One Number for a Solid, Two for a Gas

Ask how much heat it takes to warm a kilogram of copper by one kelvin and there is a single answer: 385 J. Ask the same question about a kilogram of oxygen and the honest reply is a question back — how are you holding it while you heat it?

That is not pedantry. Depending on the answer, the heat you need can differ by 40%. Getting this right is the whole of this section, and it turns out to hand us one of the prettiest results in the chapter.

First, the three capacities, in order

You met the first two in the previous chapter. Here they are again, stacked from crudest to most useful.

Key Point — the three heat capacities:

  • Heat capacity of a body: S=ΔQΔTS = \frac{\Delta Q}{\Delta T} measured in J/K. It belongs to that particular lump of stuff — a bathtub of water has a bigger SS than a cup of it.
  • Specific heat capacity, per kilogram: s=Sm=1mΔQΔTs = \frac{S}{m} = \frac{1}{m}\frac{\Delta Q}{\Delta T} in J/(kg K). Now it is a property of the material, not of the lump.
  • Molar specific heat capacity, per mole: C=Sn=1nΔQΔTC = \frac{S}{n} = \frac{1}{n}\frac{\Delta Q}{\Delta T} in J/(mol K), where nn is the number of moles, also written μ\mu.

For gases, always use the molar version. A mole is a fixed number of molecules, so comparing gases per mole compares like with like: one mole of helium and one mole of oxygen contain the same 6.022×10236.022 \times 10^{23} particles, whereas one kilogram of each contains wildly different numbers. Every clean result below is a per-mole result.

Converting between the two is just the molar mass MM in kg/mol: C=Msands=CMC = M s \qquad\text{and}\qquad s = \frac{C}{M}

[Board Important] Write CpC_p and CvC_v with capital letters for the molar specific heats in J/(mol K), and cpc_p, cvc_v in lower case for the per-kilogram ones in J/(kg K). Mixing them up is the single commonest reason a numerically correct answer scores zero.

Now the problem

Heat one mole of a gas and raise its temperature by 1 K. How much heat did that take?

Gas heated with piston bolted, then free: the free one needs extra heat

Look at the two cylinders. Same gas, same number of moles, same 1 K rise. On the left the piston is bolted so the gas cannot expand. On the right the piston floats under a fixed load, so as the gas warms it pushes the piston up and lifts that load.

The gas on the right has done a job on the way. It has pushed the atmosphere and the load back, and that work had to be paid for out of the heat you supplied. So it needed more heat for the same temperature rise.

Before going further, fix the bookkeeping.

This chapter's sign convention: ΔQ\Delta Q is positive when heat is added TO the system. ΔW\Delta W is positive when work is done BY the system. The first law is then ΔQ=ΔU+ΔW\Delta Q = \Delta U + \Delta W

Chemistry writes the first law as ΔU=Q+W\Delta U = Q + W, with WW the work done on the system — the same physics with one sign moved.

So a gas needs two specific heats

A solid needs only one because a solid barely expands. Heat a copper block by 100 K and its volume changes by about 0.5% — the work it does pushing the air aside is a fraction of a percent of the heat supplied, far below the accuracy anyone quotes. So for a solid CpC_p and CvC_v are the same number for all practical purposes, and nobody bothers with the subscript.

A gas is different by a factor of thousands. Heat one mole of gas at constant atmospheric pressure from 300 K to 400 K and its volume runs from about 24.6 litres up to about 32.8 litres — an expansion of roughly 8200 cm3^3, which is 8.2 litres. That is enough to push the atmosphere back through a real distance and do real work: ΔW=PΔV=nRΔT=1×8.314×100=831 J\Delta W = P\,\Delta V = nR\,\Delta T = 1 \times 8.314 \times 100 = 831 \text{ J}

Keep those two numbers apart, because they are the pair most often collapsed into one: 82008200 cm3^3 is how much the gas expands, and 831831 J is the work that expansion does. Different quantities, different units. nRΔTnR\Delta T hands you the joules; you get the cubic centimetres only after dividing by the pressure, ΔV=nRΔTP\Delta V = \dfrac{nR\Delta T}{P}.

Key Point — the two molar specific heats of a gas:

  • CvC_v, at constant volume: heat supplied with the volume held fixed, so ΔW=0\Delta W = 0 and every joule goes into internal energy.
  • CpC_p, at constant pressure: heat supplied with the pressure held fixed, so the gas expands and also does work on its surroundings.

Because the constant-pressure gas has to pay for that work as well, Cp>Cvalways, for every gas.C_p > C_v \quad\text{always, for every gas.}

[JEE Tip] There is a sharper version of this. For a gas, the molar specific heat is not a property of the gas at all — it is a property of the gas together with the process. Squeeze the gas as you heat it and you can make CC come out negative. Hold the temperature fixed and pour heat in, and ΔT=0\Delta T = 0 while ΔQ0\Delta Q \neq 0, so CC is infinite. Let no heat in at all and C=0C = 0. Constant volume and constant pressure are simply the two processes worth naming, because they are the two that turn up everywhere.

CvC_v: Where the Whole Joule Goes into Internal Energy

Start with the easy cylinder — the one with the piston bolted down.

The definition, and the first law

Hold the volume fixed and supply heat ΔQ\Delta Q to nn moles, raising the temperature by ΔT\Delta T. Since the volume cannot change, ΔV=0\Delta V = 0, and the work done by the gas is ΔW=PΔV=0\Delta W = P\,\Delta V = 0

The first law ΔQ=ΔU+ΔW\Delta Q = \Delta U + \Delta W then collapses to ΔQ=ΔU\Delta Q = \Delta U

Every joule of heat has become internal energy. Nothing was spent pushing anything. So

Key Point — molar specific heat at constant volume: Cv=1n(ΔQΔT)V=1nΔUΔTC_v = \frac{1}{n}\left(\frac{\Delta Q}{\Delta T}\right)_V = \frac{1}{n}\frac{\Delta U}{\Delta T} and in the limit of a small change, Cv=1ndUdTC_v = \frac{1}{n}\frac{dU}{dT} The subscript VV says "at constant volume". Rearranged, the form you will actually use is   ΔU=nCvΔT  \boxed{\;\Delta U = n\,C_v\,\Delta T\;}

The line that decides more exam questions than any other

Read that boxed equation again and notice what is not in it. There is no pressure, no volume, no mention of how the gas got from the first temperature to the second.

