This page is the workshop. On the parent note Heat capacities Cp, Cv you learned why C p > C v and how Mayer's relation is born. Here we hammer it against every case the topic can throw at you — every gas type, the constant-volume and constant-pressure paths, the degenerate limits (solids, real gases), a word problem, and an exam twist.
Before we begin, one promise: every symbol used below was defined on the parent note. As a quick reminder in plain words:
Recall The four symbols we lean on
C v ::: heat to warm 1 mole by 1 K at fixed volume — units J mol − 1 K − 1 .
C p ::: heat to warm 1 mole by 1 K at fixed pressure — always bigger than C v .
R ::: the gas constant, 8.314 J mol − 1 K − 1 — the "expansion tax" per mole per kelvin.
γ ::: the ratio C p / C v , the adiabatic index.
Every question on this topic lives in exactly one of these cells. The examples below are labelled with the cell they cover.
#
Cell class
What makes it distinct
Example
A
Monatomic gas (He, Ar)
C v = 2 3 R , γ = 3 5
Ex 1
B
Diatomic gas (N₂, O₂)
C v = 2 5 R , γ = 5 7
Ex 2
C
Polyatomic gas (CO₂, CH₄)
more [[Degrees of Freedom
degrees of freedom]], γ → 1
D
Two paths, same Δ T
compare Q V vs Q P , extract the work
Ex 4
E
Reverse problem
given C p or γ , back out C v
Ex 5
F
Degenerate: solid/liquid
C p − C v = R ; expansion work ≈ 0
Ex 6
G
Degenerate: real gas
van der Waals correction to Mayer
Ex 7
H
Word problem (real world)
heating air in a room / balloon
Ex 8
I
Exam twist
mixture of gases, or "which γ ?" identity
Ex 9
J
Limiting behaviour
γ as degrees of freedom → ∞
Ex 10
The figure below shows the single geometric fact that unifies cells A–D: at constant pressure the gas pushes a piston , and that push is the entire difference between C p and C v .
Look at the red arrow — it is the piston's outward motion. The energy stored in that motion, per mole per kelvin, is exactly R .
Worked example Helium: find
C p and γ from C v
Given: Helium, a monatomic ideal gas, C v = 2 3 R .
Find: C p and γ .
Forecast: Guess first — will γ be nearer 1 or nearer 2? (Monatomic = fewest ways to store energy, so γ is at its maximum .)
Apply Mayer: C p = C v + R = 2 3 R + R = 2 5 R .
Why this step? Mayer's relation is exact for any ideal gas — the gas type only sets C v , never the + R .
Numbers: C p = 2 5 ( 8.314 ) = 20.785 J mol − 1 K − 1 .
Why this step? Converts the symbolic answer into the value an exam grader wants.
Ratio: γ = C v C p = 3/2 R 5/2 R = 3 5 ≈ 1.667 .
Why this step? γ controls adiabatic curves; it is the headline number for a gas.
Verify: γ = 1 + C v R = 1 + ( 3/2 ) R R = 1 + 3 2 = 3 5 ✓. Units cancel (R / R ), so γ is dimensionless ✓.
Worked example Nitrogen: heat at both paths
Given: 2 mol of N₂ (C v = 2 5 R ), warmed from 300 K to 350 K.
Find: Q V (constant volume) and Q P (constant pressure).
Forecast: Which is bigger, and by how much? Predict the gap in joules before computing.
Δ T = 350 − 300 = 50 K .
Why this step? Both formulas scale with the temperature change; fix it once.
Constant volume: Q V = n C v Δ T = 2 ⋅ 2 5 ( 8.314 ) ⋅ 50 = 2078.5 J .
Why this step? At fixed V no work is done, so all heat becomes Internal Energy : Q V = Δ U .
Constant pressure: C p = C v + R = 2 7 R , so Q P = 2 ⋅ 2 7 ( 8.314 ) ⋅ 50 = 2909.9 J .
Why this step? At fixed P the gas also does expansion work, needing extra heat.
Verify: The gap Q P − Q V = 2909.9 − 2078.5 = 831.4 J must equal n R Δ T = 2 ( 8.314 ) ( 50 ) = 831.4 J ✓ — the expansion tax, exactly as the first law predicts.
