Transport Phenomena and Phase Transition
Boltzmann transport equation, H-theorem and arrow of time, mean free path, viscosity, thermal conductivity, diffusion, Brownian motion, Ehrenfest phase transition classification, Clausius-Clapeyron, and mean-field Ising model.
§7.1 The Boltzmann Transport Equation
1. Phase-Space Distribution Function ($f(\mathbf{r}, \mathbf{p}, t)$)
Let $f(\mathbf{r}, \mathbf{p}, t) \, d^3\mathbf{r} \, d^3\mathbf{p}$ be the number of particles in physical volume element $d^3\mathbf{r}$ with momenta in $d^3\mathbf{p}$ at time $t$. In the absence of interparticle collisions, particles flow smoothly through phase space according to Hamilton's equations $\mathbf{v} = \mathbf{p}/m$ and $\dot{\mathbf{p}} = \mathbf{F}$: $$f(\mathbf{r} + \mathbf{v}\delta t, \, \mathbf{p} + \mathbf{F}\delta t, \, t + \delta t) = f(\mathbf{r}, \mathbf{p}, t)$$2. The Collision Term
Interparticle collisions abruptly scatter particles into and out of the phase-space volume element: $$f(\mathbf{r} + \mathbf{v}\delta t, \, \mathbf{p} + \mathbf{F}\delta t, \, t + \delta t) - f(\mathbf{r}, \mathbf{p}, t) = \left( \frac{\partial f}{\partial t} \right)_{\text{coll}} \delta t$$ Expanding the left side in a first-order Taylor series yields the **Boltzmann Transport Equation**: $$\frac{\partial f}{\partial t} + \mathbf{v} \cdot \boldsymbol{\nabla}_{\mathbf{r}} f + \frac{\mathbf{F}}{m} \cdot \boldsymbol{\nabla}_{\mathbf{v}} f = \left( \frac{\partial f}{\partial t} \right)_{\text{coll}}$$3. The Relaxation-Time (BGK) Approximation
Because the exact non-linear collision integral involves 5-dimensional integration over collision cross sections, Bhatnagar, Gross, and Krook (1954) introduced the widely used **Relaxation-Time Approximation**: $$\left( \frac{\partial f}{\partial t} \right)_{\text{coll}} \approx -\frac{f(\mathbf{r}, \mathbf{v}, t) - f_0(\mathbf{v})}{\tau}$$ where $f_0(\mathbf{v})$ is the local equilibrium Maxwell-Boltzmann distribution, and $\tau$ is the characteristic collision relaxation time. Any local perturbation decays exponentially back to equilibrium as $e^{-t/\tau}$.§7.2 The Boltzmann H-Theorem and the Arrow of Time
1. Definition of the $H$-Function
Boltzmann defined the functional $H(t)$ for a gas with velocity distribution $f(\mathbf{v}, t)$: $$H(t) \equiv \int f(\mathbf{v}, t) \ln f(\mathbf{v}, t) \, d^3\mathbf{v}$$ Because statistical entropy is $S = -k_B \int f \ln f \, d^3\mathbf{v}$, Boltzmann's $H$-function is directly proportional to negative entropy: $$S(t) = -k_B H(t) + \text{constant}$$2. Derivation of $dH/dt \le 0$
Using the exact binary collision integral and the principle of detailed balance (microscopic time-reversibility of collisions $\mathbf{v}_1, \mathbf{v}_2 \leftrightarrow \mathbf{v}_1', \mathbf{v}_2'$): $$\frac{dH}{dt} = -\frac{1}{4} \int \dots \int (f_1' f_2' - f_1 f_2) \ln\left( \frac{f_1' f_2'}{f_1 f_2} \right) \sigma \, |\mathbf{v}_1 - \mathbf{v}_2| \, d\Omega \, d^3\mathbf{v}_1 \, d^3\mathbf{v}_2$$ Because for any positive numbers $x, y$, the inequality $(x - y)\ln(x/y) \ge 0$ holds strictly (being zero if and only if $x = y$): $$\frac{dH}{dt} \le 0 \iff \frac{dS}{dt} \ge 0$$Boltzmann's H-Theorem: The functional $H(t)$ decreases monotonically over time until the gas attains the Maxwell-Boltzmann distribution, where $dH/dt = 0$. Consequently, macroscopic entropy can never decrease!
