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Thermal unit · institution-dependent · Interactive lesson

Molar heat capacities and equipartition

A gas has two heat capacities because heating it at constant pressure also pays for pushing the atmosphere back, and the first law prices that work at exactly R per mole per kelvin. Their ratio γ fixes how steep an adiabat is, and it drifts with temperature, because the measured CV climbs in steps as rotation and then vibration thaw, breaking the classical count mode by mode.

UPIII-07.03 · Lesson 3 of 9 in this unit. Position is not a completion score.
Starting model: Molar heat capacities and equipartitionC_V in units of R against temperature on a log axis from 1 K to 10⁴ K for a diatomic gas with θ_rot = 3 K and θ_vib = 3400 K: 3/2 from translation, an Einstein step near 2θ_rot for the two rotational terms (a smooth stand-in for the exact rotational curve) and a second near θ_vib for the vibrational pair. Dashed lines mark the 3/2, 5/2 and 7/2 plateaus; the marker is at T = 316 K.CV / RT = 316 K CV = 2.50 R γ = 1.4003/2 R translation only5/2 R + rotation7/2 R + vibration1 K100 K10⁴ Kθᵣₒₜθvib
Start with a picture. Change the model in the lab below.

Thermal unit · institution-dependent. Many departments teach thermal physics separately or within Physics II. Check whether your university includes this numbered unit in Physics III.

1

Build the model

The expansion costs exactly R per mole per kelvin; the modes that thaw set the rest.

The key idea

The molar heat capacity is the heat needed per mole per kelvin of temperature rise, CV with the volume held fixed and Cₚ with the pressure held fixed; for an ideal gas Cₚ − CV = R exactly.

Example. Warming 1.00 mol of argon by 10.0 K takes 125 J at constant volume (CV = 3R/2 = 12.5 J K⁻¹ mol⁻¹) but 208 J at constant pressure; the extra 83 J is the work of pushing back 0.82 L of atmosphere.

The complete physical model and assumptions

Heat capacity measures how much energy a mole must absorb per kelvin, and for a gas the answer depends on what you hold fixed. An ideal gas has an internal energy that depends on temperature alone, so CV = (1/n)(∂U/∂T)V is really a statement about U: ΔU = nCVΔT on every path. Heating at constant pressure costs more, because the gas expands and does work pΔV = nRΔT on its surroundings, which is where Cₚ = CV + R comes from. The ratio γ = Cₚ/CV = 1 + R/CV is what an adiabatic process feels: with no heat flowing, all the compression work stays in U, so a reversible adiabat is steeper than the isotherm through the same point by exactly γ, and sound, too quick to exchange heat, travels at √(γRT/M). The size of CV itself comes from the kinetic-theory unit's equipartition count, ½kT per active quadratic term, so CV = (f/2)R and γ = 1 + 2/f. The count works for argon (f = 3, γ = 1.67) and fails visibly for nitrogen, whose seven classical terms would give γ = 1.29 while 1.40 is measured. The failure is quantum: a vibrational spacing ħω of 0.29 eV cannot be bought with kT = 0.026 eV, so the mode sits in its ground state and stores nothing. The quantum oscillator gives that mode a heat capacity R x² eˣ/(eˣ − 1)² with x = ħω/kT, which tends to R when kT ≫ ħω — recovering the classical count, as correspondence demands — and to zero when kT ≪ ħω. So f is not an integer a molecule owns but an effective count that climbs with temperature, and the classical model stops working exactly where kT falls below a level spacing.

1Two heat capacities because heat depends on the path

Heat is not a state function, so “the heat capacity of nitrogen” is undefined until you say what was held fixed while the heat went in. Hold the volume fixed and no work is done, so the first law gives Q = ΔU and CV = (1/n)(∂U/∂T)V. Hold the pressure fixed and the gas expands against its surroundings, so Q = ΔU + pΔV; the combination U + pV is the enthalpy H, and Cₚ = (1/n)(∂H/∂T)ₚ. The partial derivatives matter: U and H are functions of two variables, and the subscript says which one is being held still. For an ideal gas one fact is decisive. Joule's free expansion showed that U depends on T alone, not on V, so dU = nCV dT holds on every path — isobaric, adiabatic, any curve on the p-V plane — even though CV was defined at constant volume. Argon has CV = 12.47 J K⁻¹ mol⁻¹, so 2.00 mol warming by 25 K gains 624 J of internal energy however it was heated.