That is not an accident, and it is not sloppiness.

For an ideal gas, the internal energy depends only on the temperature — not on the volume, not on the pressure. Section 2 set this out: UU is a state function, and for an ideal gas that state is pinned by TT alone, because the molecules have no potential energy of interaction to speak of. Squash an ideal gas at fixed temperature and you have not changed its internal energy at all.

So if UU depends only on TT, then a given change in TT always produces the same change in UU, whatever route the gas took.

Key Point — the most reusable equation in the chapter: ΔU=nCvΔTfor ANY process of an ideal gas\Delta U = n\,C_v\,\Delta T \quad\text{for ANY process of an ideal gas} isothermal, adiabatic, isobaric, a wiggly path drawn freehand — all of them. CvC_v appears in the formula, but the process does not have to be at constant volume. CvC_v got its name from where it is most easily measured, not from where it is allowed to be used.

[JEE Tip] This is worth reading three times. Students happily write ΔU=nCvΔT\Delta U = nC_v\Delta T for an isochoric leg and then refuse to write it for an isobaric one, on the grounds that "the volume is changing". The volume changing is irrelevant. The moment you know ΔT\Delta T for an ideal gas, you know ΔU\Delta U, and CvC_v is the constant that converts one to the other.

There is a good way to remember why. Take the gas from T1T_1 to T2T_2 by any path you like. ΔU\Delta U is fixed by the endpoints because UU is a state function. Now choose, out of all the possible paths, the constant-volume one. Along that path ΔU=ΔQ=nCvΔT\Delta U = \Delta Q = nC_v\Delta T. But ΔU\Delta U was the same for every path — so nCvΔTnC_v\Delta T is the answer for every path.

What this means in practice

Three consequences you will use immediately:

  • In an isochoric process, ΔQ=ΔU=nCvΔT\Delta Q = \Delta U = nC_v\Delta T. Heat in, temperature up, no work at all. Section 7 develops this.
  • In an isothermal process, ΔT=0\Delta T = 0, so ΔU=0\Delta U = 0 for an ideal gas, no matter how much heat crosses the boundary. The first law then reads ΔQ=ΔW\Delta Q = \Delta W: everything you put in comes straight out as work.
  • In an adiabatic process, ΔQ=0\Delta Q = 0, so ΔW=ΔU=nCvΔT\Delta W = -\Delta U = -nC_v\Delta T. If the gas expands it does positive work, so ΔU\Delta U is negative and the gas cools itself. Section 6 does this properly.

And what CvC_v actually measures

CvC_v is a measure of how much energy a mole of the gas can absorb per kelvin internally — how many separate ways its molecules have of storing energy. A single atom can only fly about. A dumbbell molecule can fly about and tumble. A floppier molecule has more options still.

More ways of storing energy means more energy needed per kelvin, which means a bigger CvC_v. That single sentence explains every number in the next block, and it is why CvC_v is not the same for helium and for carbon dioxide.

CpC_p, and Mayer's Relation Derived from the First Law

Now the free-piston cylinder.

Setting it up

Hold the pressure constant at PP and supply heat ΔQ\Delta Q to nn moles, raising the temperature by ΔT\Delta T. The gas expands by ΔV\Delta V, and in doing so does work ΔW=PΔV\Delta W = P\,\Delta V (Section 2 derived that from force times distance; Section 5 draws it.) The first law gives ΔQ=ΔU+PΔV\Delta Q = \Delta U + P\,\Delta V

Divide by nΔTn\,\Delta T: Cp=1n(ΔQΔT)P=1nΔUΔT+Pn(ΔVΔT)PC_p = \frac{1}{n}\left(\frac{\Delta Q}{\Delta T}\right)_P = \frac{1}{n}\frac{\Delta U}{\Delta T} + \frac{P}{n}\left(\frac{\Delta V}{\Delta T}\right)_P

The first term on the right is exactly CvC_v — and this is where the previous block earns its keep. ΔU=nCvΔT\Delta U = nC_v\Delta T holds for any process of an ideal gas, so it holds here even though the volume is changing. That is the step students skip, and it is the whole derivation. Cp=Cv+Pn(ΔVΔT)PC_p = C_v + \frac{P}{n}\left(\frac{\Delta V}{\Delta T}\right)_P

The second term, from the equation of state

For an ideal gas, PV=nRTPV = nRT. Hold PP fixed and let TT change: PΔV=nRΔTP(ΔVΔT)P=nRP\,\Delta V = nR\,\Delta T \qquad\Longrightarrow\qquad P\left(\frac{\Delta V}{\Delta T}\right)_P = nR

So the second term is nRn=R\dfrac{nR}{n} = R, and we are done.

Key Point — Mayer's relation:   CpCv=R  \boxed{\;C_p - C_v = R\;} where CpC_p and CvC_v are the molar specific heats of an ideal gas and R=8.314R = 8.314 J/(mol K) is the universal gas constant.

The difference is exactly RR — not approximately, not for some gases. It does not depend on the temperature, on the pressure, or on which gas it is. Helium, nitrogen, methane: same difference, 8.3148.314 J/(mol K).

Reading the result

The physics is right there in the derivation. Take one mole and raise its temperature by 1 K.

  • At constant volume you pay CvC_v joules, all of it banked as internal energy.
  • At constant pressure you pay CvC_v joules for exactly the same internal-energy rise, plus RR joules to push the surroundings back.

So RR is not an abstract constant here. RR is the work, in joules, that one mole of an ideal gas does against a constant pressure when its temperature rises by one kelvin. That is a physical meaning for RR worth carrying around.

