Physics by Lamhi: Not Your Boring Physics

CLASS 11 · CHAPTER 12 · HEAT

DETAILED NOTES

Kinetic Theory

The complete chapter, section by section: how molecular chaos produces the orderly ideal gas law, the full derivation of pressure from first principles, why temperature really is average molecular kinetic energy, equipartition of energy, specific heats, and mean free path, explained in plain language with original worked examples. For the interactive molecules-in-a-box simulation, see the concept page.

12.1 The Molecular Nature of Matter and the Ideal Gas Equation

Everything in this chapter rests on one working picture of a gas: a huge number of molecules, each a tiny point of mass, flying about in straight lines at random, colliding elastically with each other and with the walls of their container, and otherwise exerting no force on one another at all. This is the ideal gas model. No real gas obeys it exactly, but dilute gases well above their liquefaction temperature (air in this room, for instance) come astonishingly close, which is exactly why it is worth building a whole theory around.

Experimentally, long before anyone could watch a single molecule, this picture was already compressed into one empirical law relating a gas’s pressure PP, volume VV, and absolute temperature TT:

Ideal gas equation
PV=μRT=NkBTPV = \mu RT = Nk_BT

Here μ\mu is the number of moles, NN the total number of molecules, RR the universal gas constant (8.314 J/mol·K), and kBk_B the Boltzmann constant, simply the gas constant rewritten per molecule instead of per mole:

Boltzmann constant
kB=RNA=8.3146.022×1023≈1.38×10−23 J/Kk_B = \dfrac{R}{N_A} = \dfrac{8.314}{6.022\times10^{23}} \approx 1.38\times10^{-23}\text{ J/K}

The rest of this chapter’s job is to show that this equation, along with everything it implies about temperature and heat, is not a separate law of nature at all. It falls straight out of Newton’s laws applied to a swarm of colliding molecules, once you stop tracking individual molecules and start tracking their statistical averages.

Worked example

How many molecules are in a sealed litre flask?

A 1.0 litre flask is sealed at atmospheric pressure (1.0×105 Pa1.0\times10^5\text{ Pa}) and room temperature (300 K). Estimate the number of gas molecules inside it.

Rearranging PV=NkBTPV = Nk_BT for NN, with V=1.0×10−3 m3V = 1.0\times10^{-3}\text{ m}^3:

N=PVkBT=(1.0×105)(1.0×10−3)(1.38×10−23)(300)≈2.4×1022 moleculesN = \dfrac{PV}{k_BT} = \dfrac{(1.0\times10^5)(1.0\times10^{-3})}{(1.38\times10^{-23})(300)} \approx \textcolor{#e08a1e}{2.4\times10^{22}\text{ molecules}}

Roughly twenty-four thousand billion billion molecules, in a volume you could hold in one hand, every one of them obeying nothing more exotic than Newton’s laws.

12.2 Kinetic Theory of an Ideal Gas: Deriving Pressure

Here is the central derivation of the chapter: where gas pressure actually comes from. Picture a cubical box of side LL containing NN identical molecules, each of mass mm, moving randomly and never interacting with each other, only bouncing elastically off the walls.

Take one molecule with velocity component vxv_x perpendicular to a particular wall. An elastic collision with a rigid wall simply reverses that component, vx→−vxv_x \to -v_x, leaving its speed unchanged, so the molecule’s momentum change is −2mvx-2mv_x, and by Newton’s third law the wall receives momentum +2mvx+2mv_x on every such hit.

After bouncing off this wall, the molecule must cross the box, hit the opposite wall, and return, a round trip of distance 2L2L, before it can strike this wall again. So it delivers a momentum kick of 2mvx2mv_x once every 2L/vx2L/v_x seconds, which is exactly a steady average force on the wall of:

f=2mvx2L/vx=mvx2Lf = \dfrac{2mv_x}{2L/v_x} = \dfrac{mv_x^2}{L}

Summing this over all NN molecules gives the total force on that wall, F=mL∑vx2=Nm⟨vx2⟩LF = \dfrac{m}{L}\sum v_x^2 = \dfrac{Nm\langle v_x^2\rangle}{L}, where ⟨vx2⟩\langle v_x^2\rangle is the average of vx2v_x^2 over all the molecules. Dividing by the wall’s area L2L^2 gives the pressure:

