
Thermal unit · institution-dependent · Interactive lesson
Isothermal, isobaric, isochoric, and adiabatic processes
Each named process is a constraint that fixes one term in ΔU = Q − W, and for an ideal gas ΔU = nCVΔT is always free, so every ledger closes from the path alone. The adiabat is the one you must derive: integrate the first law with no heat and pVγ = constant falls out, together with the three assumptions it silently carries.
UPIII-07.04 · Lesson 4 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
Fix one thing and the first law collapses to a single line.
The key idea
A named gas process holds a single quantity fixed along the whole path — temperature, pressure, volume, or the heat transferred, which is zero — so that the first law fixes the remaining energy terms from the path alone.
Example. Compress 1.00 mol of argon (γ = 5/3) reversibly and adiabatically from 300 K to half its volume: T₂ = 300 K × 2²⁄³ = 476 K, and with Q = 0 the work done on the gas is nCVΔT = 12.47 J K⁻¹ × 176 K = 2.20 kJ.
The complete physical model and assumptions
The first law is one equation, ΔU = Q − W, with two path-dependent terms, so on its own it predicts nothing; a process becomes computable only when a constraint pins one term. The four named processes are the four useful constraints. Holding T fixed kills ΔU for an ideal gas, because U depends on T alone, so Q = W = nRT ln(V₂/V₁). Holding V fixed kills W, so Q = ΔU = nCVΔT, which is how CV is measured. Holding p fixed makes W = pΔV = nRΔT, and the extra R per mole in Cₚ is exactly that work. Forbidding heat flow kills Q, and the first law becomes a differential equation, nCV dT = −p dV; put in pV = nRT, separate the variables and integrate, and TV(γ−1) = constant, or pVγ = constant, is the adiabat, steeper than the isotherm through the same point by the factor γ. That derivation is honest about its price. It used U = U(T) and pV = nRT, so the gas must be ideal; it used a single pressure p at every instant, so the path must be reversible; and it pulled γ outside the integral, so CV must not change over the temperature range. Drop any one and the process may still be adiabatic, but pVγ no longer describes it: a free expansion has Q = 0 and lands back on the isotherm it started from.
1Declare the ledger before the constraint
Write the first law once, with its convention stated: ΔU = Q − W, where Q is heat into the gas and W = ∫p dV is work done by the gas. Two of the three terms depend on the path; only ΔU is a state function. For an ideal gas that state function is unusually simple, because Joule's expansion showed U depends on temperature alone: ΔU = nCVΔT on every path, isobaric and adiabatic included, not just at the constant volume where CV was defined. So the working routine for any named process is the same three lines. Find the end temperatures and write ΔU = nCVΔT. Evaluate W from the path, an integral the constraint usually makes trivial. Then Q = ΔU + W is the remainder, and its sign tells you which way heat flowed. Every named process below is this routine with one term made easy.
2Isothermal: the reservoir pays for every joule of work
Hold T fixed by keeping the gas in thermal contact with a large reservoir and moving the piston slowly enough that the gas never leaves that temperature. For an ideal gas ΔU = 0 at once, and p = nRT/V along the whole path, so W = ∫nRT dV/V = nRT ln(V₂/V₁). The logarithm is the signature of a pressure that falls as 1/V: doubling the volume costs the same work whatever volume you start from. Take 2.00 mol at 300 K expanding from 10.0 L to 20.0 L: W = 2.00 × 8.314 × 300 × ln 2 = 3.46 kJ done by the gas, and since ΔU = 0 the reservoir supplied exactly Q = +3.46 kJ. Compress instead and both signs flip: the same 3.46 kJ of work done on the gas leaves as heat. Isothermal is not the process with no heat. It is the process in which heat and work are equal, and it is slow by definition.
3Isobaric and isochoric: one ledger with W, one without
At constant volume the piston is clamped, ∫p dV = 0, and the heat is the whole story: QV = ΔU = nCVΔT. This is the measurement that defines CV. At constant pressure the gas must push the surroundings back as it warms, W = pΔV, and for an ideal gas pΔV = nRΔT, so the heat needed is Qₚ = nCVΔT + nRΔT = nCₚΔT with Cₚ = CV + R. Numbers make the split visible. Warm 1.00 mol of nitrogen (CV = 5R/2 = 20.8 J mol⁻¹ K⁻¹) by 50.0 K at constant pressure: Qₚ = 29.1 × 50.0 = 1.45 kJ enters, of which ΔU = 20.8 × 50.0 = 1.04 kJ stays as internal energy and W = 8.314 × 50.0 = 416 J leaves as work on the piston. Clamp the piston and the same 50.0 K rise needs only 1.04 kJ. The extra 416 J is not lost, it is the work you can watch the piston doing, and it is the whole reason Cₚ exceeds CV.
