Equipartition, and the low-temperature failure that demanded quanta
Statement
Each quadratic degree of freedom contributes ½kBT to the mean energy of a classical system — and the observed failure of this rule at low temperature is direct evidence for energy quantisation.
Why it matters
This one line predicts the heat capacity of every classical system by counting: three translational terms for a gas atom, more for rotation and vibration, six per atom for a solid. It works beautifully at room temperature and then, on cooling, it breaks in a way classical physics cannot repair. That breakage was recognised as fundamental before it was explained, and it is one of the cleanest fingerprints of quantisation in all of thermodynamics.
Assumptions
Derivation
Result
Reading. Monatomic gas: three translational terms give U = 3⁄2 NkBT, CV = 3⁄2 NkB. A diatomic gas adds two rotational terms → 5⁄2 NkB; adding the vibrational mode (kinetic and potential, two more terms) would give 7⁄2 NkB. A solid with three vibrational modes per atom, each counted twice, gives C = 3NkB — the Dulong–Petit law.
Units check. kB carries energy per kelvin, so kBT is an energy; the ½ is dimensionless, and a has cancelled, leaving ⟨ε⟩ as a pure energy per degree of freedom. Correct.
Limiting cases
- High temperature (kBT ≫ ℏω): the exponential in step 4 expands and ⟨E⟩ → kBT, recovering equipartition exactly. The classical rule is a limit, not a wrong theory.
- Low temperature (kBT ≪ ℏω): the second term is exponentially suppressed and the mode contributes essentially nothing — it is frozen out.
- Measured diatomic heat capacities sit at 5⁄2 NkB at room temperature, not 7⁄2; solids fall below 3NkB on cooling, tending to zero as T³.
Breaks when
- Level spacing is comparable to or larger than kBT — the whole point above.
- The energy is not quadratic — an ultra-relativistic gas has ε = pc and gives kBT per momentum component, not ½.
- Applied to photons or phonons, where the mode count is not fixed — the naive application gives the ultraviolet catastrophe.
Failure modes
- Counting a vibrational mode once. It contributes twice, kinetic and potential — this halving error is extremely common.
- Assuming a degree of freedom that exists must be active. Existence and excitation are different questions, and the difference is ℏω⁄kBT.
- Presenting equipartition as simply wrong. It is exactly right in its regime, and knowing the regime is the physics.
Worked number
For CO (from D-010), ℏω = 0.27 eV and kBT = 0.026 eV at 300 K, so ℏω⁄kBT ≈ 10.4 and the vibrational contribution to CV is suppressed by roughly e−10.4 ≈ 3 × 10⁻⁵. The mode exists; it is simply never excited. Rotational spacings are far smaller (~10⁻⁴ eV), so rotations are fully active — which is exactly why the observed value is 5⁄2 NkB and not 7⁄2. Heat the gas above about 3,000 K and the vibrational contribution appears, as observed.
Plot CV(T) and overlay the classical limit →
Discussion
The arresting feature of the result is what is missing from it. The mean energy ⟨ε⟩ = ½kBT retains no trace of the constant a — not the stiffness of a spring, not the mass of a molecule, not the moment of inertia. The reason is visible if you substitute u = (βa)1/2x in both integrals of step 1: the factor a and the factor β always appear glued together in the combination βax², so a single rescaling of the dummy variable expels a from the problem entirely and leaves the answer a pure function of β. Physically, a stiff mode and a soft mode reach the same thermal energy at the same temperature; the stiff one simply sits with a smaller amplitude. Temperature, not the microscopic detail, is the shared currency of thermal contact, and it is spent equally on every quadratic term.
That "equally" is the whole content of the theorem, and it is why the result is structured as a flat ½kBT per term rather than something mode-dependent. The ½ is the fingerprint of a Gaussian phase-space measure: a quadratic energy makes the Boltzmann weight e−βax² a Gaussian, whose logarithm carries exactly one factor of ½lnβ, and −∂/∂β of that is 1/(2β). Change the power law and you change the fraction in a completely predictable way, which is the generalised equipartition theorem: for an energy term proportional to |x|s over the whole real line, ⟨ε⟩ = kBT/s. Quadratic (s = 2) gives ½; linear (s = 1), as for an ultra-relativistic particle, gives a full kBT.