3. Resolution of Historical Paradoxes
- Loschmidt's Time-Reversal Paradox (Umkehreinwand): If Newton's laws are time-reversible, reversing all velocities should make entropy decrease. Resolution: The H-theorem assumes the Molecular Chaos Hypothesis (Stoßzahlansatz)—that velocities of colliding particles are uncorrelated before collision. Reversing velocities introduces exquisite fine-tuned microscopic correlations that violate this hypothesis.
- Zermelo's Recurrence Paradox (Wiederkehreinwand): Poincaré's theorem states any bounded mechanical system must return arbitrarily close to its initial microstate. Resolution: For $10^{23}$ particles, the Poincaré recurrence time is $\sim 10^{10^{23}}$ years—vastly longer than the age of the universe!
§7.3 Mean Free Path and Kinetic Collision Theory
1. Collision Cross Section
Model gas molecules as hard spheres of diameter $d$. A collision occurs whenever the centers of two molecules approach within distance $d$. The collision cross section is the area of a disk of radius $d$: $$\sigma = \pi d^2$$2. Derivation of the Mean Free Path
If a molecule moves with relative speed $\bar{v}_{\text{rel}}$, in time $\Delta t$ its collision cross section sweeps out a cylinder of volume $\Delta V = \sigma \bar{v}_{\text{rel}} \Delta t$. If the number density of scatterers is $n = N/V$, the number of collisions is: $$\Delta N_{\text{coll}} = n \Delta V = n \pi d^2 \bar{v}_{\text{rel}} \Delta t$$ For a thermal gas, the average relative speed between two randomly oriented molecules is $\bar{v}_{\text{rel}} = \sqrt{2} \bar{v}$. The collision frequency is: $$\nu_{\text{coll}} = \frac{\Delta N_{\text{coll}}}{\Delta t} = \sqrt{2} \pi n d^2 \bar{v}$$ The mean free path is the average speed divided by collision frequency: $$\lambda = \frac{\bar{v}}{\nu_{\text{coll}}} = \frac{1}{\sqrt{2} \pi n d^2}$$ Using the ideal gas law $P = n k_B T$: $$\lambda = \frac{k_B T}{\sqrt{2} \pi d^2 P}$$ At room temperature and atmospheric pressure for air ($d \approx 3.7\text{ Å}$): $$\lambda \approx 68\text{ nm}$$ Molecules travel hundreds of times their own diameter between collisions!§7.4 Viscosity, Thermal Conductivity, and Diffusion in Gases
1. Dynamic Viscosity ($\eta$): Momentum Transport
Consider a gas with a shear flow velocity gradient $\frac{du_x}{dy}$. Molecules crossing plane $y$ from a mean free path distance $\pm \lambda$ carry momentum $m u_x(y \pm \lambda)$. The shear stress is: $$\tau_{xy} = -\frac{1}{3} n m \bar{v} \lambda \frac{du_x}{dy} = -\eta \frac{du_x}{dy}$$ $$\eta = \frac{1}{3} \rho \bar{v} \lambda = \frac{1}{3} (n m) \bar{v} \left( \frac{1}{\sqrt{2} \pi n d^2} \right) = \frac{m \bar{v}}{3 \sqrt{2} \pi d^2} = \frac{\sqrt{m k_B T}}{3 \pi^{3/2} d^2}$$Maxwell's Paradox: Notice that density $n$ cancels out completely! The viscosity of a dilute gas is completely independent of pressure and density! $$\left(\frac{\partial \eta}{\partial P}\right)_T = 0$$ Furthermore, gas viscosity increases with temperature ($\eta \propto \sqrt{T}$), unlike liquids whose viscosity drops with temperature.