Worked example Carbon dioxide: more freedoms, smaller
γ
Given: CO₂ modelled with C v = 3 R (translational + rotational fully active).
Find: C p and γ ; compare to helium.
Forecast: Will γ be above or below the diatomic 1.40 ?
C p = 3 R + R = 4 R .
Why this step? Same + R tax, larger base C v .
γ = 3 R 4 R = 3 4 ≈ 1.333 .
Why this step? Comparing this to He's 1.667 shows the trend: more degrees of freedom → γ closer to 1.
Verify: γ = 1 + 3 R R = 1 + 3 1 = 3 4 ✓. And 1.333 < 1.400 < 1.667 orders correctly by freedom count ✓.
Worked example Where did the extra heat go?
Given: 1 mol monatomic gas, Δ T = 100 K , heated once at fixed V , once at fixed P .
Find: the work done at constant pressure, and confirm it equals the heat difference.
Forecast: Guess the work in joules (R Δ T per mole) before reading on.
Δ U = n C v Δ T = 1 ⋅ 2 3 ( 8.314 ) ⋅ 100 = 1247.1 J .
Why this step? Δ U = n C v Δ T holds for an ideal gas on any path — a fact worth over-using (see Mistake 3 on parent).
Constant-pressure work: W = P Δ V = n R Δ T = 1 ( 8.314 ) ( 100 ) = 831.4 J .
Why this step? Differentiating P V = n R T at fixed P gives P d V = n R d T ; this is the piston push in the figure.
Q P = Δ U + W = 1247.1 + 831.4 = 2078.5 J .
Why this step? Direct first-law bookkeeping: heat in = energy stored + work out.
Verify: Q P should also equal n C p Δ T = 1 ⋅ 2 5 ( 8.314 ) ( 100 ) = 2078.5 J ✓ — two routes, one answer.
Worked example Identify the gas from
C p
Given: an ideal gas has C p = 29.10 J mol − 1 K − 1 .
Find: C v , γ , and name the likely gas type.
Forecast: Will γ land near 1.67 , 1.40 , or 1.33 ?
C v = C p − R = 29.10 − 8.314 = 20.786 J mol − 1 K − 1 .
Why this step? Mayer's relation rearranged — always subtract exactly R .
γ = 20.786 29.10 = 1.400 .
Why this step? γ is the fingerprint that classifies the molecule.
Read off: γ ≈ 1.40 ⇒ diatomic (N₂, O₂), rotations active, vibrations frozen.
Why this step? Maps the number back to physical structure.
Verify: C v = 2 5 R = 20.785 ✓ and C p = 2 7 R = 29.099 ✓ — consistent with the diatomic model.
C p − C v = R for water
Given: liquid water, specific c p = 4.18 J g − 1 K − 1 , molar mass M = 18 g mol − 1 . The real solid/liquid relation is C p − C v = κ T T V α 2 .
Find: molar C p , and explain why plugging into C p − C v = R is wrong.
Forecast: For a liquid, will C p − C v be near R (8.3) or near zero?
Molar C p = c p ⋅ M = 4.18 × 18 = 75.24 J mol − 1 K − 1 .
Why this step? Mistake 2 on the parent — never mix per-gram and per-mole.
A liquid barely expands on heating, so Δ V ≈ 0 , hence the expansion work P d V ≈ 0 .
Why this step? The whole + R came from ideal-gas expansion; kill the expansion, kill the R .
Therefore C p ≈ C v for water, and C p − C v = R = 8.314 would be badly wrong here.
Why this step? Marks the boundary of Mayer's validity — cell F is the "does not apply" cell.
Verify: Using measured constants for water at 298 K (α ≈ 2.1 × 1 0 − 4 K − 1 , molar V ≈ 1.8 × 1 0 − 5 m 3 , κ T ≈ 4.6 × 1 0 − 10 Pa − 1 ): κ T T V α 2 ≈ 0.51 J mol − 1 K − 1 , which is ≪ 8.314 ✓ — nowhere near R .
Worked example A whiff of van der Waals
Given: For a van der Waals gas, to first order C p − C v ≈ R ( 1 + R T V m 2 a ) where V m is molar volume. Take CO₂: a = 0.364 Pa m 6 mol − 2 , T = 300 K , V m = 0.025 m 3 mol − 1 .