2Where the R comes from

Heat 1 mol of ideal gas by dT at constant pressure. With work counted as done by the gas, the first law reads dQ = dU + p dV. The first term is CV dT on any path. The second is the expansion work, and the equation of state fixes it: with p constant, p dV = d(pV) = R dT. So dQ = (CV + R) dT, and Cₚ − CV = R with no assumption about the molecules at all. That R is the work per kelvin per mole spent pushing the atmosphere back: at 101 kPa, one mole heated by 10 K at constant pressure swells by ΔV = RΔT/p = 8.2 × 10⁻⁴ m³, about 0.82 L, and does 83 J of work. For a general substance the gap is Cₚ − CV = TVα²/κT, with α the volume expansivity in K⁻¹ and κT the isothermal compressibility in Pa⁻¹; copper at 298 K gives 0.7 J K⁻¹ mol⁻¹, about 3% of its CV, which is why solids are usually quoted with one heat capacity and gases must always be quoted with two. Dimensions check: K × m³ × K⁻² × Pa = J K⁻¹, per mole once V is molar.

3What γ does in an adiabatic process

How large CV is for a particular molecule is a counting question, and the kinetic-theory topic Equipartition and molar heat capacities of gases (UPIII-06.08) has answered it: ½kT per active quadratic term, so CV = (f/2)R, 3R/2 for a monatomic gas and 5R/2 for a diatomic whose vibration is frozen. The first law uses that number through the ratio γ = Cₚ/CV = 1 + R/CV, and uses it hardest where no heat flows. On a reversible adiabat, with work counted as done by the gas, 0 = nCV dT + p dV: every joule of compression work stays in U, so a gas with a larger CV warms less for the same squeeze. Differentiate pV = nRT to get p dV + V dp = nR dT, eliminate dT, and CV V dp = −(CV + R)p dV. Mayer's relation turns the bracket into Cₚ, so dp/p = −γ dV/V: the adiabat is steeper than the isotherm through the same point, where dp/p = −dV/V, by exactly the factor γ. Integrating that into pVγ = constant, and finding its work, belongs to the next topic; what matters here is that γ can be measured. Sound is a compression too quick for heat to cross half a wavelength, so the stiffness it feels is the adiabatic γp rather than the isothermal p. The isothermal estimate √(RT/M) gives 290 m s⁻¹ for air at 293 K; the factor √1.40 = 1.18 lifts it to the measured 343 m s⁻¹. Invert the relation and a sound speed is a heat-capacity measurement, CV = R/(γ − 1). Nitrogen at 300 K has γ = 1.40, so CV = 20.8 J K⁻¹ mol⁻¹, the f = 5 value, where all seven classical terms would give 29.1 J K⁻¹ mol⁻¹ and γ = 9/7 = 1.29. Two terms are missing.

4The missing terms: a quantum ħω that kT cannot pay for

The classical Boltzmann average behind equipartition lets a vibrating bond take any energy at all. A quantum oscillator cannot: its energies are ħω(v + ½), spaced by ħω, and thermal agitation lifts it out of the ground state only if kT is comparable to that spacing. Boltzmann-weighting the ladder gives a mean thermal energy ⟨ε⟩ = ħω/(eˣ − 1) with x = ħω/kT = θvib/T, and differentiating with respect to T gives the mode's heat capacity, Cvib = R x² eˣ/(eˣ − 1)² per mole. Both limits check. For x → 0, eˣ − 1 ≈ x and the bracket tends to 1: Cvib → R, the classical pair of terms, so the quantum result contains the classical one as it must. For x → ∞ it tends to R x² e(−x), which vanishes exponentially: the mode is frozen. Nitrogen's stretch has ħω = 0.29 eV and θvib = 3390 K. At 300 K, x = 11.3 and Cvib = 0.0016 R — a part in a thousand, invisible to a calorimeter. At 1000 K, x = 3.39 and the mode already carries 0.41 R, so CV = 2.91 R = 24.2 J K⁻¹ mol⁻¹ and γ has fallen to 1.34. Nothing switched; the mode thawed.