2. Thermal Conductivity ($\kappa$): Heat Energy Transport
For a temperature gradient $\frac{dT}{dz}$, molecules transport thermal energy $c_v m T$: $$J_q = -\kappa \frac{dT}{dz}, \quad \kappa = \frac{1}{3} n c_v m \bar{v} \lambda = \frac{1}{3} C_V \rho \bar{v} \lambda = \frac{c_v \sqrt{m k_B T}}{3 \pi^{3/2} d^2}$$ Thermal conductivity is also independent of gas pressure.3. Self-Diffusion Coefficient ($D$): Mass Transport
For a concentration gradient $\frac{dn}{dz}$, the particle flux is given by Fick's Law: $$J_N = -D \frac{dn}{dz}, \quad D = \frac{1}{3} \bar{v} \lambda = \frac{2}{3 \pi^{3/2} d^2} \frac{\sqrt{k_B T / m}}{n} \propto \frac{T^{3/2}}{P}$$ Unlike viscosity, diffusion is inversely proportional to pressure.§7.5 Electrical Conductivity and the Drude-Sommerfeld Model
1. The Drude-Sommerfeld Conductivity Formula
In an electric field $\mathbf{E}$, conduction electrons experience acceleration $\mathbf{a} = -e\mathbf{E}/m^*$. Collisions with lattice phonons and impurities randomize momentum with relaxation time $\tau$. The steady-state drift velocity is: $$\mathbf{v}_d = -\frac{e \tau}{m^*} \mathbf{E}$$ The electric current density is given by Ohm's Law $\mathbf{J} = -n e \mathbf{v}_d = \sigma \mathbf{E}$, yielding: $$\sigma = \frac{n e^2 \tau}{m^*}$$2. The Wiedemann-Franz Law and Lorenz Number
In metals, conduction electrons transport both electric charge and thermal heat. The electronic thermal conductivity is $\kappa_{\text{el}} = \frac{1}{3} C_V^{\text{el}} v_F^2 \tau$. Using the Sommerfeld linear electronic heat capacity $C_V^{\text{el}} = \frac{\pi^2}{2} n k_B (T / T_F)$: $$\kappa_{\text{el}} = \frac{1}{3} \left( \frac{\pi^2}{2} \frac{n k_B^2 T}{\epsilon_F} \right) \left( \frac{2\epsilon_F}{m^*} \right) \tau = \frac{\pi^2 n k_B^2 T \tau}{3 m^*}$$ Dividing thermal conductivity $\kappa$ by electrical conductivity $\sigma$: $$\frac{\kappa}{\sigma T} = \frac{\pi^2}{3} \left( \frac{k_B}{e} \right)^2 \equiv L$$ This is the celebrated **Wiedemann-Franz Law** (1853). The ratio is a universal physical constant known as the **Lorenz Number**: $$L = \frac{\pi^2}{3} \left( \frac{k_B}{e} \right)^2 = 2.443 \times 10^{-8}\text{ W}\cdot\Omega\text{/K}^2$$ This universal constant holds remarkably across copper, silver, gold, and aluminum at room temperature!§7.6 Brownian Motion and the Langevin Stochastic Equation
1. The Langevin Equation (Paul Langevin, 1908)
A microscopic particle of mass $m$ and radius $a$ suspended in a fluid experiences two forces:- A macroscopic viscous drag force: $-\gamma v = -6\pi \eta a v$ (Stokes' Law).
- A fluctuating, stochastic force $\xi(t)$ due to billions of thermal molecular collisions.
