g., throttling)
F(T,V,N) = U − TSHelmholtz free energyT, V, NConstant T, V, N (e.g., system in a heat bath at fixed volume)
G(T,P,N) = U + PV − TSGibbs free energyT, P, NConstant T, P, N (most common: open to atmosphere, in a heat bath)
Ω(T,V,μ) = F − μNGrand potentialT, V, μConstant T, V, μ (system in contact with both a heat bath and a particle reservoir)
Details

Why these combinations? Each potential is a Legendre transform of UU that replaces an extensive variable with its conjugate intensive variable. For example, F=U−TSF = U - TS replaces SS (extensive) with TT (intensive, its conjugate via T=(∂U/∂S)V,NT = (\partial U/\partial S)_{V,N}). At fixed T,VT, V, minimizing FF is equivalent to maximizing StotalS_{\text{total}} (system + reservoir), which is the second law.

Differential forms:

dU=T dS−P dV+μ dNdH=T dS+V dP+μ dNdF=−S dT−P dV+μ dNdG=−S dT+V dP+μ dNdΩ=−S dT−P dV−N dμdU = T\,dS - P\,dV + \mu\,dN dH = T\,dS + V\,dP + \mu\,dN dF = -S\,dT - P\,dV + \mu\,dN dG = -S\,dT + V\,dP + \mu\,dN d\Omega = -S\,dT - P\,dV - N\,d\mu

These are the fundamental relations. All thermodynamic properties can be derived from any one potential as a function of its natural variables (it is a generating function).

Microscopic derivation. The connection to statistical mechanics is direct: F=−kBTln⁡ZF = -k_B T \ln Z (canonical partition function) and G=−kBTln⁡ΞG = -k_B T \ln \Xi (isothermal–isobaric partition function). See Statistical Foundations of Thermodynamics.

Stability criteria

At equilibrium the relevant potential is at a minimum with respect to internal variables (composition, phase fractions). For the minimum to be stable (not a saddle point), the potential must satisfy convexity/concavity conditions:

These conditions ensure that the equilibrium is physically realizable: a positive heat capacity means adding heat raises temperature (not lowers it), and a positive compressibility means compressing raises pressure (not lowers it).

Chemical potential and reaction equilibrium

The chemical potential μi=(∂G/∂Ni)T,P,Nj≠i\mu_i = (\partial G / \partial N_i)_{T,P,N_{j\neq i}} is the molar Gibbs free energy of species ii in a mixture.

For a reaction ∑iνiAi=0\sum_i \nu_i A_i = 0 at constant T,PT, P:

ΔrG=∑iνiμi\Delta_r G = \sum_i \nu_i \mu_i
Details

Standard state and equilibrium constant. Writing μi=μi∘+RTln⁡ai\mu_i = \mu_i^\circ + RT\ln a_i (where aia_i is activity), at equilibrium:

ΔrG∘=−RTln⁡K\Delta_r G^\circ = -RT\ln K

where KK is the equilibrium constant. This connects thermodynamics to chemical kinetics and to electrochemistry (Nernst equation: E=E∘−(RT/nF)ln⁡Q\mathcal{E} = \mathcal{E}^\circ - (RT/nF)\ln Q).

Batteries. The maximum electrical work a battery can deliver at constant T,PT, P is ΔG\Delta G of the cell reaction. The open-circuit voltage is E=−ΔG/(nF)\mathcal{E} = -\Delta G / (nF). See also Electrochemistry (future page) for the full treatment of electrode potentials and the Nernst equation.

Phase equilibrium and the Gibbs phase rule

Two phases α\alpha and β\beta of a pure substance coexist when their chemical potentials are equal:

μα(T,P)=μβ(T,P)\mu^\alpha(T,P) = \mu^\beta(T,P)

For a system with CC components and PP phases, the Gibbs phase rule gives the number of intensive degrees of freedom:

F=C−P+2F = C - P + 2
Details

Derivation. Each phase has C+2C + 2 intensive variables (T,PT, P, and CC composition variables). At equilibrium, TT and PP are the same in all phases, and μiα=μiβ\mu_i^\alpha = \mu_i^\beta for each component and each pair of phases. Counting constraints gives F=C−P+2F = C - P + 2.