5Rotation freezes too, and γ reports the whole count

Rotation has its own quantum. A rigid rotor's levels are EJ = J(J + 1)kθᵣₒₜ with θᵣₒₜ = ħ²/(2Ik), and the first excited level sits 2θᵣₒₜ above the ground state. For most gases θᵣₒₜ is tiny — 2.9 K for N₂, 2.1 K for O₂ — so rotation is fully classical at any temperature at which the substance is a gas. Hydrogen is the exception: its moment of inertia is so small that θᵣₒₜ = 85 K, and near 25 K hydrogen gas measures CV ≈ 3R/2 and γ ≈ 1.66, behaving like a monatomic gas because its molecules cannot afford to spin. The running total is what γ = 1 + R/CV reports, and the speed of sound reads it directly: v = √(γRT/M) gives 353 m s⁻¹ in nitrogen at 300 K with γ = 1.40, and would give 338 m s⁻¹ if γ were 9/7. A resonance tube is therefore a thermometer for degrees of freedom. Read CV(T) as a staircase on a logarithmic temperature axis — 3R/2, then 5R/2 above a few θᵣₒₜ, then 7R/2 above a few θvib — with each riser smeared over roughly a decade of temperature, never a step at one point.

6The same count in a crystal, and where the count ends

A crystal is the limiting case of a molecule whose terms are all vibrational. Each atom sits in a three-dimensional harmonic well, three kinetic and three potential terms, f = 6, so equipartition predicts CV = 3R = 24.9 J K⁻¹ mol⁻¹ for every monatomic solid — the Dulong–Petit law, and copper, silver and lead all sit within a few per cent of it at room temperature. Diamond does not: its stiff, light lattice has vibrational temperatures near 2000 K, so at 298 K it holds only 6.1 J K⁻¹ mol⁻¹, a quarter of the classical value, and every solid's heat capacity falls towards zero as T → 0, as the third law requires. The rule is the same everywhere: a mode contributes its classical share once kT exceeds its level spacing by a factor of a few, and almost nothing when kT is a few times smaller. Equipartition is not wrong; it is the high-temperature limit of the quantum count, and the temperature at which a given mode joins in is set by ħω/k, which spectroscopy hands you directly.

2

Key equations

Read the units, assumptions and limits before substituting.

Heat capacity at constant volume

CV = (1/n)(∂U/∂T)V

It names how fast internal energy grows with temperature. Nothing about it needs the volume fixed once U depends on T alone.

molar, J K⁻¹ mol⁻¹; n in mol, U in J, T in K. Ideal gas: U = U(T) only, so ΔU = nCVΔT on every path

Heat capacity at constant pressure

Cₚ = (1/n)(∂H/∂T)ₚ, with H = U + pV

Constant-pressure heat also pays for expansion work, and the enthalpy bookkeeps that work automatically.

H is the enthalpy in J, p in Pa, V in m³; at constant p the heat supplied equals ΔH, so Q = nCₚΔT

Mayer's relation for an ideal gas

Cₚ − CV = R

The R is the work pΔV = nRΔT done per mole per kelvin pushing the surroundings back. For copper the analogous gap is only 0.7 J K⁻¹ mol⁻¹.

R = 8.314 J K⁻¹ mol⁻¹; true for every ideal gas, whatever its molecules

Heat-capacity ratio

γ = Cₚ/CV = 1 + R/CV

It is the factor by which a reversible adiabat is steeper than an isotherm, dp/dV = −γp/V against −p/V, so it sets the speed of sound v = √(γRT/M), with M in kg mol⁻¹ and T in K.

dimensionless; 5/3 = 1.67 monatomic, 7/5 = 1.40 rigid diatomic, 9/7 = 1.29 diatomic with vibration

Heat capacities from a measured γ

CV = R/(γ − 1), Cₚ = γR/(γ − 1)

Mayer's relation fixes the difference and γ the ratio, so one sound-speed measurement yields both heat capacities: γ = 1.40 gives 20.8 and 29.1 J K⁻¹ mol⁻¹, no calorimeter needed.

J K⁻¹ mol⁻¹; R = 8.314 J K⁻¹ mol⁻¹, γ dimensionless; ideal gas, from Cₚ − CV = R and Cₚ = γCV together

Einstein function for one vibrational mode

Cvib = R x² eˣ/(eˣ − 1)², with x = θvib/T = ħω/kT

Tends to R for T ≫ θvib, the classical pair of terms, and to R x² e(−x) → 0 for T ≪ θvib. The mode is frozen, not absent.

x dimensionless, ω in rad s⁻¹; θvib = ħω/k in K: N₂ 3390 K, O₂ 2260 K, Cl₂ 810 K, H₂ 6330 K
3

Interactive lab

Predict first. Explore the model. Compare the result.

Explore the model

2.50
0 to 4; steps of 0.05.
3 K
2 to 90 K; steps of 1.
3400 K
300 to 6500 K; steps of 50.

