Physics · Book 3 · Bachelor Year 1

University Physics — Year 1

University Physics — Year 1 · Bachelor Year 1

20Kinetic Theory and the Perfect Gas

The air in a classroom weighs as much as a grown man, and contains more molecules than there are grains of sand on Earth, each flying at the speed of a rifle bullet and colliding ten billion times a second with its neighbors. Nobody can follow one of them; nobody needs to. A handful of averages — pressure, temperature, volume, amount — describe the air completely for every purpose of engineering, and a simple picture of molecules bouncing off walls explains where those averages come from and how they are related. This chapter opens the thermodynamics part of the volume by looking at matter from both ends: the microscopic chaos and the macroscopic calm, and the kinetic theory that connects them in the case of the perfect gas.

20.1 Two scales of description

Definition 20.1 (Microscopic and macroscopic scales)

At the microscopic scale matter is made of molecules: 1 mol1\,\mathrm{mol} contains NA=6.02×1023 N_A = 6.02 \times 10^{23}\, of them, each about 0.3 nm0.3\,\mathrm{nm} across; in a gas at ordinary conditions they are 3 nm3\,\mathrm{nm} apart, move at hundreds of meters per second and collide every 70 nm70\,\mathrm{nm} or so. At the macroscopic scale a system is described by a few state variables — pressure PP, volume VV, temperature TT, amount of substance nn — that are averages over enormous numbers of molecules. A variable is extensive if it doubles when the system is doubled (VV, nn, mass, energy), intensive if it does not (PP, TT, density).

Definition 20.2 (Thermodynamic equilibrium)

A system is in thermodynamic equilibrium when its state variables are uniform and constant in time and no macroscopic flow of matter or energy crosses it. Only then are PP and TT defined for the system as a whole; the equation of state links them to VV and nn.

Definition 20.3 (Pressure)

A fluid at rest pushes on every surface element  ⁣dS\dd S of a wall with a force  ⁣dF→=P  ⁣dS n→\dd\vect F = P\,\dd S\,\vect n normal to it, toward the wall; PP is the pressure, in pascals (1 Pa=1 N/m21\,\mathrm{Pa} = 1\,\mathrm{N}/\mathrm{m}^{2}); 1 bar=1×105 Pa1\,\mathrm{bar} = 1 \times 10^{5}\,\mathrm{Pa}, 1 atm=1.013×105 Pa1\,\mathrm{atm} = 1.013 \times 10^{5}\,\mathrm{Pa}. At a given point it does not depend on the orientation of the surface (Chapter 21).

Definition 20.4 (Temperature)

Two systems in contact through a wall that lets energy pass reach, in time, a common state: they are then at the same temperature, and two bodies each in equilibrium with a third are in equilibrium with each other (the zeroth law). The kelvin scale is fixed by kB=1.380 649×10−23 J/Kk_B = 1.380\,649 \times 10^{-23}\,\mathrm{J}/\mathrm{K} exactly; Celsius: θ=T−273.15\theta = T - 273.15. The kinetic theory below gives TT its microscopic meaning.

20.2 The kinetic model of the perfect gas

Definition 20.5 (Perfect gas, microscopic model)

A perfect gas (ideal gas) is a collection of NN molecules, treated as points of mass mm, moving freely and at random — no interaction except brief collisions — in a container of volume VV. At equilibrium the velocity distribution is isotropic and stationary; n∗=N/Vn^* = N/V is the number density and ⟨v2⟩\langle v^2\rangle the mean square speed.

Theorem 20.6 (Kinetic pressure)

The pressure exerted by the gas on the walls is

P=13 n∗m⟨v2⟩=23 n∗⟨ϵk⟩,P = \tfrac13\,n^*m\langle v^2\rangle = \tfrac23\,n^*\langle\epsilon_k\rangle ,

where ⟨ϵk⟩=12m⟨v2⟩\langle\epsilon_k\rangle = \tfrac12 m\langle v^2\rangle is the mean kinetic energy of a molecule.