4Integrate the first law with Q = 0 to obtain the adiabat
Insulate the cylinder, or move the piston fast compared with the time heat needs to flow, and Q = 0. The first law then reads dU = −p dV for every infinitesimal step, and with dU = nCV dT and p = nRT/V that is nCV dT = −nRT dV/V. Separate the variables: dT/T = −(R/CV) dV/V. The ratio R/CV is (Cₚ − CV)/CV = γ − 1, so integrating from state 1 to state 2 gives ln(T₂/T₁) = −(γ − 1) ln(V₂/V₁), or TV(γ−1) = constant. Substitute T = pV/nR and pVγ = constant follows. Compare slopes at a shared point: on the isotherm dp/dV = −p/V, on the adiabat dp/dV = −γp/V, steeper by γ, because compressing without letting heat escape raises T as well as squeezing V, and both push p up. A limiting case checks the sign: γ → 1 means CV → ∞, a gas that absorbs unlimited energy without warming, and the adiabat collapses onto the isotherm.
5Adiabatic work and the temperature swing are one number
With p = K V(−γ) along the path, W = ∫p dV = K(V₂(1−γ) − V₁(1−γ))/(1 − γ) = (p₁V₁ − p₂V₂)/(γ − 1). Since Q = 0 this must also equal −ΔU = nCV(T₁ − T₂), and it does, because p₁V₁ − p₂V₂ = nR(T₁ − T₂) and R/(γ − 1) = CV. Try air (γ = 1.40) at 1.00 × 10⁵ Pa and 300 K in 1.00 L, compressed reversibly to 0.100 L: T₂ = 300 × 100.40 = 754 K and p₂ = 101.40 × 10⁵ Pa = 25.1 × 10⁵ Pa. The work is (100 J − 251 J)/0.40 = −378 J done by the gas, so 378 J was done on it, and every joule sits in the gas as internal energy. Check by the other route: n = p₁V₁/RT₁ = 0.0401 mol, CV = 20.8 J mol⁻¹ K⁻¹, ΔT = 454 K, nCVΔT = 378 J. That 754 K is why a diesel engine needs no spark plug, and why adiabatic compression always costs more work than isothermal compression to the same volume.
6The three assumptions pVγ carries, and what breaks each
The derivation borrowed three things, and pVγ = constant is only as good as all three. First, an ideal gas: U = U(T) and pV = nRT both entered, so near condensation or at high density the curve is wrong even if Q = 0 exactly. Second, a reversible path: the gas had a single pressure p at every instant, which requires the piston stroke to take far longer than the sound-crossing time of the cylinder while still being short compared with the time heat needs to leak out. Adiabatic is not the same as pVγ: a free expansion into vacuum has Q = 0 and W = 0, so ΔU = 0 and the ideal gas ends on its original isotherm, not on the adiabat. Third, a constant γ: pulling γ − 1 outside the integral needs CV independent of T. For nitrogen CV rises from 5R/2 towards 7R/2 as vibration wakes up above roughly 1000 K, so γ drifts from 1.40 towards 1.29, and a compression that reaches 750 K already wants ∫CV(T) dT/T in place of the power law.
Key equations
Read the units, assumptions and limits before substituting.
Internal energy of an ideal gas, any path
ΔU = n CV ΔT
U depends on T alone, so this holds on every path, not only at constant volume where CV was defined: it is the one term the first law always hands you free.
n in mol, CV in J mol⁻¹ K⁻¹, ΔT in K; CV = 3R/2 monatomic, 5R/2 diatomic near room temperatureIsothermal work and heat
W = Q = nRT ln(V₂/V₁)
The logarithm is ∫nRT dV/V with p falling as 1/V. Every joule of work out is a joule of heat drawn from the reservoir, so the ratio V₂/V₁ alone sets the cost.