Try this. Set θᵣₒₜ = 85 K and θvib = 6300 K for hydrogen, then slide log T from 1.3 (20 K) to 2.5 (316 K): CV climbs from 1.5R towards 2.5R while γ falls from 1.66 to 1.40. Then park log T at 2.5 and drag θvib from 3400 K down to 300 K to see nitrogen with a vibrational quantum eleven times smaller.

Live results

CV
20.81 J K⁻¹ mol⁻¹
Cₚ = CV + R
29.12 J K⁻¹ mol⁻¹
γ = Cₚ / CV
1.400
ACTIVE f = 2CV/R
5.00

Results follow this lesson’s model and assumptions. Displayed values are rounded.

Interactive Physics III modelC_V in units of R against temperature on a log axis from 1 K to 10⁴ K for a diatomic gas with θ_rot = 3 K and θ_vib = 3400 K: 3/2 from translation, an Einstein step near 2θ_rot for the two rotational terms (a smooth stand-in for the exact rotational curve) and a second near θ_vib for the vibrational pair. Dashed lines mark the 3/2, 5/2 and 7/2 plateaus; the marker is at T = 316 K.CV / RT = 316 K CV = 2.50 R γ = 1.4003/2 R translation only5/2 R + rotation7/2 R + vibration1 K100 K10⁴ Kθᵣₒₜθvib
CV in units of R against temperature on a log axis from 1 K to 10⁴ K for a diatomic gas with θᵣₒₜ = 3 K and θvib = 3400 K: 3/2 from translation, an Einstein step near 2θᵣₒₜ for the two rotational terms (a smooth stand-in for the exact rotational curve) and a second near θvib for the vibrational pair. Dashed lines mark the 3/2, 5/2 and 7/2 plateaus; the marker is at T = 316 K.

Predict → change one variable → check

Plan a change before running it. Every other input stays at the saved baseline.

Saved baseline. Temperature log₁₀(T / K): 2.50; Rotational temperature θᵣₒₜ: 3 K; Vibrational temperature θvib: 3400 K

Baseline 2.50; choose 0 to 4, in steps of 0.05.
4. Compared with the saved baseline, this result will…

This experiment is kept only while this page is open. It does not change saved course progress.

4

Catch the common trap

First-year students meet CV alongside constant-volume heating and conclude that ΔU = nCVΔT is allowed only when the volume is fixed, then reach for nCₚΔT as the internal-energy change of an isobaric process. That double-counts the work. For an ideal gas U depends on temperature alone, so ΔU = nCVΔT on every path; what changes between paths is the heat, not ΔU. Heat 2.00 mol of nitrogen by 40 K at constant pressure and 2328 J go in, but only 1663 J = 2.00 × (5/2)R × 40 K stays as internal energy — the other 665 J left again as expansion work. Cₚ is not the heat capacity that goes with U at constant pressure; it is CV plus the price of the expansion.

5

Practice & worked examples

3 authored examples. Make an attempt, then reveal the reasoning one step at a time.

EasyExample 1

A cylinder with a free piston holds 2.50 mol of argon at atmospheric pressure. It is warmed from 290 K to 340 K. Find the rise in internal energy, the heat supplied and the work done by the gas.

Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.

0 of 4 steps revealed.

MediumExample 2

A resonance tube filled with carbon dioxide (M = 44.0 g mol⁻¹) at 300 K gives a speed of sound of 270 m s⁻¹. Using v = √(γRT/M), find γ, CV, Cₚ and the effective number of active quadratic terms, then compare with the full classical count for a linear triatomic molecule.

Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.

0 of 5 steps revealed.

HardExample 3

0.800 mol of oxygen (θvib = 2260 K) is heated at constant volume from 300 K to 1500 K. Treating the vibration as a harmonic mode, find the heat required exactly, compare it with the rigid-rotor and fully classical estimates, and give γ at 1500 K.

Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.

0 of 6 steps revealed.

6

Quick check

Select an answer and explain it before checking.

One mole of nitrogen, treated as an ideal gas with rotation active and vibration frozen, is heated from 300 K to 350 K at constant pressure. Heat Q = 1455 J flows in. By how much does the internal energy rise?
7

Review & continue

The molar heat capacity is the heat needed per mole per kelvin of temperature rise, CV with the volume held fixed and Cₚ with the pressure held fixed; for an ideal gas Cₚ − CV = R exactly.

  • Explain the relationship without looking at the equation.
  • Check a sign, a unit and a model assumption in your working.
  • Return to the lab or worked example if a step is still unclear.

Extra challenging questions

Connect several ideas, explore supplied data, and compare your reasoning with a worked solution.