Seen this way, equipartition and its collapse are a single organising principle running through classical and quantum statistical physics. The same "½kBT per quadratic slot" underlies the Dulong–Petit law for solids, the thermal (Johnson–Nyquist) voltage noise of a resistor — where ⟨½C V²⟩ = ½kBT fixes the mean-square fluctuation of a capacitor's voltage — and Einstein's 1905 account of Brownian motion, where ⟨½m v²⟩ = ½kBT per component ties a visible jiggle to kB. Its most famous failure, the ultraviolet catastrophe, is not a different disease: assigning kBT to each electromagnetic mode is exactly equipartition applied to an unbounded set of oscillators, and it diverges for precisely the reason a diatomic vibration freezes — the classical average ignores the discrete ladder En = (n+½)ħω. Whenever the level spacing ħω becomes comparable to kBT, the continuous integral of step 2 is no longer a legitimate stand-in for the sum, and the mode either freezes out (matter) or is exponentially cut off at high frequency (radiation). One inequality, ħω ≳ kBT, governs both.
Common misconceptions. The rule is ½kBT per quadratic term in the energy, not per particle and not loosely "per degree of freedom": a one-dimensional oscillator has a kinetic term and a potential term, so it carries kBT, and forgetting the potential half is the single most common error. A second confusion is treating a frozen mode as absent — the vibrational mode of room-temperature CO physically exists, it is simply never excited, and existence versus excitation is settled entirely by the ratio ħω/kBT. A third is calling equipartition "wrong". It is exactly correct in its regime — the high-temperature limit — and the quantum result reduces to it precisely there; knowing the regime is the physics.
Worked examples
Example 1 — Heat capacity of an Einstein solid below its Einstein temperature. Model copper as 3N independent quantum oscillators of a single frequency ω, with Einstein temperature θE = ħω/kB = 240 K. Find the molar heat capacity at T = 80 K and compare with the classical Dulong–Petit value.
Answer. At T = 80 K ≈ θE/3, roughly half of each oscillator's classical heat capacity has frozen out, giving CV ≈ 12.4 J mol−1 K−1 against the classical 24.9. Cool the copper further and CV collapses toward zero; the Einstein model gives an exponential fall, and the more accurate Debye model the observed T³.
Example 2 — A vibration that is not frozen: iodine gas at room temperature. The derivation showed CO's stiff bond (ħω ≈ 0.27 eV) is frozen at 300 K. Iodine, I2, has a much softer bond, vibrational wavenumber ν̃ = 214 cm−1. Find the vibrational contribution to its molar CV at 300 K and the total CV.
Answer. Because iodine's bond is soft, ħω ≈ kBT at room temperature and the vibration is nearly fully active, contributing 7.6 J mol−1 K−1. The molecule sits close to the classical (7/2)R that CO only reaches above ~3000 K — a direct, measurable demonstration that freeze-out is controlled by ħω/kBT and nothing else.
Problems
- Bookkeeping the quadratic terms. Using equipartition alone, predict the molar CV of (a) argon gas, (b) nitrogen gas at 300 K, (c) nitrogen with its vibration fully active, and (d) crystalline diamond. Give each as a multiple of R and in J mol−1 K−1.
Solution
(a) Monatomic: 3 translational terms → CV = (3/2)R = 12.5 J mol−1 K−1. (b) Diatomic with rotation active, vibration frozen: 3 translational + 2 rotational = 5 half-terms → (5/2)R = 20.8. (c) Add the vibrational mode (2 more terms, kinetic + potential) → (7/2)R = 29.1. (d) A solid has 3 vibrational modes per atom, each with 2 quadratic terms → 3R = 24.9 (Dulong–Petit). Diamond in fact sits far below this at 300 K because its θE is very high (~1300 K), a foreshadowing of Problem 4.
- The generalised theorem and a relativistic gas. For an energy term ε = A|x|s with x over the whole real line, prove ⟨ε⟩ = kBT/s. Then find U and CV for an ultra-relativistic monatomic gas (ε = pc for each of three momentum components), and compare with the ordinary non-relativistic gas.
