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Optional extension · Interactive lesson

Isothermal, isobaric, isochoric and adiabatic processes

Four constraints, four different answers to the same question: when a gas takes in energy, how much of it stays inside and how much leaves through the piston? Read the constraint off the apparatus, then let the first law and the right molar heat capacity finish the arithmetic.

UPII-E3.03 · Lesson 3 of 9 in this extension. Position is not a completion score.
Starting model: Isothermal, isobaric, isochoric and adiabatic processesFour processes leave one state at p₁, V₁, 300 K: the dashed hyperbola is the isotherm, the solid curve below it the adiabat, the horizontal segment the isobar, the vertical stub the isochore, which sweeps no area. At V₂ = 3.0 V₁ with γ = 1.40 the adiabat has fallen to 0.215 p₁ and 193 K; the isotherm ends at 0.333 p₁, still at 300 K.p / p₁isobar p = p₁isotherm ΔU = 0adiabat Q = 0isochore W = 0V / V₁adiabat ends at 193 K
Start with a picture. Change the model in the lab below.

Optional extension. Use this unnumbered support sequence where your university’s syllabus or prerequisite needs require it. It is not an additional numbered unit. Optional work is not a required completion gate.

1

Build the model

Name the constraint and the energy split follows.

The key idea

A named gas process is a quasi-static path on which one thing is held fixed — the volume, the pressure, the temperature, or the heat flow at zero — and that single constraint fixes both the shape of the p-V curve and the split of energy between heat and work.

Example. Take 1.00 mol of nitrogen from 300 K to 400 K at constant volume and it absorbs 2.08 kJ, all of it internal energy. Do it at constant pressure and it needs 2.91 kJ, because 831 J leaves again as the work of pushing the surroundings back.

The complete physical model and assumptions

A gas in equilibrium has only two free variables, because pV = nRT ties the third to them, so every quasi-static process is a curve in the p-V plane and the first law ΔU = Q − W is one equation in three unknowns. Naming a constraint supplies what is missing. Fix the volume and W = ∫p dV vanishes; fix the pressure and the integral collapses to pΔV = nRΔT; fix the temperature and p = nRT/V turns it into a logarithm; block the heat and the gas must pay for its work out of its own internal energy, which is what bends the adiabat below the isotherm and gives p Vγ = constant. Underneath all four sits one ideal-gas fact: U depends on temperature alone, so ΔU = n CV ΔT on every path, not merely the constant-volume one where that coefficient is measured. The model stops where its assumptions do. It wants a gas close to ideal, it wants CV and Cₚ roughly constant over the range — γ for nitrogen drifts from 1.40 towards 1.29 as vibrational modes wake up near 1000 K — and it wants the change slow enough that one pressure and one temperature describe the whole sample. A gas bursting into a vacuum has Q = 0 and still breaks p Vγ = constant, because it is never in equilibrium on the way.

1One constraint picks out one curve in the p-V plane

For n moles of an ideal gas pV = nRT leaves only two of the three variables free, so a state is a point in the p-V plane and a quasi-static process is a curve through it. That curve is what the work integral W = ∫p dV needs before it can be evaluated at all, because the integral wants p as a known function of V. Each name supplies one. Isochoric: V fixed, a vertical line, and dV = 0 kills the integral. Isobaric: p fixed, a horizontal line, and p comes outside the integral. Isothermal: T fixed, so p = nRT/V, a hyperbola. Adiabatic: Q = 0, and the curve p = p₁(V₁/V)γ falls away faster than the hyperbola because the gas cools as it expands. Draw all four through one starting point and the whole behaviour of the topic is visible before a single number is substituted.

2CV measures internal energy, not constant-volume heat

Hold the volume fixed and the gas can do no work, so the first law reduces to Q = ΔU and the measured heat gives the molar heat capacity directly: CV = (1/n)(ΔU/ΔT). What happens next decides half the problems in this topic. For an ideal gas the internal energy is a function of temperature alone — kinetic theory gives U = (f/2)nRT for f active degrees of freedom — so once CV has been identified as the temperature coefficient of U, that identification travels with U. Take 2.00 mol of argon from 300 K to 450 K and ΔU = n CV ΔT = 2.00 × 12.47 × 150 = 3.74 kJ, whether the gas was heated in a rigid bottle, allowed to expand at constant pressure, or compressed by a piston with the heat blocked. Only the split between Q and W changes with the path. ΔU does not, because U is a state function and temperature is the only state variable it answers to.