T in K, R = 8.314 J mol⁻¹ K⁻¹, W done by the gas in J; ΔU = 0 for an ideal gasIsobaric bookkeeping
Q = n Cₚ ΔT = n CV ΔT + p ΔV
The heat splits into the internal-energy rise and the work of pushing the surroundings back, which is why Cₚ exceeds CV by exactly R for an ideal gas.
p in Pa, ΔV in m³, so pΔV = nRΔT in J; Cₚ = CV + R in J mol⁻¹ K⁻¹Isochoric bookkeeping
Q = ΔU = n CV ΔT, with W = 0
With no work term the heat is the whole internal-energy change, so measuring Q at fixed volume is the experiment that defines CV.
Q in J, positive into the gas; a clamped volume makes ∫p dV vanish whatever p doesReversible adiabat of an ideal gas
T V(γ−1) = constantp Vγ = constant
Integrating dU = −p dV with Q = 0 gives this curve, steeper than an isotherm by γ; it needs an ideal gas, a reversible path and a constant γ.
γ = Cₚ/CV, dimensionless: 5/3 monatomic, 7/5 diatomic; the two forms are linked by pV = nRTAdiabatic work
W = (p₁V₁ − p₂V₂)/(γ − 1) = n CV (T₁ − T₂)
With Q = 0 the work is paid entirely from internal energy, so the temperature swing and the work are the same number in two currencies.
W done by the gas in J; positive in an expansion, where the gas cools, negative in a compressionInteractive lab
Predict first. Explore the model. Compare the result.
Explore the model
Try this. Drag V₂ below 1.0 L and watch the adiabat climb above the isotherm, so the same compression costs more work when no heat can leave; then raise γ from 1.40 to 1.67 and the adiabat steepens and T₂ swings further, while near γ = 1.10 it sinks onto the isotherm.
Live results
- T₂ ON THE ADIABAT
- 227 K
- p₂ ON THE ADIABAT
- 0.38 ×10⁵ Pa
- W ALONG THE ADIABAT
- 60.5 J
- W ALONG THE ISOTHERM
- 69.3 J
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. Heat-capacity ratio γ: 1.40; Final volume V₂: 2.00 L
This experiment is kept only while this page is open. It does not change saved course progress.
Catch the common trap
No heat flow does not mean no temperature change. First-year students carry the everyday equation of heat with temperature into Q = 0 and conclude ΔT = 0, the opposite of the truth. In an adiabatic compression the work done on the gas has nowhere to go but internal energy, so the temperature rises by more than in any compression to the same volume that lets heat leak out: air compressed tenfold reaches 754 K without a single joule of heat entering. The same confusion runs the other way for the isotherm: the temperature stays constant precisely because heat flows in as fast as the gas spends energy on work. Heat and temperature change are different quantities, linked only through the path, and ΔU = nCVΔT is the bookkeeping that keeps them apart.
Practice & worked examples
3 authored examples. Make an attempt, then reveal the reasoning one step at a time.
EasyExample 1
0.250 mol of helium at 350 K expands reversibly and isothermally from 2.00 L to 5.00 L. Find the work done by the gas, the heat transferred and the change in internal energy, and state which way the heat flows.
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.
- Isothermal and ideal: U depends on T alone, so ΔU = nCVΔT = 0 before any integral is written.
- Along the path p = nRT/V, so W = ∫p dV = nRT ln(V₂/V₁). Here nRT = 0.250 × 8.314 × 350 = 727 J.
- ln(5.00/2.00) = ln 2.50 = 0.916, so W = 727 J × 0.916 = 667 J, positive because the gas expands and does work on the piston.
- First law: Q = ΔU + W = 0 + 667 J = +667 J. Positive Q is heat into the gas: the reservoir replaces every joule the gas spends as work, which is what holds T at 350 K.
- Check the pressures: p₁ = nRT/V₁ = 727 J/(2.00 × 10⁻³ m³) = 3.64 × 10⁵ Pa falls to p₂ = 1.45 × 10⁵ Pa, the 1/V drop the logarithm came from.
Answer. W = +667 J by the gas, Q = +667 J into the gas from the reservoir, ΔU = 0.
MediumExample 2
0.0400 mol of air (γ = 1.40, CV = 5R/2) at 295 K fills 1.00 L of a cylinder. It is compressed reversibly and adiabatically to 0.125 L. Find the final temperature and pressure and the work done on the gas, then check the work a second way.
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.
- Adiabatic and reversible: TV(γ−1) = constant, so T₂ = T₁(V₁/V₂)(γ−1) = 295 K × 80.40. 80.40 = 2.297, so T₂ = 678 K, a rise of 383 K with no heat entering.