Solution
Following step 2 of the derivation, ⟨ε⟩ = −∂/∂β ln ∫ e−βA|x|s dx. Substitute u = β1/sx, so dx = β−1/sdu and the integral becomes β−1/s ∫ e−A|u|s du, a constant times β−1/s. Then ln(...) = −(1/s)lnβ + const, and −∂/∂β gives 1/(sβ) = kBT/s. For quadratic s = 2 this is ½kBT; for the linear relativistic term s = 1 it is a full kBT per component. Three components give U = 3NkBT and CV = 3NkB = 3R = 24.9 J mol−1 K−1 — exactly double the non-relativistic (3/2)R. (This is why the interior of a hot, radiation-pressure-dominated star has an adiabatic index near 4/3 rather than 5/3.)
- Oxygen: nearly frozen, then thawing. The vibrational wavenumber of O2 is 1580 cm−1. Compute the fraction of the classical vibrational heat capacity active at (a) 300 K and (b) 2000 K. Take kBT/hc = 208.5 cm−1 at 300 K (and scale linearly with T).
Solution
Fraction active = x²ex/(ex−1)² with x = 1580/(kBT/hc). (a) At 300 K, x = 1580/208.5 = 7.58; e7.58 = 1957, so fraction = (57.4)(1957)/(1956)² = 1.123×10⁵/3.826×10⁶ = 0.029. Only ~3% active — essentially frozen, so O2 shows the expected (5/2)R at room temperature. (b) At 2000 K, kBT/hc = 208.5×(2000/300) = 1390 cm−1, x = 1580/1390 = 1.137; e1.137 = 3.117, fraction = (1.293)(3.117)/(2.117)² = 4.030/4.482 = 0.90. About 90% active. The vibration thaws over roughly a thousand kelvin, not abruptly.
- Where is a mode "half active"? Define a vibration as half active when CV,vib = R/2. Solve the transcendental condition for x = ħω/kBT numerically, then find the temperature at which O2 (1580 cm−1) reaches this point. Note 1 cm−1 ↔ 1.4388 K.
Solution
Require x²ex/(ex−1)² = ½. Iterate: at x = 2.90, value = 0.518; at x = 3.00, value = 0.496; interpolating gives x ≈ 2.98. So a mode is half-frozen when the thermal energy is about one third of the level spacing — freeze-out is well underway before kBT even reaches ħω. For O2, θvib = ħω/kB = 1580 × 1.4388 = 2273 K, so T½ = θvib/2.98 = 763 K. Below ~760 K the O2 vibration contributes less than half of R; the value 0.90R at 2000 K found in Problem 3 is consistent with this.
- The ultraviolet catastrophe as equipartition, and Planck's cure. The number of electromagnetic modes per unit volume with angular frequency in [ω, ω+dω] is dn = (ω²/π²c³) dω (two polarisations included). (a) Assign each mode the classical ⟨E⟩ = kBT and write the spectral energy density u(ω); show it diverges. (b) Replace ⟨E⟩ by the quantum-oscillator value from the derivation (drop the zero point) and obtain the Planck law; show it recovers part (a) when ħω ≪ kBT and is exponentially cut off when ħω ≫ kBT. (c) Integrate to recover the Stefan–Boltzmann T⁴ law.
Solution
(a) With ⟨E⟩ = kBT per mode, u(ω) = (ω²/π²c³)·kBT — the Rayleigh–Jeans law. It grows without bound as ω → ∞ and ∫u dω diverges: the ultraviolet catastrophe. This is precisely equipartition applied to infinitely many oscillators, exactly the assumption (continuous energy) flagged in the derivation. (b) The quantised mode has ⟨E⟩ = ħω/(eħω/kBT−1), so
u(ω) = ħω³ / [ π²c³ (eħω/kBT − 1) ]the Planck law. For ħω ≪ kBT, ex−1 ≈ x = ħω/kBT, and u → ω²kBT/π²c³, the Rayleigh–Jeans result — equipartition is the low-frequency limit. For ħω ≫ kBT the denominator ≈ eħω/kBT and u is exponentially suppressed — the same freeze-out that silences a stiff vibration silences the high-frequency modes, curing the catastrophe. (c) Total energy density U/V = ∫₀∞ u dω. Substitute y = ħω/kBT: U/V = (kBT)⁴/(π²c³ħ³) ∫₀∞ y³/(ey−1) dy. The integral is π⁴/15, giving U/V = (π²kB⁴/15ħ³c³) T⁴ — the Stefan–Boltzmann law, with the T⁴ dependence emerging entirely from the quantum cutoff that classical equipartition lacked.