Partial proof. Take the simplified model in which the molecules all have speed uu and move along the three axes, one sixth in each direction. A molecule hitting the wall x=0x = 0 head-on bounces back elastically and delivers the momentum 2mu2mu to it. In time  ⁣dt\dd t, the molecules moving toward the wall that reach an area SS are those within the slab u  ⁣dtu\,\dd t thick, one sixth of the n∗Su  ⁣dtn^*Su\,\dd t molecules there. Force == momentum per time =(n∗Su  ⁣dt/6)(2mu)/ ⁣dt=13n∗mu2S= (n^*Su\,\dd t/6)(2mu)/\dd t = \tfrac13 n^*mu^2S, so P=13n∗mu2P = \tfrac13 n^*mu^2. Averaging over the actual distribution of speeds and directions replaces u2u^2 by ⟨v2⟩\langle v^2\rangle (the isotropy gives ⟨vx2⟩=13⟨v2⟩\langle v_x^2\rangle = \tfrac13\langle v^2\rangle); the Year 2 volume does it in full. ∎

Left: the kinetic origin of pressure — molecules striking a wall and bouncing back deliver momentum to it; their number per second times 2mu is the force. Right: the actual speeds are spread (Maxwell’s distribution, here for nitrogen at two temperatures); the model’s single u is replaced by the root-mean-square speed.
Left: the kinetic origin of pressure — molecules striking a wall and bouncing back deliver momentum to it; their number per second times 2mu2mu is the force. Right: the actual speeds are spread (Maxwell’s distribution, here for nitrogen at two temperatures); the model’s single uu is replaced by the root-mean-square speed.

Definition 20.7 (Kinetic temperature; equation of state)

The temperature of a perfect gas is defined by the mean kinetic energy of its molecules,

⟨ϵk⟩=12m⟨v2⟩=32kBT,\langle\epsilon_k\rangle = \tfrac12 m\langle v^2\rangle = \tfrac32 k_BT ,

so that, combining with Theorem 20.6,

PV=NkBT=nRT,R=NAkB=8.314 J/(mol K),PV = Nk_BT = nRT, \qquad R = N_Ak_B = 8.314\,\mathrm{J}/(\mathrm{mol}\,\mathrm{K}) ,

the equation of state of the perfect gas. The root-mean-square speed is u=⟨v2⟩=3kBT/m=3RT/Mu = \sqrt{\langle v^2\rangle} = \sqrt{3k_BT/m} = \sqrt{3RT/M}, MM the molar mass.

Example 20.8 (Numbers for air)

Nitrogen at 300 K300\,\mathrm{K}: u=3×8.314×300/0.028=517 m/su = \sqrt{3 \times 8.314 \times 300/0.028} = 517\,\mathrm{m}/\mathrm{s}; hydrogen, 1930 m/s1930\,\mathrm{m}/\mathrm{s}; the heavier the slower, as 1/M1/\sqrt M. At 1 bar1\,\mathrm{bar} and 300 K300\,\mathrm{K}, n∗=P/kBT=2.4×1025 m−3n^* = P/k_BT = 2.4 \times 10^{25}\,\mathrm{m}^{-3}: 24 L24\,\mathrm{L} per mole, 2.7×1022 2.7 \times 10^{22}\, molecules in a liter. A classroom of 200 m3200\,\mathrm{m}^{3}: 8300 mol8300\,\mathrm{mol}, 240 kg240\,\mathrm{kg} of air.

Remark 20.9 (Why the model works, and when it fails)

Between collisions a molecule of air flies a mean free path λ≈1/(2πd2n∗)≈70 nm\lambda \approx 1/(\sqrt2\pi d^2n^*) \approx 70\,\mathrm{nm} — two hundred times its size: the gas is mostly empty, interactions are rare, and PV=nRTPV = nRT holds to better than a percent at ordinary pressures. At high pressure or low temperature the molecules’ own volume and their attraction matter: van der Waals’s equation (P+an2/V2)(V−nb)=nRT(P + an^2/V^2)(V - nb) = nRT corrects for both, and below a critical temperature the gas liquefies (Chapter 25).