Find: the fractional correction to R .
Forecast: Big correction or tiny? (Hint: at low pressure a real gas ≈ ideal.)
Compute R T V m 2 a = ( 8.314 ) ( 300 ) ( 0.025 ) 2 ( 0.364 ) .
Why this step? This dimensionless number is the size of the departure from ideal Mayer.
= 62.355 0.728 = 0.01168 , i.e. about a 1.2% correction.
Why this step? Quantifies "how non-ideal" — small here because V m is large (dilute gas).
Verify: C p − C v ≈ 8.314 ( 1.01168 ) = 8.411 J mol − 1 K − 1 , just above R ✓ — real attractions make the tax slightly higher than ideal.
Worked example Heating the air in a room
Given: A sealed rigid room holds n = 100 mol of air (treat as diatomic, C v = 2 5 R ). A heater raises the temperature by Δ T = 5 K .
Find: the heat supplied, and what changes if instead a window is open (constant pressure).
Forecast: Sealed vs open — which needs more heat for the same 5 K rise?
Sealed (rigid = constant volume): Q V = n C v Δ T = 100 ⋅ 2 5 ( 8.314 ) ⋅ 5 = 10392.5 J .
Why this step? A rigid room can't expand, so this is the pure Δ U case.
Open window (air free to expand at atmospheric P ): Q P = n C p Δ T = 100 ⋅ 2 7 ( 8.314 ) ⋅ 5 = 14549.5 J .
Why this step? Now warm air pushes out through the window — expansion work is paid.
Verify: Difference = 14549.5 − 10392.5 = 4157.0 J , which must equal n R Δ T = 100 ( 8.314 ) ( 5 ) = 4157.0 J ✓ — the open-window "energy leak" is precisely the expansion tax.
Worked example Mixture of two gases
Given: A mixture of n 1 = 2 mol helium (C v , 1 = 2 3 R ) and n 2 = 3 mol nitrogen (C v , 2 = 2 5 R ).
Find: the effective γ mix .
Forecast: Will γ mix sit between 1.40 and 1.67 ? (It must — it's a weighted blend.)
Total C v = n 1 C v , 1 + n 2 C v , 2 = 2 ( 2 3 R ) + 3 ( 2 5 R ) = 3 R + 7.5 R = 10.5 R .
Why this step? Heat capacities are extensive — moles of each gas add their storage.
Total C p = C v + ( n 1 + n 2 ) R = 10.5 R + 5 R = 15.5 R .
Why this step? Every mole pays one R of expansion tax, so add ( n 1 + n 2 ) R .
γ mix = 10.5 R 15.5 R = 21 31 = 1.4762 .
Why this step? Ratio of the total capacities gives the mixture's adiabatic index.
Verify: 1.400 < 1.476 < 1.667 ✓ — the blend lies strictly between its ingredients, as any weighted average must.
Worked example What happens as degrees of freedom grow?
Given: A gas with f active degrees of freedom has C v = 2 f R .
Find: γ ( f ) and its limit as f → ∞ .
Forecast: Toward what number does γ creep as molecules get more complex?
C p = 2 f R + R = 2 f + 2 R .
Why this step? Same + R , now written for general f .
γ ( f ) = f /2 ( f + 2 ) /2 = f f + 2 = 1 + f 2 .
Why this step? A clean formula showing γ decreasing with f .
Limit: as f → ∞ , f 2 → 0 , so γ → 1 .
Why this step? Confirms the trend seen in Ex 1→3: monatomic (f = 3 ) at top, very complex molecules approaching γ = 1 .
Verify: Check the known cases: f = 3 ⇒ γ = 1 + 3 2 = 3 5 ✓; f = 5 ⇒ γ = 1 + 5 2 = 5 7 ✓; f = 6 ⇒ γ = 3 4 ✓.
Recall Rapid self-test
Extra heat for constant-P vs constant-V over Δ T , n moles ::: n R Δ T
γ for a diatomic gas ::: 7/5 = 1.40
Does C p − C v = R hold for liquid water? ::: No — negligible expansion, C p ≈ C v
γ as degrees of freedom → ∞ ::: approaches 1