2. Derivation of Mean Squared Displacement (Einstein, 1905)
Multiplying the Langevin equation by $x$ and taking ensemble averages: $$m \left\langle x \frac{dv}{dt} \right\rangle = -\gamma \langle x v \rangle + \langle x \xi \rangle$$ Using $\frac{d}{dt}(x^2) = 2xv$ and $\frac{d}{dt}(xv) = v^2 + x\frac{dv}{dt}$: $$\frac{m}{2} \frac{d^2}{dt^2} \langle x^2 \rangle - m \langle v^2 \rangle = -\frac{\gamma}{2} \frac{d}{dt} \langle x^2 \rangle$$ By the equipartition theorem, $m \langle v^2 \rangle = k_B T$. In the overdamped regime ($t \gg m/\gamma$): $$\frac{\gamma}{2} \frac{d}{dt} \langle x^2 \rangle = k_B T \implies \frac{d}{dt} \langle x^2 \rangle = \frac{2 k_B T}{\gamma}$$ Integrating over time: $$\langle x^2(t) \rangle = 2 D t$$ where $D$ is the **Einstein Diffusion Coefficient**: $$D = \frac{k_B T}{\gamma} = \frac{k_B T}{6\pi \eta a}$$ By tracking the displacement $\langle x^2 \rangle$ of gamboge particles under a microscope, Jean Perrin measured Boltzmann's constant $k_B$ and calculated Avogadro's number $N_A$, winning the 1926 Nobel Prize for proving the reality of atoms!§7.7 Thermodynamic Classification of Phase Transitions and Clausius-Clapeyron
1. The Ehrenfest Classification of Phase Transitions
Paul Ehrenfest (1933) classified phase transitions by the lowest order derivative of Gibbs free energy $G(T, P)$ that exhibits a mathematical discontinuity:- First-Order Phase Transitions: Discontinuity in the first derivatives of $G$: $$\Delta S = -\Delta \left(\frac{\partial G}{\partial T}\right)_P \ne 0, \quad \Delta V = \Delta \left(\frac{\partial G}{\partial P}\right)_T \ne 0$$ Characterized by a non-zero **Latent Heat** $L = T \Delta S$ and a discontinuous change in volume/density $\Delta V$. Examples: Ice melting, water boiling, sublimation.
- Second-Order (Continuous) Phase Transitions: First derivatives are continuous (no latent heat: $\Delta S = 0, \Delta V = 0$), but second derivatives diverge or jump discontinuously: $$C_P = -T \left(\frac{\partial^2 G}{\partial T^2}\right)_P, \quad \kappa_T = -\frac{1}{V} \left(\frac{\partial^2 G}{\partial P^2}\right)_T, \quad \alpha = \frac{1}{V} \frac{\partial^2 G}{\partial T \partial P}$$ Examples: Ferromagnetic Curie transition, superconductor-normal transition in zero field, superfluid He-II $\lambda$-transition.
2. The Clausius-Clapeyron Equation
Along a first-order phase coexistence boundary curve $P(T)$, the two phases ($1$ and $2$) have identical chemical potential: $$dG_1 = dG_2 \implies -S_1 dT + V_1 dP = -S_2 dT + V_2 dP$$ Rearranging gives the **Clausius-Clapeyron Equation**: $$\frac{dP}{dT} = \frac{S_2 - S_1}{V_2 - V_1} = \frac{\Delta S}{\Delta V} = \frac{L}{T \Delta V}$$ Because ice expands when freezing ($V_{\text{ice}} > V_{\text{water}} \implies \Delta V < 0$), the melting curve of ice has a negative slope ($dP/dT < 0$), allowing ice skates to glide on a thin liquid layer!§7.8 Mean-Field Theory of the Ising Model
1. The Microscopic Ising Hamiltonian
Consider a crystal lattice where each site $i$ has an Ising spin $s_i = \pm 1$ (spin up or spin down): $$H = -J \sum_{\langle i, j \rangle} s_i s_j - h \sum_i s_i$$ where $J > 0$ is the ferromagnetic exchange coupling between nearest neighbors $\langle i, j \rangle$, and $h = g \mu_B B$ is an external magnetic field.2. Weiss Molecular Mean-Field Approximation
In Mean-Field Theory (MFT), we approximate the fluctuating neighbor spins $s_j$ by their average expectation value $\langle s \rangle = m$ (the **order parameter**): $$s_i s_j = (s_i - m + m)(s_j - m + m) \approx m s_i + m s_j - m^2$$ For a lattice with coordination number $z$ (number of nearest neighbors per site): $$H_{\text{MF}} = -\sum_i s_i (h + z J m) + \frac{1}{2} N z J m^2 = -\sum_i s_i h_{\text{eff}} + \frac{1}{2} N z J m^2$$ where $h_{\text{eff}} = h + z J m$ is the effective **Weiss molecular field**.3. The Self-Consistency Equation
