2.2 Temperature and equipartition
The pressure derivation of 2.1 ended on a striking identity: the mean translational kinetic energy of a molecule is . Temperature, the macroscopic quantity, is a measure of microscopic kinetic energy. This lesson generalises that statement into the equipartition theorem and uses it to read off the heat capacity of a gas.
Temperature as mean energy
A monatomic molecule stores energy only in its translation, — three independent quadratic terms, one per direction. With , each direction carries on average. That the share is the same for every direction, and for every molecule regardless of mass, is the first instance of a general rule.
The equipartition theorem
Every quadratic term in a system’s energy carries, on average, in thermal equilibrium. The translational , a rotational , the kinetic and potential terms and of a vibration — each is one such term, and each gets the same .
▶ ½α⟨q²⟩ = ½kᴮT — the equipartition integral Derivation
For a coordinate entering the energy as , the Boltzmann-weighted mean is
The denominator is the Gaussian integral . The numerator follows by differentiating the denominator with respect to :
The ratio is , independent of the stiffness . ✓
The independence from is the heart of the theorem: a stiffer coordinate has a narrower Boltzmann distribution (smaller ), but the mean energy is unchanged. That is what makes equipartition a clean accounting tool — count the quadratic terms, multiply by .
Vary α: the parabola widens or narrows, and the Gaussian narrows or widens in compensation. The integral of energy × density is *unchanged* at fixed T; it always equals ½kBT. This is equipartition — each quadratic degree of freedom contributes exactly ½kBT regardless of stiffness.
Vary at fixed : the parabola widens or narrows, the Gaussian narrows or widens in compensation, and the area under the integrand is invariant — always .
Heat capacity and the ratio of specific heats
Counting the active quadratic terms — the degrees of freedom — gives the internal energy , the molar heat capacity at constant volume , and (with Mayer’s relation ) the ratio of specific heats :
| Molecule | Active DOF at room | | | | |---|---|---|---|---| | Monatomic (He, Ar) | 3 (translation) | | | | | Diatomic (N₂, O₂) | 5 (3 trans. + 2 rot.) | | | | | Triatomic (CO₂, H₂O) | 6+ | | | |
The vibrational degrees of freedom of N₂ and O₂ are frozen out at room temperature: the energy quantum of the molecular vibration is much larger than , so the oscillator sits in its ground state and contributes nothing to the heat capacity. This is the first sign that classical equipartition is incomplete — it overcounts the energy of stiff oscillators, and the correction is quantum: a mode whose energy quantum exceeds is frozen in its ground state and drops out of the count. Classically, though, equipartition is exact, and it fixes for a gas from nothing but a count of its molecular degrees of freedom.