The Clapeyron diagram of a perfect gas: at each temperature the isotherm is a hyperbola P = nRT/V, higher for higher T. A transformation is a path in this plane; a cycle, a closed loop ().
The Clapeyron diagram of a perfect gas: at each temperature the isotherm is a hyperbola P=nRT/VP = nRT/V, higher for higher TT. A transformation is a path in this plane; a cycle, a closed loop (Chapter 24).

20.3 Internal energy of the perfect gas

Definition 20.10 (Internal energy)

The internal energy UU of a system is the sum of the kinetic energies of its molecules in the frame where the system is at rest and of their mutual potential energies; it is an extensive state function.

Proposition 20.11 (Internal energy of perfect gases)

For a perfect gas UU depends on TT alone (first Joule law):

U=32nRT(monatomic: He, Ne, Ar),U=52nRT(diatomic at ordinary temperatures: N2,O2,H2),\begin{gather*} U = \tfrac32 nRT \quad (\text{monatomic: He, Ne, Ar}), \\ U = \tfrac52 nRT \quad (\text{diatomic at ordinary temperatures: N}_2, \text{O}_2, \text{H}_2), \end{gather*}

so the molar heat capacity at constant volume CV,m= ⁣dUm/ ⁣dTC_{V,m} = \dd U_m/\dd T is 32R=12.5 J/(mol K)\tfrac32 R = 12.5\,\mathrm{J}/(\mathrm{mol}\,\mathrm{K}) and 52R=20.8 J/(mol K)\tfrac52 R = 20.8\,\mathrm{J}/(\mathrm{mol}\,\mathrm{K}) respectively.

Partial proof. No mutual potential energy by hypothesis, so U=N⟨ϵk⟩=32NkBTU = N\langle\epsilon_k\rangle = \tfrac32 Nk_BT for point molecules. A diatomic molecule also rotates: each of its two rotational degrees of freedom carries, at equilibrium, the same 12kBT\tfrac12 k_BT as each translational one (the equipartition theorem, admitted; the Year 3 volume derives it and explains why the vibration joins in only above a thousand kelvins). ∎

Example 20.12 (A room’s worth)

The 8300 mol8300\,\mathrm{mol} of air in the classroom at 300 K300\,\mathrm{K}: U=52×8300×8.314×300=5.2×107 JU = \tfrac52 \times 8300 \times 8.314 \times 300 = 5.2 \times 10^{7}\,\mathrm{J} — the energy of a liter and a half of gasoline, held in molecular motion. Warming the room by 11 K costs 52nR=170 kJ\tfrac52 nR = 170\,\mathrm{kJ} (at constant volume).

20.4 Condensed phases

Proposition 20.13 (Model of the incompressible, indilatable phase)

Liquids and solids are modeled, at this level, as phases of fixed volume — neither compressible nor dilatable — whose internal energy depends on TT alone:  ⁣dU=C  ⁣dT\dd U = C\,\dd T with C=mcC = mc, cc the specific heat capacity (4180 J/(kg K)4180\,\mathrm{J}/(\mathrm{kg}\,\mathrm{K}) for water, 450 J/(kg K)450\,\mathrm{J}/(\mathrm{kg}\,\mathrm{K}) for steel). The real, small deviations are measured by the thermal expansion coefficient α=(1/V)(∂V/∂T)P\alpha = (1/V)(\partial V/\partial T)_P (∼1×10−5 K−1\sim1 \times 10^{-5}\,\mathrm{K}^{-1} for metals, 2×10−4 K−12 \times 10^{-4}\,\mathrm{K}^{-1} for liquids) and the isothermal compressibility χT=−(1/V)(∂V/∂P)T\chi_T = -(1/V)(\partial V/\partial P)_T (∼5×10−10 Pa−1\sim5 \times 10^{-10}\,\mathrm{Pa}^{-1} for water, against 1/P≈1×10−5 Pa−11/P \approx 1 \times 10^{-5}\,\mathrm{Pa}^{-1} for a gas).

