Heat Capacity at Constant Volume
Also known as: Isochoric Heat Capacity · C_v
Heat capacity at constant volume measures the energy needed to raise temperature when no work is done — pure internal energy storage.
Molecules vibrate harder with T; U(T) grows linearly, marker moves.
Equivalent forms
Equipartition makes a complicated quantity trivially countable — just count degrees of freedom and multiply by R/2.
Unit systems
Where it holds
Dimensional analysis
Black first distinguished heat from temperature; Joule's mechanical-equivalent experiments and Clausius's energy formulation in 1850 unified heat capacities into the thermodynamic definition.
Why does a steel pot heat faster than the water inside it?
1.5 mol of monatomic He gas is heated at constant volume. How much heat raises T by 40 K?
- Bomb calorimetry (combustion at constant V)
- Specific heat measurements in materials science
- Atmospheric thermodynamics — heating of trapped air parcels
- Cryogenic engineering
- C_v is not the heat capacity of an isolated system — it's defined for a process at constant V
- For solids and liquids, because volume changes negligibly, but the distinction matters for gases
- Equipartition fails at low T — Einstein and Debye models explain behavior of solids
Limiting cases
What if…
You need twice the heat for the same — heat capacity is extensive.
C_v jumps to 7R/2 for diatomic gases — equipartition adds 2 more quadratic terms per vibrational mode.
Quantum effects freeze degrees of freedom; as solids (Debye law) and exponentially for gases.
Heat for 1.5 mol He, ΔT = 40 K
- n:
- 1.5
- C v:
- 12.47
- ΔT:
- 40
- He is monatomic
ΔT of diatomic N₂ given Q
- n:
- 2
- Q:
- 1000
- C v:
- 20.785
- diatomic
- Rearrange: