Maxwell’s Thermodynamic Relations
Cross-derivative Maxwell identities, Clausius-Clapeyron equation, rigorous heat capacity differences Cp - Cv, the two TdS equations, internal energy equations of state, and Joule-Kelvin throttling coefficients.
§5.1 Derivation of the Four Maxwell Relations
1. Mathematical Foundation of Maxwell's Relations
James Clerk Maxwell (1871) realized that because the four thermodynamic potentials ($U, H, F, G$) are exact state functions, their mixed second partial derivatives must commute by Schwarz's theorem:
2. Systematic Derivations from Fundamental Differentials
1. First Maxwell Relation (from Internal Energy $U(S, V)$):
Since $dU$ is exact:
Equating mixed second derivatives $\frac{\partial^2 U}{\partial V \partial S} = \frac{\partial^2 U}{\partial S \partial V}$:
2. Second Maxwell Relation (from Enthalpy $H(S, P)$):
Equating $\frac{\partial^2 H}{\partial P \partial S} = \frac{\partial^2 H}{\partial S \partial P}$:
3. Third Maxwell Relation (from Helmholtz Free Energy $F(T, V)$):
Equating $\frac{\partial^2 F}{\partial V \partial T} = \frac{\partial^2 F}{\partial T \partial V}$:
4. Fourth Maxwell Relation (from Gibbs Free Energy $G(T, P)$):
Equating $\frac{\partial^2 G}{\partial P \partial T} = \frac{\partial^2 G}{\partial T \partial P}$:
3. Max Born's Mnemonic Square
To quickly reconstruct these relations, Max Born proposed the mnemonic square:
$$\begin{array}{ccc} -V & & P \\ F & & H \\ -T & & S \end{array} \quad \text{or mnemonic: "Good Physicists Have Studied Under Very Fine Teachers"}$$
The potentials flank the edges between their natural variables. Arrow directions encode negative signs.
§5.2 The Clausius-Clapeyron Equation
1. Phase Coexistence Equilibrium
Consider two distinct macroscopic phases of a pure substance (e.g., liquid 1 and vapor 2) coexisting in dynamic phase equilibrium at temperature $T$ and pressure $P$. Equilibrium requires equality of their specific Gibbs free energies (chemical potentials):
If temperature shifts by an infinitesimal $dT$, the equilibrium coexistence pressure must shift along the phase line by $dP$ such that:
Expanding in total differentials $dg = -s dT + v dP$:
Rearranging terms:
2. The Latent Heat Formula
The entropy change during a reversible phase transformation at constant temperature $T$ is related to the latent heat $L$ per mole by $\Delta s = L / T$:
This is the Clausius-Clapeyron Equation.
3. Physical Applications
1. Boiling Point Elevation with Pressure: For vaporization, $v_{\text{vapor}} \gg v_{\text{liquid}} \implies \Delta v > 0$. Since vaporization is endothermic ($L > 0$), $\frac{dP}{dT} > 0$. Increasing pressure elevates the boiling point (utilized in pressure cookers and autoclave sterilization).
2. Depression of Freezing Point of Water: For water, ice has a lower density than liquid water at $0^\circ\text{C}$ ($v_{\text{water}} < v_{\text{ice}} \implies \Delta v = v_{\text{water}} - v_{\text{ice}} < 0$). Because latent heat of fusion $L_f > 0$:
Applying pressure lowers the melting temperature of ice (facilitating glacier regelation and ice skating).
§5.3 Specific Heat Relations (Cp - Cv) & The Two TdS Equations
1. Derivation of the First TdS Equation
Let entropy be expressed as a function of temperature and volume, $S = S(T, V)$:
Multiplying by absolute temperature $T$:
Using the definition of isochoric heat capacity $C_v = T (\partial S/\partial T)_V$ and the Third Maxwell Relation $(\partial S/\partial V)_T = (\partial P/\partial T)_V$:
This is the First $T dS$ Equation.
2. Derivation of the Second TdS Equation
Now let entropy be expressed as a function of temperature and pressure, $S = S(T, P)$:
Multiplying by $T$:
Using isobaric heat capacity $C_p = T (\partial S/\partial T)_P$ and the Fourth Maxwell Relation $(\partial S/\partial P)_T = -(\partial V/\partial T)_P$:
This is the Second $T dS$ Equation.