[Board Important] A three-mark derivation, in the order examiners want it: (1) write the first law ΔQ=ΔU+PΔV\Delta Q = \Delta U + P\Delta V for nn moles at constant pressure; (2) divide by nΔTn\Delta T and identify 1nΔUΔT=Cv\dfrac{1}{n}\dfrac{\Delta U}{\Delta T} = C_v, stating that UU of an ideal gas depends only on TT; (3) differentiate PV=nRTPV = nRT at constant PP to get PΔV=nRΔTP\Delta V = nR\Delta T; (4) conclude CpCv=RC_p - C_v = R. Miss step (2)'s justification and you lose the mark that separates the two grades.

The per-kilogram version

Divide Mayer's relation by the molar mass MM in kg/mol. Since c=CMc = \dfrac{C}{M}, cpcv=RMc_p - c_v = \frac{R}{M}

Now the difference does depend on which gas it is, because MM does. For hydrogen (M=0.002M = 0.002 kg/mol) the gap is 41574157 J/(kg K); for oxygen (M=0.032M = 0.032) it is only 260260 J/(kg K). This is exactly why the molar form is the one to learn — the per-kilogram form hides the universality behind a molar mass.

[NEET Important] A favourite one-liner: given cpc_p and cvc_v per kilogram for a gas, find its molar mass. Answer: M=RcpcvM = \dfrac{R}{c_p - c_v}. For nitrogen, with cp=1040c_p = 1040 and cv=743c_v = 743 J/(kg K), that gives M=8.314297=0.028M = \dfrac{8.314}{297} = 0.028 kg/mol, which is 28 g/mol. Correct.

Why the relation is only for an ideal gas

Two things were assumed. First, that UU depends only on TT — true for an ideal gas, only approximately true for a real one, because real molecules attract each other and pulling them apart costs energy. Second, that PV=nRTPV = nRT — again an idealisation. For real gases at ordinary pressures CpCvC_p - C_v comes out within a percent or so of RR, which is why the relation is used freely; near a liquefaction point it fails outright. For a solid or a liquid, ΔV\Delta V is so tiny that CpCvC_p - C_v is a small fraction of RR, and the two are treated as equal.

The Ratio γ\gamma, and the Numbers You Cannot Do Without

Mayer's relation gives the difference of the two specific heats. Their ratio turns out to matter even more.

Key Point — the ratio of specific heats: γ=CpCv=cpcv\gamma = \frac{C_p}{C_v} = \frac{c_p}{c_v} a pure number with no units, and always greater than 1, because Cp>CvC_p > C_v always. It is sometimes called the adiabatic index.

The ratio is unitless, so the molar and the per-kilogram versions give the same γ\gamma — a rare place where it does not matter which you use.

Combine γ\gamma with Mayer's relation and both specific heats fall out of γ\gamma alone. From Cp=γCvC_p = \gamma C_v and CpCv=RC_p - C_v = R: Cv=Rγ1Cp=γRγ1C_v = \frac{R}{\gamma - 1} \qquad\qquad C_p = \frac{\gamma R}{\gamma - 1}

Learn this pair. Almost every adiabatic problem hands you γ\gamma and expects you to produce CvC_v.

The values of γ\gamma — and why they are here

The values of γ\gamma, and the molecular counting that produces them, sit outside the rationalised syllabus body text, yet Boards, JEE and NEET ask them every single year and no adiabatic problem in this chapter can be solved without them, so they are set out here from first principles.

The counting rule is short. Energy gets shared out equally among every independent way a molecule has of storing it, and each way contributes 12R\frac{1}{2}R to the molar specific heat at constant volume. Call the number of ways ff. Then Cv=f2R,Cp=(f2+1)R,γ=1+2fC_v = \frac{f}{2}R, \qquad C_p = \left(\frac{f}{2} + 1\right)R, \qquad \gamma = 1 + \frac{2}{f}

Cp and Cv in units of R, and the storage modes behind gamma

Now count, for the three families:

  • Monatomic (helium, neon, argon, and metal vapours). A single atom is a point as far as this goes. It can move along three independent directions and that is all — it has no shape to tumble. So f=3f = 3.
  • Diatomic (hydrogen, nitrogen, oxygen, carbon monoxide, and air, which is mostly the first two). A dumbbell can move three ways and tumble about two axes — end over end in two independent planes. Spinning about its own long axis does not count; there is essentially nothing out there to spin. So f=5f = 5.
  • Polyatomic, not in a straight line (ammonia, methane, water vapour). A lopsided molecule can tumble about all three axes, so f=3+3=6f = 3 + 3 = 6.

The table — commit it to memory

Type of gas ff CvC_v CpC_p CvC_v (J/(mol K)) CpC_p (J/(mol K)) γ\gamma
Monatomic — He, Ne, Ar 3 32R\frac{3}{2}R 52R\frac{5}{2}R 12.47 20.79 531.67\frac{5}{3} \approx 1.67
Diatomic — H2_2, N2_2, O2_2, air 5 52R\frac{5}{2}R 72R\frac{7}{2}R 20.79 29.10 75=1.40\frac{7}{5} = 1.40
Polyatomic — NH3_3, CH4_4, H2_2O 6 3R3R 4R4R 24.94 33.26 431.33\frac{4}{3} \approx 1.33

Every value in the last three columns uses R=8.314R = 8.314 J/(mol K).

Read down the γ\gamma column and the pattern is clean: the more ways a molecule has of storing energy, the closer γ\gamma sits to 1. A monatomic gas has the fewest options and so the largest γ\gamma; a floppy polyatomic has the most and so the smallest. And since ff can never be less than 3, γ\gamma can never exceed 53\frac{5}{3} for any gas. That is a genuine upper bound and it makes a good multiple-choice trap: an option offering γ=1.8\gamma = 1.8 is wrong on sight.

[NEET Important] Three numbers, memorised cold: 1.67 monatomic, 1.40 diatomic, 1.33 polyatomic. And the pair that goes with them — for a diatomic gas Cv=20.8C_v = 20.8 and Cp=29.1C_p = 29.1 J/(mol K). Air is diatomic for this purpose, so γair=1.4\gamma_{\text{air}} = 1.4 is the default whenever a question says "a gas" without saying which.

