
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.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.
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.
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 pathHeat 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 = nCₚΔTMayer'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 moleculesHeat-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 vibrationHeat 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 togetherEinstein 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 KInteractive lab
Predict first. Explore the model. Compare the result.
Explore the model
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.
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
This experiment is kept only while this page is open. It does not change saved course progress.
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.
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.
- Argon is monatomic: f = 3, so CV = 3R/2 = 12.47 J K⁻¹ mol⁻¹ and Cₚ = CV + R = 20.79 J K⁻¹ mol⁻¹. The rise is ΔT = 50 K.
- ΔU = nCVΔT = 2.50 × 12.47 × 50 = 1.56 × 10³ J. This holds whatever the path, because an ideal gas's U depends on T alone.
- The piston is free, so the pressure stays fixed and Q = nCₚΔT = 2.50 × 20.79 × 50 = 2.60 × 10³ J.
- W = Q − ΔU = 1.04 × 10³ J. Check it against the expansion work directly: pΔV = nRΔT = 2.50 × 8.314 × 50 = 1039 J. The ratio ΔU/Q = CV/Cₚ = 1/γ = 0.60: three-fifths of the heat is stored.
Answer. ΔU = 1.56 kJ, Q = 2.60 kJ, W = 1.04 kJ done by the gas — ΔU/Q = 3/5.
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.
- Invert the sound-speed relation: γ = v²M/(RT) = 270² × 0.0440 / (8.314 × 300) = 3208 / 2494 = 1.286.
- CV = R/(γ − 1) = 8.314 / 0.286 = 29.1 J K⁻¹ mol⁻¹ and Cₚ = γCV = 37.4 J K⁻¹ mol⁻¹; check Cₚ − CV = 8.3 J K⁻¹ mol⁻¹ = R.
- Effective count: f = 2/(γ − 1) = 6.99 ≈ 7.0 active quadratic terms.
- Classical count for linear CO₂: 3 translational + 2 rotational + 2 × (3N − 5 = 4) vibrational = 13, giving CV = 13R/2 = 54.0 J K⁻¹ mol⁻¹, γ = 15/13 = 1.154 and v = 256 m s⁻¹. The rigid-linear count f = 5 gives γ = 1.40 and v = 282 m s⁻¹. The measurement sits between.
- Translation and rotation supply 5 terms; the two degenerate bending modes (θvib = 960 K, x = 3.2) each contribute 0.45 R by the Einstein function, about 2 effective terms, while the stretches at θvib ≈ 1900 K and 3400 K add 0.07 R between them.
Answer. γ = 1.29, CV = 29.1 J K⁻¹ mol⁻¹, Cₚ = 37.4 J K⁻¹ mol⁻¹, feff ≈ 7.0 — not the classical 13. At 300 K the bends are thawing and the stretches are still frozen.
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.
- At constant volume Q = ΔU. Translation and rotation are classical throughout: their share is n(5/2)RΔT = 0.800 × 2.5 × 8.314 × 1200 = 1.995 × 10⁴ J.
- The vibrational contribution needs ∫Cvib dT, but Cvib is the derivative of the mode's mean energy, so the integral is already done: Uvib = Rθvib/(e(θvib/T) − 1) per mole, with Rθvib = 8.314 × 2260 = 1.879 × 10⁴ J mol⁻¹.
- At 300 K, x = 7.53, eˣ − 1 = 1868 and Uvib = 10.1 J mol⁻¹. At 1500 K, x = 1.507, eˣ − 1 = 3.512 and Uvib = 5.35 × 10³ J mol⁻¹.
- ΔUvib = 0.800 × (5350.6 − 10.1) = 4.27 × 10³ J, so Q = 1.995 × 10⁴ + 0.427 × 10⁴ = 2.42 × 10⁴ J.
- Rigid rotor alone (5R/2) gives 1.995 × 10⁴ J, 18% low; fully classical (7R/2) gives 0.800 × 3.5 × 8.314 × 1200 = 2.79 × 10⁴ J, 15% high. The mode is thawing across this range: its average contribution between 300 K and 1500 K is 0.54 R, neither 0 nor R.
- At 1500 K the Einstein bracket is x²eˣ/(eˣ − 1)² = 2.270 × 4.512 / 12.33 = 0.831, so CV = (2.5 + 0.831)R = 27.7 J K⁻¹ mol⁻¹, Cₚ = 36.0 J K⁻¹ mol⁻¹ and γ = 1.300, down from 1.395 at 300 K.
Answer. Q = 2.42 × 10⁴ J (24.2 kJ); the rigid-rotor estimate is 20.0 kJ and the classical one 27.9 kJ. At 1500 K, CV = 27.7 J K⁻¹ mol⁻¹ and γ = 1.30.
Quick check
Select an answer and explain it before checking.
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.