P=FL2=Nm⟨vx2⟩L3=Nm⟨vx2⟩VP = \dfrac{F}{L^2} = \dfrac{Nm\langle v_x^2\rangle}{L^3} = \dfrac{Nm\langle v_x^2\rangle}{V}

Nothing in the setup singled out the xx-direction, so by symmetry ⟨vx2⟩=⟨vy2⟩=⟨vz2⟩\langle v_x^2\rangle = \langle v_y^2\rangle = \langle v_z^2\rangle, and since v2=vx2+vy2+vz2v^2 = v_x^2+v_y^2+v_z^2 for every molecule, each of these three equal pieces must be exactly one third of the total: ⟨vx2⟩=13⟨v2⟩\langle v_x^2\rangle = \tfrac{1}{3}\langle v^2\rangle. Substituting this in gives the chapter’s key result:

Pressure from kinetic theory
P=13NmV⟨v2⟩=13ρ⟨v2⟩,PV=13Nm⟨v2⟩\textcolor{#e08a1e}{P} = \dfrac{1}{3}\dfrac{Nm}{V}\langle v^2\rangle = \dfrac{1}{3}\rho\langle v^2\rangle, \qquad PV = \dfrac{1}{3}Nm\langle v^2\rangle

where ρ=Nm/V\rho = Nm/V is the gas’s mass density and ⟨v2⟩\langle v^2\rangle is the mean square speed, averaged over every molecule in the box. Notice what this derivation never assumed: it never needed molecules to push against each other, only against the walls. A gas of molecules that never collided with one another at all would still, by this argument, exert a perfectly ordinary pressure.

Worked example

RMS speed of carbon dioxide from its density

A sample of carbon dioxide gas has density 1.98 kg/m31.98\text{ kg/m}^3 at a pressure of 1.0×105 Pa1.0\times10^5\text{ Pa}. Find the rms speed of its molecules.

Rearranging P=13ρ⟨v2⟩P = \tfrac{1}{3}\rho\langle v^2\rangle for vrms=⟨v2⟩v_{rms} = \sqrt{\langle v^2\rangle}:

vrms=3Pρ=3(1.0×105)1.98≈389 m/sv_{rms} = \sqrt{\dfrac{3P}{\rho}} = \sqrt{\dfrac{3(1.0\times10^5)}{1.98}} \approx \textcolor{#e08a1e}{389\text{ m/s}}

A single equation, built purely from the mechanics of elastic collisions, already lets you read off a molecular speed from two bulk, everyday, thermometer-and-scale measurements.

12.3 Kinetic Interpretation of Temperature, and RMS Speed

The derivation above is mechanics alone, it never mentioned temperature. The link appears the moment you compare it with the §12.1 ideal gas equation. Both expressions give PVPV, so they must be equal:

13Nm⟨v2⟩=NkBT\dfrac{1}{3}Nm\langle v^2\rangle = Nk_BT

The NN cancels, and rearranging gives one of the most important results in all of thermal physics:

Kinetic interpretation of temperature
12m⟨v2⟩=32kBT\tfrac{1}{2}m\langle v^2\rangle = \tfrac{3}{2}k_BT

The left side is the average translational kinetic energy per molecule. The right side is a multiple of absolute temperature alone. In other words, temperature is not some separate quantity that happens to be correlated with molecular motion, it is a direct, literal measure of the average kinetic energy of molecular motion, and nothing else about the gas (its pressure, its volume, which gas it even is) enters this relation at all. Taking the square root of ⟨v2⟩\langle v^2\rangle gives the rms speed:

RMS speed
vrms=⟨v2⟩=3kBTm=3RTMv_{rms} = \sqrt{\langle v^2\rangle} = \sqrt{\dfrac{3k_BT}{m}} = \sqrt{\dfrac{3RT}{M}}

with M=NAmM = N_Am the molar mass. This is exactly the quantity the molecules-in-a-box simulation on the concept page tracks, and it is worth being precise about what it depends on and what it does not. vrmsv_{rms} depends only on TT (for a fixed gas). It does not appear anywhere in terms of PP or VV separately, even though PP and VV were exactly what the §12.2 derivation was built from.