Where the counting comes from

Everything above is the law of equipartition of energy, and it is properly a result of the kinetic theory of gases, which is the very next chapter. There it is derived rather than quoted: you will show that each independent quadratic way of holding energy carries an average 12kBT\frac{1}{2}k_BT per molecule, hence 12RT\frac{1}{2}RT per mole, hence 12R\frac{1}{2}R per kelvin in CvC_v.

For thermodynamics, all we need is the output — the three values of γ\gamma and the two of CvC_v — and the assurance that they are not arbitrary. Treat this block as the bridge: the numbers are used here, and earned there.

Real Gases, the Staircase, and the Traps

The table in the last block is a prediction. Here is what measurement actually says.

Measured values

Gas Type CvC_v (J/(mol K)) CpC_p (J/(mol K)) CpCvC_p - C_v γ\gamma
Helium (He) monatomic 12.47 20.79 8.3 1.67
Argon (Ar) monatomic 12.47 20.79 8.3 1.67
Hydrogen (H2_2) diatomic 20.4 28.8 8.4 1.41
Nitrogen (N2_2) diatomic 20.8 29.1 8.3 1.40
Oxygen (O2_2) diatomic 21.0 29.4 8.4 1.40
Air mostly diatomic 20.8 29.1 8.3 1.40
Carbon dioxide (CO2_2) polyatomic 28.5 36.9 8.4 1.29
Ammonia (NH3_3) polyatomic 27.8 36.1 8.3 1.30

Values near room temperature and ordinary pressure. Helium and argon carry identical entries because at this precision they genuinely measure the same: a lone atom is a lone atom, and a helium atom and an argon atom store energy in exactly the same three ways however different their masses. Every γ\gamma in the last column is just that row's own CpC_p divided by its own CvC_v — check one or two and you will see the table is self-consistent, which is the first thing to test on any table of measured specific heats.

Two things jump out. The CpCvC_p - C_v column is 8.38.3 or 8.48.4 all the way down — Mayer's relation holding to better than 1% across gases whose molecules could hardly be more different. And the predicted values of CvC_v (12.47, 20.79, 24.94) land on top of the measured ones for the monatomic gases and very close for the diatomic ones.

The polyatomic row is the soft one: carbon dioxide measures 28.528.5 where the simple count predicts 24.9424.94. The extra comes from the molecule's vibration — the bonds stretch and bend, and that is one more place to put energy. Which brings us to the interesting part.

Why CvC_v climbs in steps

If the counting were the whole story, CvC_v would be a fixed number for each gas at every temperature. Measure it carefully over a wide range and it is nothing of the sort.

Molar specific heat of hydrogen rising in steps as rotation then vibration switch on

Take hydrogen. Below about 50 K its CvC_v sits near 32R\frac{3}{2}R — the value for a monatomic gas. Warm it through room temperature and CvC_v settles at 52R\frac{5}{2}R: the tumbling has switched on. Push it above about 2000 K and CvC_v starts climbing again towards 72R\frac{7}{2}R as the bond begins to vibrate.

The molecule has not changed shape. What changes is whether it has enough energy to use a mode at all. Classical physics has no answer to this — a classical dumbbell tumbles at any temperature, however cold. Quantum mechanics does: rotational and vibrational energies come in discrete steps, and until a typical collision carries more energy than the first step, the mode simply cannot be excited and stays frozen out.

This staircase was one of the earliest hard clues that classical mechanics was incomplete, decades before anyone had a quantum theory to explain it. You will meet it again in kinetic theory.

[JEE Tip] For every problem in this chapter, use the plain table values — γ=1.67\gamma = 1.67, 1.41.4, 1.331.33. The staircase is worth understanding, not worth applying. If a question wants vibration included it will say so, usually by handing you f=7f = 7 or a value of CvC_v to use.

And why a solid gets away with one number

Run the same count for a solid. Each atom is pinned to a lattice site and oscillates about it in three directions, and an oscillator stores energy in two forms, kinetic and potential — so it carries 2×12R=R2 \times \frac{1}{2}R = R per direction, giving C3R=24.9 J/(mol K)C \approx 3R = 24.9 \text{ J/(mol K)}

For copper, M=0.0635M = 0.0635 kg/mol, so this predicts a specific heat of 24.90.0635=393\dfrac{24.9}{0.0635} = 393 J/(kg K) against a measured 385 — about 2% out. The rule works for most solids at ordinary temperatures (carbon is a famous exception) and it fails at low temperatures, for exactly the quantum reason above.

And because a solid hardly expands, it does almost no work when heated, so its CpC_p and CvC_v differ by far less than RR. One number does the job.

The five traps

  • Molar or per kilogram. CpCv=RC_p - C_v = R is the molar statement. Per kilogram it is cpcv=RMc_p - c_v = \dfrac{R}{M}. Check the units of the numbers you were given before you subtract.
  • ΔU=nCvΔT\Delta U = nC_v\Delta T is not restricted to constant volume. It works for every process of an ideal gas. Refusing to use it on an isobaric leg is the classic self-inflicted wound.
  • ΔQ=nCpΔT\Delta Q = nC_p\Delta T is restricted — to a constant-pressure process, and nothing else. It is a heat formula, and heat is a path function.
  • Kelvin. ΔT\Delta T is the same number in kelvin and in Celsius, so a difference is safe. But the moment a gas-law step appears — PV=nRTPV = nRT, or any ratio of temperatures — the temperature must be absolute.
  • γ>53\gamma > \frac{5}{3} is impossible. So is Cv<32RC_v < \frac{3}{2}R. Use both as sanity checks on an answer before you write it down.

Solved Examples

Constants used throughout, unless a problem says otherwise: R=8.314R = 8.314 J/(mol K); 1 atm =1.013×105= 1.013 \times 10^5 Pa; 0°C=273.150°C = 273.15 K. Monatomic γ=53\gamma = \frac{5}{3} with Cv=12.47C_v = 12.47 and Cp=20.79C_p = 20.79 J/(mol K); diatomic γ=1.4\gamma = 1.4 with Cv=20.79C_v = 20.79 and Cp=29.10C_p = 29.10; polyatomic γ=43\gamma = \frac{4}{3} with Cv=24.94C_v = 24.94 and Cp=33.26C_p = 33.26.

