Helmholtz and Gibbs Free Energies
Two thermodynamic functions: Helmholtz energy (A) and Gibbs free energy (G).
Used to predict spontaneity of reactions, more convenient than entropy.
Helmholtz energy: A ≡ U − TS. At constant V and T, \Delta A = \Delta U − T\Delta S \le 0.
Gibbs free energy: G ≡ H − TS. At constant P and T, \Delta G = \Delta H − T\Delta S \le 0.
Gibbs free energy ($\Delta G$) is more useful because most reactions occur at constant P.
Maximum work done for reversible, isothermal change: w_{max} = \Delta A
\Delta G equals maximum free work at constant T & P.
\Delta G \le w_{non-expansion}, which is the theoretical limit of free work.
\Delta G^o = \Delta H^o − T\Delta S^o
\Delta G_f^o for elements in their most stable form is zero.
\Delta Gr^o = \sum n \Delta Gf^o(products) − \sum m \Delta G_f^o(reactants), where n and m are stoichiometric coefficients.
\Delta G = \Delta H − T\Delta S. Temperature contribution is through entropy.
Spontaneity depends on the signs of \Delta H and \Delta S and temperature.
Internal Energy: dU = TdS − PdV
Enthalpy: dH = TdS + VdP
Helmholtz: dA = −SdT − PdV
Gibbs energy: dG = −SdT + VdP
dG = (\frac{\partial G}{\partial T})P dT + (\frac{\partial G}{\partial P})T dP
\frac{\partial G}{\partial T}_P = -S
\frac{\partial G}{\partial P}_T = V
For ideal gases: G(P) = G^o + nRT \ln \frac{P}{P_o}
dG = −SdT + VdP + \mu1dn1 + \mu2dn2
\mu = (\frac{\partial G}{\partial n})_{P,T}
For a pure substance: \mu = G_M
\mu(P) = \mu^o + RT \ln \frac{P}{P_o}
Molecules move from high to low concentration (or chemical potential).
Equilibrium is reached when chemical potentials are equal.
\Delta G{mix} = nRT(xA \ln xA + xB \ln x_B)
\Delta S{mix} = −nR(xA \ln xA + xB \ln x_B)
Mixing is spontaneous because \Delta G_{mix} < 0
\Delta Gr = \Delta Gr^o + RT \ln Q_P
\Delta G_r < 0: forward reaction spontaneous.
\Delta G_r > 0: backward reaction spontaneous.
\Delta G_r = 0: equilibrium.
\Delta G_r^o = −RT \ln K
An equilibrium mixture would shift in a direction that counteracts the change.
\frac{\partial \ln K_P}{\partial T} = \frac{\Delta H^o}{RT^2}
KP = Kx(\frac{P}{P_o})^{\Delta n}
\left(\frac{\partial T}{\partial V}\right)S = -\left(\frac{\partial P}{\partial S}\right)V
\left(\frac{\partial T}{\partial P}\right)S = \left(\frac{\partial V}{\partial S}\right)P
\left(\frac{\partial S}{\partial V}\right)T = \left(\frac{\partial P}{\partial T}\right)V
\left(\frac{\partial S}{\partial P}\right)T = -\left(\frac{\partial V}{\partial T}\right)P