3Isobaric heating pays twice, and the surcharge is R

Let the gas expand against a fixed external pressure and both terms of the first law are alive. The work is W = pΔV, and pV = nRT turns that into W = nRΔT — a result that never mentions p, because a higher pressure forces a proportionally smaller volume change. The heat needed is therefore Q = ΔU + W = n CV ΔT + nRΔT = n(CV + R)ΔT, which is where Cₚ = CV + R comes from. Numbers make the split concrete. Heat 1.00 mol of nitrogen from 300 K to 400 K at 1.013 × 10⁵ Pa: the gas expands by nRΔT/p = 8.21 × 10⁻³ m³, does 831 J of work, gains 2079 J of internal energy, and so needs 2910 J of heat. The fraction that leaves through the piston is R/Cₚ = 8.314/29.10 = 0.286, so 28.6% of every joule supplied to a diatomic gas at constant pressure never stays in the gas.

4The isotherm: all heat, no change in internal energy

Clamp the temperature — a thin-walled cylinder in a large stirred bath, moved slowly — and ΔU = n CV ΔT = 0 for the whole process. The first law then reads Q = W exactly: every joule the gas delivers to the piston is a joule the reservoir has just delivered to the gas, and the gas is only the conduit. The work follows from p = nRT/V with T held constant, so W = ∫nRT dV/V from V₁ to V₂, which is W = nRT ln(V₂/V₁). Expand 1.00 mol at 300 K from 10.0 L to 25.0 L and W = 8.314 × 300 × ln 2.50 = 2.29 kJ out, matched by 2.29 kJ of heat in. Compress instead and the logarithm turns negative: work goes in, and the same energy must be dumped to the bath or the temperature will not hold. Note what the formula needs — only the volume ratio, so litres and cubic metres give the same answer provided both volumes use one unit.

5The adiabat: all work, no heat, and steeper by γ

Insulate the cylinder, or move the piston faster than heat can leak through it, and Q = 0. The first law becomes dU = −dW, that is n CV dT = −p dV: the work is now financed entirely out of internal energy, so an expanding gas must cool. Substituting p = nRT/V separates the variables into CV dT/T = −R dV/V, and integrating with R = Cₚ − CV gives T V(γ−1) = constant, which pV = nRT converts into p Vγ = constant. Differentiate that last form and dp/dV = −γp/V, against the isotherm's −p/V: at any shared point the adiabat is steeper by the factor γ. The work is easiest from the first law itself, W = −ΔU = n CV (T₁ − T₂). Compress 1.00 mol of air, γ = 1.40, from 20.0 L to 5.00 L starting at 300 K: T₂ = 300 × 4.000.40 = 522 K, so W = 20.79 × (300 − 522) = −4.62 kJ. That is 4.62 kJ done on the gas, all of it still inside as a 222 K rise — which is why a bicycle pump gets hot.

6Which constraint has the apparatus really imposed?

Choosing the name is a physical judgement about two times: how long the process takes, against how long heat needs to cross the walls. A gas compressed over a minute in a thin copper cylinder standing in a water bath holds the bath's temperature and is isothermal. The same compression done in 30 ms in an insulated cylinder is adiabatic to within a per cent. Between those extremes no named process applies and the work has to be read off a measured p-V curve instead. The second requirement is easier to forget: all four relations assume quasi-static change, so that one pressure and one temperature describe the whole sample at every instant. Let a gas burst through a valve into an evacuated chamber and it is thermally isolated, Q = 0, but it pushes nothing, so W = 0 and ΔU = 0. The temperature is unchanged, the gas has not cooled at all, and p Vγ = constant is simply false along that path.

2

Key equations

Read the units, assumptions and limits before substituting.

Internal energy of an ideal gas

ΔU = n CV ΔT

True on every ideal-gas path, because U depends on temperature alone — not only on the constant-volume path where CV is measured.

n in mol, CV in J mol⁻¹ K⁻¹, ΔT in K, ΔU in J

Constant volume: isochoric heating

Q = n CV ΔT

A vertical line on a p-V diagram has no area beneath it, so every joule of heat shows up as temperature.

V fixed in m³, so W = ∫p dV = 0 and Q in J equals ΔU exactly

Constant pressure: isobaric work

W = p ΔV = n R ΔT

The work depends only on the temperature rise, not on the pressure the expansion happens at.

p in Pa, ΔV in m³, R = 8.314 J mol⁻¹ K⁻¹, W in J and positive when the gas expands

Mayer's relation

Cₚ = CV + R

The gap is exactly the expansion work per mole per kelvin, and it fixes the ratio γ = Cₚ/CV.

both molar heat capacities in J mol⁻¹ K⁻¹, R the molar gas constant

Constant temperature: isothermal work

W = n R T ln(V₂/V₁)

ΔU = 0 on an isotherm, so this is also the heat the reservoir has to supply.