Example 1: The same gas, the same heating, two different bills

Two moles of a diatomic ideal gas are taken from 300 K to 400 K, (a) at constant volume and (b) at constant pressure. For each, find ΔQ\Delta Q, ΔU\Delta U and ΔW\Delta W, state the sign of each and say what it means physically.

Solution:

  1. Fix the constants. Diatomic, so Cv=52R=20.79C_v = \frac{5}{2}R = 20.79 and Cp=72R=29.10C_p = \frac{7}{2}R = 29.10 J/(mol K). Both temperatures are already absolute and positive; ΔT=+100\Delta T = +100 K.

  2. (a) Constant volume. The volume cannot change, so ΔW=PΔV=0\Delta W = P\,\Delta V = 0 ΔU=nCvΔT=2×20.79×100=4157 J\Delta U = nC_v\Delta T = 2 \times 20.79 \times 100 = 4157 \text{ J} ΔQ=ΔU+ΔW=4157+0=4157 J\Delta Q = \Delta U + \Delta W = 4157 + 0 = 4157 \text{ J} Signs: ΔQ\Delta Q is positive, so heat was added to the gas. ΔU\Delta U is positive, so its internal energy rose. ΔW\Delta W is zero — the gas neither pushed nor was pushed.

  3. (b) Constant pressure. Now ΔU\Delta U is the same, because the temperature change is the same and UU depends only on TT: ΔU=nCvΔT=4157 J\Delta U = nC_v\Delta T = 4157 \text{ J} The work follows from PΔV=nRΔTP\Delta V = nR\Delta T: ΔW=nRΔT=2×8.314×100=1662.8 J\Delta W = nR\,\Delta T = 2 \times 8.314 \times 100 = 1662.8 \text{ J} ΔQ=ΔU+ΔW=4157+1662.8=5819.8 J\Delta Q = \Delta U + \Delta W = 4157 + 1662.8 = 5819.8 \text{ J} Cross-check with ΔQ=nCpΔT=2×29.10×100=5820\Delta Q = nC_p\Delta T = 2 \times 29.10 \times 100 = 5820 J. Agreed. Signs: ΔQ\Delta Q positive — heat added. ΔU\Delta U positive — same rise as before. ΔW\Delta W positive — the gas expanded and did work on its surroundings.

  4. Compare. The second case needed 5819.84157=1662.85819.8 - 4157 = 1662.8 J more, and that is exactly nRΔTnR\Delta T: the work of pushing the surroundings back. The ratio of the two heats is 5819.84157=1.40=γ\dfrac{5819.8}{4157} = 1.40 = \gamma.

Final Answer: (a) ΔQ=+4157\Delta Q = +4157 J, ΔU=+4157\Delta U = +4157 J, ΔW=0\Delta W = 0. (b) ΔQ=+5819.8\Delta Q = +5819.8 J, ΔU=+4157\Delta U = +4157 J, ΔW=+1662.8\Delta W = +1662.8 J.

Takeaway: Same two temperatures means the same ΔU\Delta U, whatever the process. All the difference between the two cases sits in ΔW\Delta W, and the ratio of the heats is γ\gamma.

Example 2: Getting RR out of laboratory data

For nitrogen, measurement gives cp=1040c_p = 1040 J/(kg K) and cv=743c_v = 743 J/(kg K). The molar mass of nitrogen is 28 g/mol. Show that these figures reproduce the universal gas constant, and find γ\gamma.

Solution:

  1. These are per-kilogram values, so the difference is RM\dfrac{R}{M}, not RR: cpcv=1040743=297 J/(kg K)c_p - c_v = 1040 - 743 = 297 \text{ J/(kg K)}

  2. Multiply by the molar mass in kg/mol, which is M=0.028M = 0.028: R=M(cpcv)=0.028×297=8.316 J/(mol K)R = M(c_p - c_v) = 0.028 \times 297 = 8.316 \text{ J/(mol K)} Against the accepted 8.3148.314, that is a 0.02% agreement from two ordinary measured numbers.

  3. The ratio needs no conversion at all, since the molar mass cancels: γ=cpcv=1040743=1.40\gamma = \frac{c_p}{c_v} = \frac{1040}{743} = 1.40 Nitrogen is diatomic, so 1.41.4 is exactly what the counting predicts.

Final Answer: R=8.32R = 8.32 J/(mol K); γ=1.40\gamma = 1.40.

Takeaway: Multiply a per-kilogram difference by MM to get a molar one; divide a molar one by MM to go back. And γ\gamma is the same number either way, which makes it the safest quantity to compute when you are unsure which units you were handed.

Example 3: From γ\gamma alone to both specific heats

A gas has γ=1.4\gamma = 1.4. Find its molar specific heats at constant volume and at constant pressure, and then find the same two quantities per kilogram if the gas is oxygen, M=32M = 32 g/mol.

Solution:

  1. Two equations, two unknowns. Mayer gives CpCv=RC_p - C_v = R and the definition gives Cp=γCvC_p = \gamma C_v. Substituting, γCvCv=RCv=Rγ1\gamma C_v - C_v = R \qquad\Longrightarrow\qquad C_v = \frac{R}{\gamma - 1}

  2. Put the numbers in: Cv=8.3141.41=8.3140.4=20.79 J/(mol K)C_v = \frac{8.314}{1.4 - 1} = \frac{8.314}{0.4} = 20.79 \text{ J/(mol K)} Cp=γCv=1.4×20.79=29.10 J/(mol K)C_p = \gamma C_v = 1.4 \times 20.79 = 29.10 \text{ J/(mol K)} Check: 29.1020.79=8.3129.10 - 20.79 = 8.31. Mayer holds.

  3. Per kilogram, divide by M=0.032M = 0.032 kg/mol: cv=20.790.032=649.5 J/(kg K),cp=29.100.032=909.3 J/(kg K)c_v = \frac{20.79}{0.032} = 649.5 \text{ J/(kg K)}, \qquad c_p = \frac{29.10}{0.032} = 909.3 \text{ J/(kg K)} And cpcv=259.8=8.3140.032c_p - c_v = 259.8 = \dfrac{8.314}{0.032}, as it must be.