The single-spin partition function is: $$z_1 = e^{\beta h_{\text{eff}}} + e^{-\beta h_{\text{eff}}} = 2 \cosh(\beta h_{\text{eff}})$$ The average magnetization per site is: $$m = \langle s_i \rangle = \frac{e^{\beta h_{\text{eff}}} - e^{-\beta h_{\text{eff}}}}{z_1} = \tanh(\beta h_{\text{eff}})$$ Substituting $h_{\text{eff}} = h + z J m$: $$m = \tanh\left( \frac{z J m + h}{k_B T} \right)$$4. Spontaneous Magnetization and Critical Curie Temperature
In zero external field ($h = 0$): $$m = \tanh\left( \frac{z J}{k_B T} m \right)$$ For high temperatures, the slope of $\tanh(x)$ at $x = 0$ is less than $1$: the only solution is $m = 0$ (paramagnetic phase). A non-trivial solution ($m \ne 0$) emerges when the slope at the origin exceeds $1$: $$\left.\frac{d}{dm}\tanh\left(\frac{z J m}{k_B T}\right)\right|_{m=0} = \frac{z J}{k_B T} > 1$$ This defines the **Curie Transition Temperature**: $$T_c = \frac{z J}{k_B}$$ For $T < T_c$, spontaneous symmetry breaking occurs: the spins spontaneously align into a macroscopic ferromagnet with $m \propto (T_c - T)^{1/2}$ near $T_c$ (mean-field critical exponent $\beta = 1/2$).📝 Chapter Worked Examples & Exercises
Complete derivations & analytical proofsAt an altitude of $100\text{ km}$ in the thermosphere (the Kármán line), the atmospheric pressure is $P = 0.032\text{ Pa}$ and the temperature is $T = 200\text{ K}$. Assuming an effective molecular diameter $d = 3.7 \times 10^{-10}\text{ m}$ and average molecular mass $m = 4.8 \times 10^{-26}\text{ kg}$ (diatomic nitrogen). (a) Calculate the number density $n$ and the mean free path $\lambda$. (b) Determine the average collision frequency $\nu_{\text{coll}}$.
This establishes the molecular density at the edge of outer space.
At $100\text{ km}$ altitude, the mean free path is over $14\text{ centimeters}$, compared to $68\text{ nanometers}$ at sea level. Aerodynamic continuum fluid mechanics breaks down, requiring Knudsen rarefied gas dynamics.
Molecules collide only a few thousand times per second, compared to billions of collisions per second at sea level.
In a Brownian motion experiment, spherical colloidal particles of radius $a = 0.50\,\mu\text{m}$ are suspended in water at $T = 293\text{ K}$ (viscosity $\eta = 1.00 \times 10^{-3}\text{ Pa}\cdot\text{s}$). (a) Calculate the diffusion coefficient $D$. (b) If the observed root-mean-square displacement in the $x$-direction over time $t = 60\text{ s}$ is $\sqrt{\langle x^2 \rangle} = 7.18\,\mu\text{m}$, calculate Boltzmann's constant $k_B$ and Avogadro's number $N_A = R / k_B$ (taking $R = 8.314\text{ J/(mol}\cdot\text{K)}$).
This gives the experimental diffusion coefficient of the microscopic colloidal particles.
This directly yields Boltzmann's constant.
The experimental measurement yields $N_A \approx 6.02 \times 10^{23}\text{ mol}^{-1}$, proving that thermal fluctuations are caused by discrete microscopic atoms.
At atmospheric pressure ($P_0 = 1.013 \times 10^5\text{ Pa}$), water boils at $T_0 = 373.15\text{ K}$ with latent heat of vaporization $L = 2.260 \times 10^6\text{ J/kg}$ (molar latent heat $L_m = 40.68\text{ kJ/mol}$). At the summit of Mount Everest ($8,848\text{ m}$), atmospheric pressure drops to $P = 3.37 \times 10^4\text{ Pa}$. (a) Assuming the vapor behaves as an ideal gas and $V_{\text{vapor}} \gg V_{\text{liquid}}$, derive the integrated Clausius-Clapeyron equation. (b) Calculate the boiling point of water on Mount Everest.
Because the volume of steam is over 1600 times greater than liquid water, liquid volume can be neglected.
This gives the vapor pressure curve as a function of temperature.
On Mount Everest, water boils at only $71.1^\circ\text{C}$ ($160^\circ\text{F}$), illustrating the dramatic pressure dependence predicted by the Clausius-Clapeyron equation.