T in K, V₁ and V₂ in any one shared unit since only their ratio enters, W in J

Adiabatic curve

p Vγ = constant

Q = 0 along the curve, which makes it steeper than the isotherm by the factor γ at every point.

γ = Cₚ/CV, dimensionless: 5/3 for a monatomic gas, 7/5 for a diatomic one near 300 K
3

Interactive lab

Predict first. Explore the model. Compare the result.

Explore the model

3.0 × V₁
1.5 to 5 × V₁; steps of 0.1.
1.40
1.2 to 1.67; steps of 0.01.

Try this. Push γ to 1.67 and drag V₂ out to 5 V₁: the adiabat ends at 0.068 p₁ where the isotherm ends at 0.200 p₁, because that work came out of internal energy and cooled the gas to 102 K. Slide γ back to 1.20 and the two curves close up.

Live results

ADIABAT p₂/p₁
0.215
ADIABAT T₂ FROM 300 K
193 K
ISOTHERMAL W PER MOLE
2740 J mol⁻¹
ADIABATIC W PER MOLE
2217 J mol⁻¹

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

Interactive Physics II modelFour processes leave one state at p₁, V₁, 300 K: the dashed hyperbola is the isotherm, the solid curve below it the adiabat, the horizontal segment the isobar, the vertical stub the isochore, which sweeps no area. At V₂ = 3.0 V₁ with γ = 1.40 the adiabat has fallen to 0.215 p₁ and 193 K; the isotherm ends at 0.333 p₁, still at 300 K.p / p₁isobar p = p₁isotherm ΔU = 0adiabat Q = 0isochore W = 0V / V₁adiabat ends at 193 K
Four processes leave one state at p₁, V₁, 300 K: the dashed hyperbola is the isotherm, the solid curve below it the adiabat, the horizontal segment the isobar, the vertical stub the isochore, which sweeps no area. At V₂ = 3.0 V₁ with γ = 1.40 the adiabat has fallen to 0.215 p₁ and 193 K; the isotherm ends at 0.333 p₁, still at 300 K.

Predict → change one variable → check

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

Saved baseline. Final volume V₂ / V₁: 3.0 × V₁; Adiabatic index γ = Cₚ/CV: 1.40

Baseline 3.0; choose 1.5 to 5, in steps of 0.1.
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

The commonest failure here is reading CV as the heat capacity you are allowed to use when the volume is fixed, and Cₚ as its replacement when the pressure is fixed. Cₚ is indeed the right coefficient for the heat at constant pressure — but ΔU = n CV ΔT on every path, including that one. Heat 1.00 mol of nitrogen from 300 K to 400 K at constant pressure and ΔU is 2079 J, not the 2910 J that n Cₚ ΔT returns; the extra 831 J never entered the internal energy at all, it left again as expansion work. Writing ΔU = n Cₚ ΔT counts that work twice, and the error survives into every cycle built from such a leg. The internal energy of an ideal gas answers to temperature alone, so it cannot know which path brought it there.

5

Practice & worked examples

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

EasyExample 1

A sealed rigid steel flask of volume 8.00 L holds 0.400 mol of helium at 295 K. An internal heater delivers 250 J. Find the temperature rise, the final pressure, and the work done by the gas. Take CV = 3R/2 for a monatomic 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 vertical cylinder is closed by a frictionless piston of area 1.20 × 10⁻² m², loaded so that the gas pressure stays at 1.40 × 10⁵ Pa. It holds 0.600 mol of nitrogen at 290 K. Heat is supplied until the temperature reaches 430 K. Find the work done by the gas, the change in internal energy, the heat supplied, and how far the piston rises. Take CV = 5R/2.

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

A diesel-type compression squeezes 2.00 × 10⁻³ m³ of air at 1.00 × 10⁵ Pa and 310 K down to 1.25 × 10⁻⁴ m³, quasi-statically and with no heat exchange. Treat air as ideal with γ = 1.40 and CV = 5R/2. Find the final pressure and temperature, the work done on the gas, and how much work an isothermal compression between the same two volumes would have taken instead.

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.

Two identical 1.00 mol samples of nitrogen start at 300 K in 10.0 L. One expands isothermally to 20.0 L, the other adiabatically to 20.0 L, with γ = 1.40. Which statement about the two expansions is correct?
7

Review & continue

A named gas process is a quasi-static path on which one thing is held fixed — the volume, the pressure, the temperature, or the heat flow at zero — and that single constraint fixes both the shape of the p-V curve and the split of energy between heat and work.

  • 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 II completion tasks.

Extra challenging questions

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