3. Rigorous Derivation of $C_p - C_v$
Equating the First and Second $T dS$ equations:
Dividing by $dT$ at constant pressure ($dP = 0$):
Expressing in terms of thermal expansion coefficient $\alpha = \frac{1}{V}(\partial V/\partial T)_P$ and isothermal compressibility $\kappa_T = -\frac{1}{V}(\partial V/\partial P)_T$, with the cyclic identity $(\partial P/\partial T)_V = \alpha / \kappa_T$:
§5.4 The Energy Equations & Internal Pressure
1. The First Energy Equation (Volume Dependence of U)
From the First Law, $dU = T dS - P dV$. Dividing by $dV$ at constant temperature $T$:
Substituting the Third Maxwell Relation $(\partial S/\partial V)_T = (\partial P/\partial T)_V$:
This is the First Energy Equation. The term $(\partial U/\partial V)_T$ is called the internal pressure ($P_i$), representing the internal force per unit area exerted by intermolecular attractive forces.
Examples:
1. Ideal Gas: $P = nRT / V \implies (\partial P/\partial T)_V = nR/V$.
proving Joule's law theoretically without approximations.
2. Van der Waals Gas: $P = \frac{n R T}{V - n b} - \frac{n^2 a}{V^2} \implies (\partial P/\partial T)_V = \frac{n R}{V - n b}$.
Internal energy increases during isothermal expansion as intermolecular bonds stretch.
2. The Second Energy Equation (Pressure Dependence of H)
From enthalpy $dH = T dS + V dP$, dividing by $dP$ at constant temperature $T$:
Substituting the Fourth Maxwell Relation $(\partial S/\partial P)_T = -(\partial V/\partial T)_P$:
This is the Second Energy Equation. For an ideal gas, $(\partial V/\partial T)_P = V/T$, so $(\partial H/\partial P)_T = 0$.
§5.5 Joule-Kelvin Throttling & Inversion Temperature
1. The Porous Plug Throttling Experiment
In the Joule-Thomson (Joule-Kelvin) experiment (1852), a continuous gas stream under steady high pressure $P_1$ is forced through an insulated porous plug or throttling valve to a lower pressure $P_2$.
- Upstream work done on the gas by piston: $W_1 = -P_1 V_1$.
- Downstream work done by the gas on piston: $W_2 = +P_2 V_2$.
- Net work done by gas: $W = P_2 V_2 - P_1 V_1$.
- Because the tube is thermally insulated, $Q = 0$.
By the First Law:
A throttling process is strictly isenthalpic ($\Delta H = 0$).
2. Derivation of the Joule-Thomson Coefficient
The Joule-Thomson Coefficient $\mu_{\text{JT}}$ is the rate of temperature change with pressure under constant enthalpy:
By the cyclic permutation identity for $(T, P, H)$:
Substituting the Second Energy Equation $(\partial H/\partial P)_T = V - T(\partial V/\partial T)_P$:
3. Joule-Thomson Cooling for Real Gases
1. Ideal Gas: $(\partial V/\partial T)_P = V/T \implies \mu_{\text{JT}} = 0$ (no temperature change).
2. Van der Waals Gas: Using $(P + a/V_m^2)(V_m - b) \approx RT$, we find:
- Cooling Zone ($\mu_{\text{JT}} > 0$): Since $dP < 0$ across the throttle, $dT = \mu_{\text{JT}} dP < 0$. Gas cools if $T < T_i$.
- Heating Zone ($\mu_{\text{JT}} < 0$): Gas heats up upon throttling if $T > T_i$.
- Temperature of Inversion $T_i$: The boundary where $\mu_{\text{JT}} = 0$:
For air, $T_i \approx 600\text{ K}$ (cools at room temperature). For hydrogen ($T_i \approx 200\text{ K}$) and helium ($T_i \approx 40\text{ K}$), pre-cooling below their inversion temperatures is mandatory before throttling can produce liquefaction.
Rigorous Analytical & Numerical Solved Problems
Comprehensive step-by-step mathematical proofs, dimensional evaluations, and calculations matching B.Sc. Honors university examinations.
At standard atmospheric pressure $P_0 = 1.013\times 10^5\text{ Pa}$, water boils at $T_0 = 373.15\text{ K}$ ($100.0^\circ\text{C}$) with a specific latent heat of vaporization of $L_v = 2.257\times 10^6\text{ J/kg}$. The specific volume of steam is $v_{\text{steam}} = 1.673\text{ m}^3\text{/kg}$, while the specific volume of liquid water is $v_{\text{water}} = 1.043\times 10^{-3\text{ m}^3\text{/kg}$. (a) Calculate the rate of change of boiling point with pressure $dT/dP$ at $100^\circ\text{C}$. (b) If atmospheric pressure at a high-altitude mountain station is $P = 70.0\text{ kPa}$, estimate the boiling temperature of water at that station using the integrated Clausius-Clapeyron equation.