This is why squeezing the same gas into a smaller fixed box, at the same temperature, does not speed its molecules up at all. The pressure rises, but purely because the molecules now hit the (closer) walls more often, not because any molecule is moving any faster between hits. In the simulation, dragging the Volume slider visibly shrinks the box and visibly changes the pressure readout, while every single dot keeps exactly the speed it had before. Only dragging Temperature changes how fast the dots move. That separation, speed is set by TT alone, pressure is set by TT and the collision rate that VV controls, is the single most important idea in this section.

Worked example

Comparing hydrogen and oxygen at the same temperature

Find the rms speed of hydrogen (M=2 g/molM = 2\text{ g/mol}) and of oxygen (M=32 g/molM = 32\text{ g/mol}) molecules at 300 K, and compare them.

vrms(H2)=3(8.314)(300)0.002≈1934 m/sv_{rms}(\text{H}_2) = \sqrt{\dfrac{3(8.314)(300)}{0.002}} \approx \textcolor{#e08a1e}{1934\text{ m/s}}vrms(O2)=3(8.314)(300)0.032≈484 m/sv_{rms}(\text{O}_2) = \sqrt{\dfrac{3(8.314)(300)}{0.032}} \approx \textcolor{#e08a1e}{484\text{ m/s}}

The ratio is 1934/484≈4.01934/484 \approx 4.0, exactly 32/2=16=4\sqrt{32/2} = \sqrt{16} = 4, as the vrms∝1/Mv_{rms}\propto 1/\sqrt{M} scaling demands. Both gases, at the same 300 K, carry the same average kinetic energy per molecule, 32kBT\tfrac{3}{2}k_BT; hydrogen molecules only move faster because they carry sixteen times less mass to carry that same energy in.

12.4 Law of Equipartition of Energy

Section 12.3 derived 12m⟨v2⟩=32kBT\tfrac{1}{2}m\langle v^2\rangle = \tfrac{3}{2}k_BT by counting three independent translational directions, xx, yy, and zz, each contributing an equal share, 12kBT\tfrac{1}{2}k_BT, to the total. The law of equipartition of energy generalises this counting argument far beyond translation:

In thermal equilibrium, the total energy of a system is shared equally among every independent (quadratic) degree of freedom available to it, each contributing an average of 12kBT\tfrac{1}{2}k_BT, regardless of the nature of that degree of freedom or the temperature.

A “degree of freedom” here just means an independent way a molecule can store energy that enters its energy expression as a square, a velocity component, an angular velocity component, a spring-like displacement. Translation along xx, yy, and zz gives three such terms for any molecule; what changes between gases is what else is available besides translation.

12.4.1 Monatomic gases

A monatomic molecule (helium, argon, a single atom with essentially all its mass at a point) has only the three translational degrees of freedom. Its average energy per molecule is 3×12kBT=32kBT3\times\tfrac{1}{2}k_BT = \tfrac{3}{2}k_BT, exactly the §12.3 result, so for μ\mu moles (N=μNAN=\mu N_A molecules), the total internal energy is:

U=μ(32NAkBT)=32μRTU = \mu\left(\tfrac{3}{2}N_Ak_BT\right) = \tfrac{3}{2}\mu RT

12.4.2 Diatomic gases

A diatomic molecule (N2, O2, the air around you) is a tiny dumbbell. Besides the same three translational terms, it can also rotate, about two axes perpendicular to the bond, since it has essentially no moment of inertia about the bond axis itself, that spin stores no measurable energy. So a rigid diatomic molecule has 3+2=53+2=5 degrees of freedom at moderate temperatures:

U=μ(5×12RT)=52μRTU = \mu\left(5\times\tfrac{1}{2}RT\right) = \tfrac{5}{2}\mu RT

A real diatomic bond can also vibrate, which would add two more quadratic terms (vibrational kinetic and potential energy), pushing the total to 77 degrees of freedom at high enough temperature. But vibration is quantised with a large energy gap, so at ordinary temperatures it stays almost entirely “frozen out”, which is exactly why N2 and O2 behave as 5-degree-of-freedom gases near room temperature and only drift toward the 7-degree value at much higher temperatures.