Proof. Admitted at this level. ∎

Example 20.14 (How incompressible)

Water at the bottom of the Mariana trench (1100 bar1100\,\mathrm{bar}) is compressed by χTΔP≈5×10−10×1.1×108=5%\chi_T\Delta P \approx 5\times10^{-10} \times 1.1\times10^8 = 5\%; a 30 m30\,\mathrm{m} steel rail warmed by 5050 K lengthens by αLΔT=18 mm\alpha L\Delta T = 18\,\mathrm{mm} — the reason for expansion joints. Against a gas, whose volume halves under a doubled pressure, the model of a fixed volume is good to a few percent in most situations of this volume.

20.5 Exercises

Exercise 20.1 ★

Number of molecules in 1.0 L1.0\,\mathrm{L} of gas at 0∘C0{}^{\circ}\mathrm{C} and 1 atm1\,\mathrm{atm}; mean distance between neighbors; compare with the molecular size 0.3 nm0.3\,\mathrm{nm}.

Solution

Solution of Exercise 20.1.

N=PV/kBT=1.013×105×10−3/(1.38×10−23×273)=2.7×1022N = PV/k_BT = 1.013\times10^5 \times 10^{-3}/(1.38\times10^{-23} \times 273) = 2.7 \times 10^{22}; n∗−1/3=(3.7×10−26)1/3=3.3 nmn^{*-1/3} = (3.7\times10^{-26})^{1/3} = 3.3\,\mathrm{nm}, ten times the molecular size.

Exercise 20.2 ★

Root-mean-square speeds of H2_2, N2_2, O2_2 and CO2_2 at 300 K300\,\mathrm{K}, and of N2_2 at 77 K77\,\mathrm{K} (boiling nitrogen).

Solution

Solution of Exercise 20.2.

u=3RT/Mu = \sqrt{3RT/M}: H2_2 1930 m/s1930\,\mathrm{m}/\mathrm{s}, N2_2 517 m/s517\,\mathrm{m}/\mathrm{s}, O2_2 484 m/s484\,\mathrm{m}/\mathrm{s}, CO2_2 412 m/s412\,\mathrm{m}/\mathrm{s}; N2_2 at 77 K77\,\mathrm{K}: 262 m/s262\,\mathrm{m}/\mathrm{s}.

Exercise 20.3 ★

A car tire of volume 30 L30\,\mathrm{L} is inflated to a gauge pressure of 2.5 bar2.5\,\mathrm{bar} at 20∘C20{}^{\circ}\mathrm{C}. Amount and mass of air inside; absolute pressure after a drive that heats it to 50∘C50{}^{\circ}\mathrm{C}.

Solution

Solution of Exercise 20.3.

P=3.5 barP = 3.5\,\mathrm{bar} absolute: n=PV/RT=3.5×105×0.030/(8.314×293)=4.3 moln = PV/RT = 3.5\times10^5 \times 0.030/(8.314 \times 293) = 4.3\,\mathrm{mol}, 125 g125\,\mathrm{g}. At 323 K323\,\mathrm{K}, P∝TP \propto T: 3.86 bar3.86\,\mathrm{bar} (gauge 2.85 bar2.85\,\mathrm{bar}).

Exercise 20.4 ★

Estimate the mean free path of air molecules at 1 bar1\,\mathrm{bar}, 300 K300\,\mathrm{K} (d=0.37 nmd = 0.37\,\mathrm{nm}), and the collision frequency of one molecule. At what pressure does the mean free path reach 1 m1\,\mathrm{m} (a “vacuum”)?