Final Answer: Cv=20.79C_v = 20.79 and Cp=29.10C_p = 29.10 J/(mol K); for oxygen cv=649.5c_v = 649.5 and cp=909.3c_p = 909.3 J/(kg K).

Takeaway: Cv=Rγ1C_v = \dfrac{R}{\gamma - 1} and Cp=γRγ1C_p = \dfrac{\gamma R}{\gamma - 1} are the two most useful lines in the section. Nearly every adiabatic problem starts by using them.

Example 4: What fraction of the heat becomes work?

A gas is heated at constant pressure. What fraction of the heat supplied leaves as work done by the gas? Evaluate for a monatomic, a diatomic and a polyatomic gas.

Solution:

  1. Write both quantities for the same ΔT\Delta T. At constant pressure, ΔQ=nCpΔTandΔW=nRΔT\Delta Q = nC_p\Delta T \qquad\text{and}\qquad \Delta W = nR\Delta T

  2. Divide. The nn and the ΔT\Delta T cancel: ΔWΔQ=RCp=CpCvCp=11γ=γ1γ\frac{\Delta W}{\Delta Q} = \frac{R}{C_p} = \frac{C_p - C_v}{C_p} = 1 - \frac{1}{\gamma} = \frac{\gamma - 1}{\gamma}

  3. Evaluate for each family:

  • Monatomic, γ=53\gamma = \frac{5}{3}: fraction =2/35/3=0.40= \dfrac{2/3}{5/3} = 0.40, so 40%.
  • Diatomic, γ=1.4\gamma = 1.4: fraction =0.41.4=27=0.286= \dfrac{0.4}{1.4} = \dfrac{2}{7} = 0.286, so 28.6%.
  • Polyatomic, γ=43\gamma = \frac{4}{3}: fraction =1/34/3=0.25= \dfrac{1/3}{4/3} = 0.25, so 25%.
  1. Why the trend runs that way. A monatomic gas has the fewest places to bank energy internally, so a larger slice of the heat is left over to do work. A floppier molecule swallows more of the heat internally and pushes less.

Final Answer: ΔWΔQ=γ1γ\dfrac{\Delta W}{\Delta Q} = \dfrac{\gamma - 1}{\gamma}: 40%, 28.6% and 25% respectively.

Takeaway: In an isobaric process the split between ΔU\Delta U and ΔW\Delta W is decided entirely by γ\gamma. The rest goes into internal energy: ΔUΔQ=1γ\dfrac{\Delta U}{\Delta Q} = \dfrac{1}{\gamma}.

Example 5: One gram of helium under a free piston

One gram of helium in a cylinder fitted with a frictionless piston is heated at constant atmospheric pressure from 27°C to 127°C. Take the molar mass of helium as 4 g/mol. Find the heat supplied, the change in internal energy and the work done by the gas.

Solution:

  1. Kelvin first. 27°C=27+273.15=300.1527°C = 27 + 273.15 = 300.15 K and 127°C=400.15127°C = 400.15 K, both positive as they must be. The rise is ΔT=+100\Delta T = +100 K.

  2. Moles. n=mM=14=0.25n = \dfrac{m}{M} = \dfrac{1}{4} = 0.25 mol.

  3. Constants. Helium is monatomic: Cv=32R=12.47C_v = \frac{3}{2}R = 12.47 and Cp=52R=20.79C_p = \frac{5}{2}R = 20.79 J/(mol K).

  4. Heat supplied, at constant pressure: ΔQ=nCpΔT=0.25×20.79×100=519.6 J\Delta Q = nC_p\Delta T = 0.25 \times 20.79 \times 100 = 519.6 \text{ J}

  5. Internal energy, always through CvC_v: ΔU=nCvΔT=0.25×12.47×100=311.8 J\Delta U = nC_v\Delta T = 0.25 \times 12.47 \times 100 = 311.8 \text{ J}

  6. Work, from the first law or directly from nRΔTnR\Delta T: ΔW=ΔQΔU=519.6311.8=207.8 J\Delta W = \Delta Q - \Delta U = 519.6 - 311.8 = 207.8 \text{ J} check: nRΔT=0.25×8.314×100=207.85 J\text{check: } nR\Delta T = 0.25 \times 8.314 \times 100 = 207.85 \text{ J} \quad\checkmark

  7. The signs. All three are positive: heat flowed into the gas, its internal energy rose, and it did work on its surroundings by lifting the piston. Note that 40% of the heat left as work — exactly the monatomic fraction from Example 4.

Final Answer: ΔQ=+519.6\Delta Q = +519.6 J, ΔU=+311.8\Delta U = +311.8 J, ΔW=+207.8\Delta W = +207.8 J.

Takeaway: Convert the mass to moles before anything else, and convert the temperatures to kelvin even when only the difference is needed — it costs one line and it stops the habit of forgetting when a ratio does appear.

Example 6: Same heat, two containers

1000 J of heat is supplied to one mole of a diatomic gas, once at constant volume and once at constant pressure. Find the temperature rise in each case, and the ratio of the two.

Solution:

  1. Constant volume. All 1000 J becomes internal energy: ΔTV=ΔQnCv=10001×20.79=48.1 K\Delta T_V = \frac{\Delta Q}{nC_v} = \frac{1000}{1 \times 20.79} = 48.1 \text{ K}

  2. Constant pressure. Now some of the 1000 J is spent on work: ΔTP=ΔQnCp=10001×29.10=34.4 K\Delta T_P = \frac{\Delta Q}{nC_p} = \frac{1000}{1 \times 29.10} = 34.4 \text{ K}

  3. The ratio: ΔTVΔTP=CpCv=γ=1.40\frac{\Delta T_V}{\Delta T_P} = \frac{C_p}{C_v} = \gamma = 1.40

  4. Read the physics. The same 1000 J heats the gas 40% more when it is not allowed to expand, because none of it is diverted into work. In the constant-pressure case ΔW=nRΔTP=8.314×34.4=286\Delta W = nR\Delta T_P = 8.314 \times 34.4 = 286 J went into pushing, and only 714714 J into ΔU\Delta U.