12.5 Specific Heats of Gases from Equipartition

Equipartition hands over the internal energy U(T)U(T) of an ideal gas directly, and specific heats are just derivatives of that. The molar specific heat at constant volume is defined as the heat needed per mole per degree, with volume held fixed, so no work is done and all the heat goes into raising UU:

Cv=1μdUdTC_v = \dfrac{1}{\mu}\dfrac{dU}{dT}

12.5.1 Monatomic gases

From U=32μRTU = \tfrac{3}{2}\mu RT:

Cv=32R≈12.5 J/mol⋅K,Cp=Cv+R=52R,γ=CpCv=53C_v = \tfrac{3}{2}R \approx 12.5\text{ J/mol·K}, \qquad C_p = C_v + R = \tfrac{5}{2}R, \qquad \gamma = \dfrac{C_p}{C_v} = \dfrac{5}{3}

12.5.2 Diatomic gases

From U=52μRTU = \tfrac{5}{2}\mu RT (rigid, moderate temperature):

Cv=52R≈20.8 J/mol⋅K,Cp=Cv+R=72R,γ=CpCv=75C_v = \tfrac{5}{2}R \approx 20.8\text{ J/mol·K}, \qquad C_p = C_v + R = \tfrac{7}{2}R, \qquad \gamma = \dfrac{C_p}{C_v} = \dfrac{7}{5}

The step Cp=Cv+RC_p = C_v + R used above, Mayer’s relation, is not specific to monatomic or diatomic gases, it holds for any ideal gas, and is worth deriving once in general. For μ=1\mu=1 mole, PV=RTPV=RT, so at constant pressure, P dV=R dTP\,dV = R\,dT. The first law gives dQ=dU+P dV=Cv dT+R dTdQ = dU + P\,dV = C_v\,dT + R\,dT, and since this same dQdQ at constant pressure is by definition Cp dTC_p\,dT, matching coefficients gives:

Mayer's relation
Cp−Cv=R\textcolor{#e08a1e}{C_p - C_v} = R

The extra RR is simply the work a gas does pushing back its surroundings as it expands at constant pressure, work a gas held at constant volume never has to do, so it always takes more heat to raise its temperature by one degree at constant pressure than at constant volume.

Worked example

Heating a diatomic gas at constant volume

2.0 mol of nitrogen gas (treated as a rigid diatomic ideal gas) is heated at constant volume through 50 K. Find the increase in its internal energy. (R=8.314 J/mol⋅KR = 8.314\text{ J/mol·K})

At constant volume, all the heat becomes internal energy:

ΔU=μCvΔT=(2.0)(52×8.314)(50)≈2.08×103 J\Delta U = \mu C_v\Delta T = (2.0)\left(\tfrac{5}{2}\times8.314\right)(50) \approx \textcolor{#e08a1e}{2.08\times10^3\text{ J}}

about 2.08 kJ, five-halves times what the same calculation would give for a monatomic gas of the same amount and temperature rise, exactly the extra rotational degrees of freedom at work.

12.6 Mean Free Path

Section 12.3’s rms speeds come out to hundreds of metres per second, faster than sound. Yet open a bottle of perfume across a still room and the smell visibly takes minutes to arrive, not milliseconds. The resolution is that a molecule almost never travels in a straight line for long: real molecules have a finite size, and they constantly collide with each other, each collision flinging them off in a new, effectively random direction.