From the Clausius-Clapeyron equation:
Inverting to obtain $dT/dP$:
Every $1\text{ kPa}$ drop in pressure lowers the boiling point of water by $0.0276^\circ\text{C}$.
Approximating steam as an ideal gas ($v_{\text{steam}} \approx R T / P M$) and neglecting $v_{\text{liquid}}$:
Molar latent heat: $L_{v, m} = L_v \times M = (2.257 \times 10^6)(0.018015\text{ kg/mol}) = 40660\text{ J/mol}$.
(a) $dT/dP = 2.76\times 10^{-4}\text{ K/Pa} = 27.6\text{ mK/kPa}$. (b) At $70.0\text{ kPa}$, water boils at $T = 362.9\text{ K}$ ($89.8^\circ\text{C}$), a drop of over $10^\circ\text{C}$ below standard sea-level boiling.
Liquid water at initial temperature $T_1 = 293.15\text{ K}$ ($20.0^\circ\text{C}$) and atmospheric pressure $P_1 = 1.0\text{ bar}$ ($1.0\times 10^5\text{ Pa}$) is compressed reversibly and adiabatically to a final pressure of $P_2 = 1000.0\text{ bar}$ ($1.0\times 10^8\text{ Pa}$). Over this pressure range, the average density is $\rho = 1010\text{ kg/m}^3$, isobaric specific heat capacity is $c_p = 4180\text{ J/(kg}\cdot\text{K)}$, and thermal expansion coefficient is $\alpha = 2.10\times 10^{-4}\text{ K}^{-1}$. Derive the adiabatic heating formula $\left(\frac{\partial T}{\partial P}\right)_S = \frac{T v \alpha}{c_p}$ and calculate the final water temperature $T_2$.
From the Second $T dS$ equation:
For a reversible adiabatic process, $dS = 0$:
Recalling the definition of thermal expansion coefficient $\alpha = \frac{1}{v} \left(\frac{\partial v}{\partial T}\right)_P \implies \left(\frac{\partial v}{\partial T}\right)_P = v \alpha$:
This confirms that compressing any substance with positive thermal expansion ($\alpha > 0$) adiabatically raises its temperature.
Assuming $T \approx T_1$ in the derivative because $\Delta T$ is small relative to $T_1$:
Given values:
Final temperature:
Despite an enormous pressure increase of $1000\text{ bar}$, water heats by only $1.46^\circ\text{C}$ due to its high density, large heat capacity, and low thermal expansion.
Formula derived: $\left(\frac{\partial T}{\partial P}\right)_S = \frac{T v \alpha}{c_p}$. Temperature increase is $\Delta T = +1.46\text{ K}$, yielding final temperature $T_2 = 294.61\text{ K}$ ($21.46^\circ\text{C}$).
For gaseous nitrogen ($\text{N}_2$), the Van der Waals constants are $a = 0.137\text{ J}\cdot\text{m}^3\text{/mol}^2$ and $b = 3.87\times 10^{-5}\text{ m}^3\text{/mol}$, and the molar heat capacity at constant pressure is $C_p = 29.12\text{ J/(mol}\cdot\text{K)}$. (a) Calculate the maximum inversion temperature $T_i$ for nitrogen. (b) Calculate the Joule-Thomson coefficient $\mu_{\text{JT}}$ at $T = 300.0\text{ K}$. (c) If nitrogen at $300.0\text{ K}$ is throttled from $P_1 = 150.0\text{ bar}$ to $P_2 = 1.0\text{ bar}$, calculate the temperature drop $\Delta T$ across the porous plug.
For a Van der Waals gas, the inversion temperature at zero pressure is:
Because room temperature ($300\text{ K}$) is well below $851.6\text{ K}$, nitrogen will cool upon throttling.
The theoretical Joule-Thomson coefficient for a Van der Waals gas is:
Each bar of pressure reduction across the throttle drops the nitrogen temperature by $0.244^\circ\text{C}$.
The pressure drop across the porous plug is:
Final temperature downstream of throttle:
This significant cooling illustrates the physical basis for industrial regenerative air liquefaction (the Linde-Hampson process).
(a) Maximum inversion temperature $T_i = 851.6\text{ K}$ ($578.4^\circ\text{C}$). (b) At $300\text{ K}$, $\mu_{\text{JT}} = 0.244\text{ K/bar}$. (c) Throttling across $149\text{ bar}$ produces a cooling of $\Delta T = -36.4\text{ K}$, reaching $263.6\text{ K}$ ($-9.6^\circ\text{C}$).