Examples:

Clapeyron and Clausius–Clapeyron equations. The slope of a phase boundary:

dPdT=ΔSΔV=ΔHT ΔV\frac{dP}{dT} = \frac{\Delta S}{\Delta V} = \frac{\Delta H}{T\,\Delta V}

For a vapor–liquid transition (Vgas≫VliqV_{\text{gas}} \gg V_{\text{liq}}, ideal gas): dP/dT=ΔHmol/(RT2)dP/dT = \Delta H_{\text{mol}}/(RT^2) (Clausius–Clapeyron), where ΔHmol\Delta H_{\text{mol}} is the molar latent heat (the enthalpy change per mole transferred between phases). This integrates to the familiar vapor-pressure curve.

Maxwell relations

From the equality of mixed partials of a potential, e.g. from dG=−S dT+V dP+μ dNdG = -S\,dT + V\,dP + \mu\,dN:

(∂S∂P)T,N=−(∂V∂T)P,N\left(\frac{\partial S}{\partial P}\right)_{T,N} = -\left(\frac{\partial V}{\partial T}\right)_{P,N}

The four Maxwell relations (one per potential) allow you to compute entropy changes from measurable P,V,TP, V, T data.

Details

All four (pure substance, NN fixed):

(∂T∂V)S=−(∂P∂S)V(U)(∂T∂P)S=(∂V∂S)P(H)(∂S∂V)T=(∂P∂T)V(F)(∂S∂P)T=−(∂V∂T)P(G)\left(\frac{\partial T}{\partial V}\right)_S = -\left(\frac{\partial P}{\partial S}\right)_V \quad (U) \left(\frac{\partial T}{\partial P}\right)_S = \left(\frac{\partial V}{\partial S}\right)_P \quad (H) \left(\frac{\partial S}{\partial V}\right)_T = \left(\frac{\partial P}{\partial T}\right)_V \quad (F) \left(\frac{\partial S}{\partial P}\right)_T = -\left(\frac{\partial V}{\partial T}\right)_P \quad (G)

Use. To find (∂S/∂T)P=CP/T(\partial S/\partial T)_P = C_P/T, or to compute (∂U/∂V)T=T(∂P/∂T)V−P(\partial U/\partial V)_T = T(\partial P/\partial T)_V - P (which vanishes for an ideal gas, confirming U=U(T)U = U(T)).

Example problem

At 298 K and 1 atm, the standard Gibbs free energies of formation are: ΔfG∘(H2O, l)=−237.1 kJ/mol\Delta_f G^\circ(\text{H}_2\text{O, l}) = -237.1\,\text{kJ/mol}, ΔfG∘(H2, g)=0\Delta_f G^\circ(\text{H}_2\text{, g}) = 0, ΔfG∘(O2, g)=0\Delta_f G^\circ(\text{O}_2\text{, g}) = 0. For the reaction H2+12O2→H2O(l)\text{H}_2 + \tfrac{1}{2}\text{O}_2 \to \text{H}_2\text{O(l)}, find ΔrG∘\Delta_r G^\circ and the maximum electrical work per mole of water produced. What is the corresponding cell voltage (n=2n = 2 electrons)?

Solution ΔrG∘=ΔfG∘(H2O)−ΔfG∘(H2)−12ΔfG∘(O2)=−237.1 kJ/mol\Delta_r G^\circ = \Delta_f G^\circ(\text{H}_2\text{O}) - \Delta_f G^\circ(\text{H}_2) - \tfrac{1}{2}\Delta_f G^\circ(\text{O}_2) = -237.1 \text{ kJ/mol}

Maximum electrical work (at constant T,PT, P): welec,max=ΔrG∘=−237.1 kJ/molw_{\text{elec,max}} = \Delta_r G^\circ = -237.1\,\text{kJ/mol} (negative sign means work is done by the system).

Cell voltage:

E∘=−ΔrG∘nF=2371002×96485≈1.23 V\mathcal{E}^\circ = \frac{-\Delta_r G^\circ}{nF} = \frac{237100}{2 \times 96485} \approx 1.23 \text{ V}

This is the standard hydrogen fuel-cell voltage.