The average distance a molecule covers between one collision and the next is its mean free path, λ\lambda. For a gas of molecules of effective diameter dd and number density n=N/Vn = N/V, a reasonably careful count of how many other molecules lie within a molecule’s collision “tube” as it travels gives:

Mean free path
λ=12 πd2n\lambda = \dfrac{1}{\sqrt{2}\,\pi d^2 n}

Using n=P/(kBT)n = P/(k_BT) from the ideal gas equation, this can equally be written in terms of pressure and temperature directly, which is often more convenient:

λ=kBT2 πd2P\lambda = \dfrac{k_BT}{\sqrt{2}\,\pi d^2P}

Two features are worth remembering. First, λ\lambda shrinks as pressure rises (more molecules packed into the same space means more frequent collisions) and grows with temperature at fixed pressure. Second, λ\lambda is typically hundreds of molecular diameters even at atmospheric pressure, a molecule travels a long way, relatively speaking, before each collision, but it does so in a random zig-zag, not a straight line, which is exactly why diffusion is so much slower than the rms speed alone would suggest. The worked exercise below puts real numbers to both λ\lambda and the rate of collisions this implies.

— From the NCERT exercises

Two of the chapter’s own classic exercise questions, with original worked solutions.

NCERT Exercise 13.9

At what temperature is the rms speed of an argon gas atom equal to the rms speed of a helium gas atom at -20°C? (Atomic mass of Ar = 39.9 u, of He = 4.0 u.)

Solution

Since vrms=3RT/Mv_{rms} = \sqrt{3RT/M}, equal rms speeds for the two gases require equal T/MT/M:

TArMAr=THeMHe⇒TAr=THe×MArMHe\dfrac{T_{Ar}}{M_{Ar}} = \dfrac{T_{He}}{M_{He}} \quad\Rightarrow\quad T_{Ar} = T_{He}\times\dfrac{M_{Ar}}{M_{He}}

With THe=−20°C=253 KT_{He} = -20°\text{C} = 253\text{ K}:

TAr=253×39.94.0≈2.52×103 KT_{Ar} = 253\times\dfrac{39.9}{4.0} \approx \textcolor{#e08a1e}{2.52\times10^3\text{ K}}

Argon, being nearly ten times heavier per atom, needs a correspondingly much higher temperature to shake its atoms up to the same speed as helium’s.

NCERT Exercise 13.10

Estimate the mean free path and collision frequency of a nitrogen molecule in a cylinder of nitrogen at a pressure of 2.0 atm and temperature 17°C. Take the radius of a nitrogen molecule to be about 1.0 Å. (Molar mass of N2 = 28.0 g/mol.)

Solution

Diameter d=2×1.0 A˚=2.0×10−10 md = 2\times1.0\text{ Å} = 2.0\times10^{-10}\text{ m}, P=2.0 atm≈2.03×105 PaP = 2.0\text{ atm} \approx 2.03\times10^5\text{ Pa}, T=290 KT = 290\text{ K}. Using the pressure form of the mean free path:

λ=kBT2 πd2P=(1.38×10−23)(290)2 π(2.0×10−10)2(2.03×105)≈1.11×10−7 m\lambda = \dfrac{k_BT}{\sqrt{2}\,\pi d^2P} = \dfrac{(1.38\times10^{-23})(290)}{\sqrt{2}\,\pi(2.0\times10^{-10})^2(2.03\times10^5)} \approx \textcolor{#e08a1e}{1.11\times10^{-7}\text{ m}}

about 550 molecular diameters. The rms speed at this temperature:

vrms=3RTM=3(8.314)(290)0.028≈508 m/sv_{rms} = \sqrt{\dfrac{3RT}{M}} = \sqrt{\dfrac{3(8.314)(290)}{0.028}} \approx 508\text{ m/s}

so a molecule suffers, on average, a collision every:

λvrms=1.11×10−7508≈2.2×10−10 s,i.e. a collision frequency of    vrmsλ≈4.6×109 per second\dfrac{\lambda}{v_{rms}} = \dfrac{1.11\times10^{-7}}{508} \approx 2.2\times10^{-10}\text{ s}, \quad\text{i.e. a collision frequency of}\;\; \dfrac{v_{rms}}{\lambda} \approx \textcolor{#e08a1e}{4.6\times10^9\text{ per second}}

Roughly four and a half billion collisions every second for every single molecule, despite each one travelling at over 500 m/s between hits.