Final Answer: 48.148.1 K at constant volume, 34.434.4 K at constant pressure; the ratio is γ=1.40\gamma = 1.40.

Takeaway: A gas that is free to expand is harder to heat. The ratio of the two temperature rises for the same heat is always exactly γ\gamma — a one-line answer worth recognising.

Example 7: An isobaric expansion, worked in full

Five moles of a monatomic ideal gas expand at a constant pressure of 2 atm from 0.0500.050 m3^3 to 0.0800.080 m3^3. Find the work done by the gas, the temperature change, the change in internal energy and the heat supplied. Verify the first law.

Solution:

  1. SI. P=2×1.013×105=2.026×105P = 2 \times 1.013 \times 10^5 = 2.026 \times 10^5 Pa; ΔV=0.0800.050=+0.030\Delta V = 0.080 - 0.050 = +0.030 m3^3.

  2. Work done by the gas. Pressure is constant, so ΔW=PΔV=2.026×105×0.030=6078 J\Delta W = P\,\Delta V = 2.026 \times 10^5 \times 0.030 = 6078 \text{ J} Positive, because the gas expanded.

  3. Temperature change, from PΔV=nRΔTP\Delta V = nR\Delta T: ΔT=PΔVnR=60785×8.314=146.2 K\Delta T = \frac{P\,\Delta V}{nR} = \frac{6078}{5 \times 8.314} = 146.2 \text{ K} (The initial temperature, if you want it, is T1=PV1nR=2.026×105×0.05041.57=243.7T_1 = \dfrac{PV_1}{nR} = \dfrac{2.026 \times 10^5 \times 0.050}{41.57} = 243.7 K — positive and absolute, as required.)

  4. Internal energy. Monatomic, Cv=12.47C_v = 12.47: ΔU=nCvΔT=5×12.47×146.2=9117 J\Delta U = nC_v\Delta T = 5 \times 12.47 \times 146.2 = 9117 \text{ J}

  5. Heat supplied, two ways: ΔQ=ΔU+ΔW=9117+6078=15195 J\Delta Q = \Delta U + \Delta W = 9117 + 6078 = 15195 \text{ J} check: nCpΔT=5×20.79×146.2=15195 J\text{check: } nC_p\Delta T = 5 \times 20.79 \times 146.2 = 15195 \text{ J} \quad\checkmark

  6. Signs. ΔQ>0\Delta Q > 0: heat entered. ΔU>0\Delta U > 0: the gas got hotter. ΔW>0\Delta W > 0: the gas did work on its surroundings. And 15195=9117+607815195 = 9117 + 6078 closes exactly.

Final Answer: ΔW=+6078\Delta W = +6078 J, ΔT=+146.2\Delta T = +146.2 K, ΔU=+9117\Delta U = +9117 J, ΔQ=+15195\Delta Q = +15195 J.

Takeaway: When a problem gives you PP and both volumes, get ΔW\Delta W first from PΔVP\Delta V, then ΔT\Delta T from PΔV=nRΔTP\Delta V = nR\Delta T. You never need the individual temperatures.

Example 8: Naming a gas from one number

An unknown gas is found to have a molar specific heat at constant volume of 24.924.9 J/(mol K). Identify the type of gas, and predict CpC_p and γ\gamma.

Solution:

  1. Express it in units of RR, which is where the structure shows: CvR=24.98.314=2.9953\frac{C_v}{R} = \frac{24.9}{8.314} = 2.995 \approx 3

  2. Match to the table. Cv=3RC_v = 3R means f2=3\dfrac{f}{2} = 3, so f=6f = 6: three translations plus three rotations. That is a polyatomic molecule that is not in a straight line — ammonia, methane, water vapour.

  3. Predict the other two: Cp=Cv+R=24.9+8.31=33.2 J/(mol K)C_p = C_v + R = 24.9 + 8.31 = 33.2 \text{ J/(mol K)} γ=CpCv=33.224.9=1.33=43\gamma = \frac{C_p}{C_v} = \frac{33.2}{24.9} = 1.33 = \frac{4}{3}

  4. Sanity check. γ=1.33\gamma = 1.33 lies between 1 and 53\frac{5}{3}, as every γ\gamma must.

Final Answer: A polyatomic (non-linear) gas; Cp=33.2C_p = 33.2 J/(mol K) and γ=431.33\gamma = \frac{4}{3} \approx 1.33.

Takeaway: Divide any molar specific heat by RR before you try to interpret it. 1.51.5, 2.52.5 and 3.03.0 for CvC_v — or 2.52.5, 3.53.5 and 4.04.0 for CpC_p — identify the gas instantly.

Example 9: Helium against carbon dioxide

One mole of helium and one mole of carbon dioxide are each heated through 50 K at constant pressure. Which needs more heat, and by what factor? Treat carbon dioxide as an ideal polyatomic gas with f=6f = 6.

Solution:

  1. Pick the right CpC_p for each. Helium is monatomic: Cp=52R=20.79C_p = \frac{5}{2}R = 20.79. Carbon dioxide, treated as polyatomic: Cp=4R=33.26C_p = 4R = 33.26 J/(mol K).

  2. Heat each: ΔQHe=1×20.79×50=1039.3 J\Delta Q_{\text{He}} = 1 \times 20.79 \times 50 = 1039.3 \text{ J} ΔQCO2=1×33.26×50=1662.8 J\Delta Q_{\text{CO}_2} = 1 \times 33.26 \times 50 = 1662.8 \text{ J}

  3. The factor: ΔQCO2ΔQHe=33.2620.79=1.60\frac{\Delta Q_{\text{CO}_2}}{\Delta Q_{\text{He}}} = \frac{33.26}{20.79} = 1.60

  4. Why. Both gases contain the same number of molecules and both push their surroundings back by the same nRΔT=415.7nR\Delta T = 415.7 J. The whole difference is internal: a carbon dioxide molecule has six ways to hold energy against helium's three, so it swallows twice as much internally. Both ΔQ\Delta Q values are positive — heat added — as is each ΔU\Delta U, and each ΔW\Delta W is +415.7+415.7 J.