- Initial pressure from the state equation: p₁ = nRT₁/V₁ = (0.0400 × 8.314 × 295)/(1.00 × 10⁻³) = 9.81 × 10⁴ Pa.
- Along the adiabat pVγ is fixed: p₂ = p₁ × 81.40 = 9.81 × 10⁴ × 18.38 = 1.80 × 10⁶ Pa. Cross-check with nRT₂/V₂ = (0.0400 × 8.314 × 678)/(1.25 × 10⁻⁴) = 1.80 × 10⁶ Pa.
- Energy route: Q = 0, so Wₒₙ = ΔU = nCVΔT = 0.0400 × 20.79 × 383 = 318 J.
- Integral route: Wₒₙ = (p₂V₂ − p₁V₁)/(γ − 1) = (225.4 J − 98.1 J)/0.40 = 318 J. The two agree, as they must, since p₁V₁ − p₂V₂ = nR(T₁ − T₂).
- Compare the isothermal alternative: nRT₁ ln 8 = 98.1 J × 2.079 = 204 J. The adiabatic compression costs 56% more work because it pushes against a pressure that climbs to 1.80 MPa rather than 0.785 MPa.
Answer. T₂ = 678 K, p₂ = 1.80 × 10⁶ Pa, Wₒₙ = 318 J by both routes (against 204 J for the isothermal compression).
HardExample 3
1.50 mol of helium (γ = 5/3) at 400 K and 2.00 L expands reversibly and adiabatically to 4.00 L, then is compressed at constant pressure back to 2.00 L. Draw up the ledger of W, Q and ΔU for each stage and for the whole path, and confirm that ΔU closes as a state function.
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.
- Stage 1, adiabatic: T₂ = T₁(V₁/V₂)(γ−1) = 400 K × 0.5²⁄³ = 400 × 0.630 = 252 K. Pressures: p₁ = nRT₁/V₁ = (1.50 × 8.314 × 400)/(2.00 × 10⁻³) = 2.49 × 10⁶ Pa and p₂ = p₁ × 0.5⁵⁄³ = 7.86 × 10⁵ Pa.
- Stage 1 ledger: Q₁ = 0; W₁ = nCV(T₁ − T₂) = 1.50 × 12.47 × 148 = 2.77 kJ by the gas; ΔU₁ = −2.77 kJ. Cross-check: (p₁V₁ − p₂V₂)/(γ − 1) = (4988 J − 3142 J)/(2/3) = 2.77 kJ.
- Stage 2, isobaric at p₂ = 7.86 × 10⁵ Pa from 4.00 L to 2.00 L: T₃ = T₂ × (2.00/4.00) = 126 K. W₂ = p₂ΔV = 7.86 × 10⁵ × (−2.00 × 10⁻³) = −1.57 kJ, work done on the gas.
- Stage 2 ledger: ΔU₂ = nCV(T₃ − T₂) = 1.50 × 12.47 × (−126) = −2.36 kJ; Q₂ = ΔU₂ + W₂ = −2.36 − 1.57 = −3.93 kJ, heat leaving. Cross-check: nCₚΔT = 1.50 × 20.79 × (−126) = −3.93 kJ.
- Whole path: W = 2.77 − 1.57 = +1.20 kJ by the gas, Q = 0 − 3.93 = −3.93 kJ, ΔU = −2.77 − 2.36 = −5.13 kJ. State-function check: nCV(T₃ − T₁) = 1.50 × 12.47 × (−274) = −5.13 kJ, and Q − W = −3.93 − 1.20 = −5.13 kJ. The ledger closes.
- Read the result: the gas did net work while losing heat, paid for entirely by a 274 K fall in temperature. Helium is still a good ideal gas at 126 K; argon at this pressure would be within 15 K of condensing, and the ideal-gas assumption behind every line would be failing.
Answer. Stage 1: W = +2.77 kJ, Q = 0, ΔU = −2.77 kJ. Stage 2: W = −1.57 kJ, Q = −3.93 kJ, ΔU = −2.36 kJ. Whole path: W = +1.20 kJ, Q = −3.93 kJ, ΔU = −5.13 kJ = nCV(T₃ − T₁), with T₃ = 126 K.
Quick check
Select an answer and explain it before checking.
Review & continue
A named gas process holds a single quantity fixed along the whole path — temperature, pressure, volume, or the heat transferred, which is zero — so that the first law fixes the remaining energy terms from the path alone.
- 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.
Optional supporting lessons
These chapter resources can help with earlier ideas; they are not additional required Physics III completion tasks.