Final Answer: Carbon dioxide needs 1.6 times as much heat: 1662.81662.8 J against 1039.31039.3 J.

Takeaway: Per mole, the more complicated molecule always costs more to heat. Per kilogram the comparison can invert completely, because a mole of helium weighs 4 g and a mole of carbon dioxide weighs 44 g.

Example 10: Hydrogen's staircase, in joules

How much heat is needed to raise the temperature of one mole of hydrogen by 10 K at constant volume (a) around 100 K, where only translation is active, (b) at room temperature, where rotation has switched on, and (c) around 3000 K, where vibration has also switched on and f=7f = 7?

Solution:

  1. Use Cv=f2RC_v = \frac{f}{2}R for each regime, and ΔQ=nCvΔT\Delta Q = nC_v\Delta T with n=1n = 1 and ΔT=10\Delta T = 10 K.

  2. (a) f=3f = 3: Cv=1.5×8.314=12.47C_v = 1.5 \times 8.314 = 12.47, so ΔQ=12.47×10=124.7 J\Delta Q = 12.47 \times 10 = 124.7 \text{ J}

  3. (b) f=5f = 5: Cv=2.5×8.314=20.79C_v = 2.5 \times 8.314 = 20.79, so ΔQ=20.79×10=207.9 J\Delta Q = 20.79 \times 10 = 207.9 \text{ J}

  4. (c) f=7f = 7: Cv=3.5×8.314=29.10C_v = 3.5 \times 8.314 = 29.10, so ΔQ=29.10×10=291.0 J\Delta Q = 29.10 \times 10 = 291.0 \text{ J}

  5. All three ΔQ\Delta Q are positive and, since the volume is fixed, ΔW=0\Delta W = 0 and ΔU=ΔQ\Delta U = \Delta Q in every case. The same gas, the same ten kelvin, and the bill more than doubles between the coldest and the hottest case — purely because more storage modes have woken up.

Final Answer: (a) 124.7124.7 J; (b) 207.9207.9 J; (c) 291.0291.0 J.

Takeaway: CvC_v is not a constant of a gas; it is a constant of a gas in a temperature range. For everything in this chapter, use the room-temperature value unless told otherwise.

Example 11: Predicting the specific heat of copper

Use the counting rule for a solid to predict the specific heat capacity of copper in J/(kg K), given M=63.5M = 63.5 g/mol, and compare with the measured value of 385 J/(kg K).

Solution:

  1. Count for a solid. Each atom oscillates about a fixed site in three directions, and an oscillator stores energy both as kinetic and as potential — two forms per direction, so six in all: C=62R=3R=3×8.314=24.94 J/(mol K)C = \frac{6}{2}R = 3R = 3 \times 8.314 = 24.94 \text{ J/(mol K)}

  2. Convert to per kilogram with M=0.0635M = 0.0635 kg/mol: c=CM=24.940.0635=392.8 J/(kg K)c = \frac{C}{M} = \frac{24.94}{0.0635} = 392.8 \text{ J/(kg K)}

  3. Compare. The measured value is 385, so the prediction is high by 392.8385385=2.0%\frac{392.8 - 385}{385} = 2.0\% which is remarkable for a calculation containing no information about copper except how heavy one mole of it is.

  4. A note on CpC_p against CvC_v. For a solid this argument gives essentially both at once. Copper's volume expands by roughly 0.005% per kelvin, so the work it does pushing the atmosphere aside is a few thousandths of a joule per mole per kelvin — utterly negligible beside 24.9 J. Hence one specific heat, not two.

Final Answer: c393c \approx 393 J/(kg K), about 2% above the measured 385 J/(kg K).

Takeaway: C3R25C \approx 3R \approx 25 J/(mol K) for most solids at room temperature. Divide by the molar mass to get the per-kilogram value, and expect agreement within a few percent.

Example 12: When "the molar specific heat" is a meaningless question

A gas is taken through (a) an isothermal expansion in which 500 J of heat is absorbed, and (b) an adiabatic expansion. What is the molar specific heat of the gas in each process? What does this tell you?

Solution:

  1. Start from the definition, C=1nΔQΔTC = \dfrac{1}{n}\dfrac{\Delta Q}{\Delta T}, and read each process honestly.

  2. (a) Isothermal. By definition the temperature does not change, so ΔT=0\Delta T = 0, while ΔQ=+500\Delta Q = +500 J is definitely not zero: C=1n5000C = \frac{1}{n}\frac{500}{0} \rightarrow \infty The molar specific heat is infinite. Physically: you can pour in any amount of heat and the temperature will not move a millikelvin, because all of it leaves again as work. Signs: ΔQ=+500\Delta Q = +500 J (heat added), ΔU=0\Delta U = 0 (temperature fixed, ideal gas), so ΔW=+500\Delta W = +500 J (all of it done by the gas).

  3. (b) Adiabatic. By definition ΔQ=0\Delta Q = 0, while the temperature certainly does change: C=1n0ΔT=0C = \frac{1}{n}\frac{0}{\Delta T} = 0 The molar specific heat is zero. Physically: the gas cools as it expands without any heat leaving at all. Signs: ΔQ=0\Delta Q = 0, ΔW>0\Delta W > 0 for an expansion, so ΔU=ΔW<0\Delta U = -\Delta W < 0 — the internal energy falls and the gas gets colder.

  4. The lesson. Between 00 and \infty lies every value, including negative ones for suitably chosen processes. So "the molar specific heat of oxygen" is an incomplete question. CvC_v and CpC_p are singled out and given names because those two processes are the ones that recur.

Final Answer: Isothermal, CC \to \infty; adiabatic, C=0C = 0.

Takeaway: CC belongs to the process, not to the gas. Whenever you write a CC, be able to name which process it goes with — and if you cannot, you do not yet have enough information to answer.