Solution

Solution of Exercise 20.4.

n∗=P/kBT=2.4×1025 m−3n^* = P/k_BT = 2.4 \times 10^{25}\,\mathrm{m}^{-3}; λ=1/(2π×1.37×10−19×2.4×1025)=6.8×10−8 m\lambda = 1/(\sqrt2\pi \times 1.37\times 10^{-19} \times 2.4\times10^{25}) = 6.8 \times 10^{-8}\,\mathrm{m}; frequency u/λ≈500/7×10−8=7×109 s−1u/\lambda \approx 500/7\times10^{-8} = 7 \times 10^{9}\,\mathrm{s}^{-1}. λ∝1/P\lambda \propto 1/P: 1 m1\,\mathrm{m} at P≈105×7×10−8=7×10−3 PaP \approx 10^5 \times 7\times10^{-8} = 7 \times 10^{-3}\,\mathrm{Pa}.

Exercise 20.5 ★★

Density of air at 1.013 bar1.013\,\mathrm{bar} and 20∘C20{}^{\circ}\mathrm{C} (M=29 g/molM = 29\,\mathrm{g}/\mathrm{mol}), then at 100∘C100{}^{\circ}\mathrm{C}. Lift of a 2800 m32800\,\mathrm{m}^{3} hot-air balloon (difference of the two weights of air).

Solution

Solution of Exercise 20.5.

ρ=PM/RT\rho = PM/RT: 1.20 kg/m31.20\,\mathrm{kg}/\mathrm{m}^{3} at 293 K293\,\mathrm{K}, 0.946 kg/m30.946\,\mathrm{kg}/\mathrm{m}^{3} at 373 K373\,\mathrm{K}. Lift (1.20−0.95)×2800×9.81=7.0 kN(1.20 - 0.95) \times 2800 \times 9.81 = 7.0\,\mathrm{kN}: about 720 kg720\,\mathrm{kg}.

Exercise 20.6 ★★

Air is 21%21\% O2_2 by molecules. Partial pressure of oxygen at sea level; at 5000 m5000\,\mathrm{m} where P=0.54 atmP = 0.54\,\mathrm{atm}; at the summit of Everest (0.33 atm0.33\,\mathrm{atm}). Why does the body struggle there?

Solution

Solution of Exercise 20.6.

PO2=0.21PP_{\mathrm{O}_2} = 0.21P: 0.21 atm0.21\,\mathrm{atm}; 0.11 atm0.11\,\mathrm{atm} at 5000 m5000\,\mathrm{m}; 0.07 atm0.07\,\mathrm{atm} on Everest — a third of sea level. Oxygen enters the blood in proportion to its partial pressure; at a third, the lungs cannot saturate the hemoglobin.

Exercise 20.7 ★★

One mole of CO2_2 at 300 K300\,\mathrm{K} in 1.0 L1.0\,\mathrm{L}: pressure from the perfect-gas law, then from van der Waals (a=0.364 Pa m6/mol2a = 0.364\,\mathrm{Pa}\,\mathrm{m}^{6}/\mathrm{mol}^{2}, b=4.27×10−5 m3/molb = 4.27 \times 10^{-5}\,\mathrm{m}^{3}/\mathrm{mol}). Which correction dominates here?

Solution

Solution of Exercise 20.7.

Perfect gas: P=RT/V=2494/10−3=24.9 barP = RT/V = 2494/10^{-3} = 24.9\,\mathrm{bar}. Van der Waals: RT/(V−b)−a/V2=2494/9.57×10−4−0.364/10−6=26.1−3.6=22.4 barRT/(V - b) - a/V^2 = 2494/9.57\times10^{-4} - 0.364/10^{-6} = 26.1 - 3.6 = 22.4\,\mathrm{bar}: the attraction (−3.6-3.6 bar) outweighs the excluded volume (+1.2+1.2 bar); real CO2_2 is 10%10\% below the ideal value.

Exercise 20.8 ★★

Internal energy of the air in a 50 m350\,\mathrm{m}^{3} room at 1 bar1\,\mathrm{bar}, 300 K300\,\mathrm{K}; energy to warm it by 5 K5\,\mathrm{K} at constant volume; time with a 2 kW2\,\mathrm{kW} heater (no losses).

Solution

Solution of Exercise 20.8.

n=PV/RT=105×50/(8.314×300)=2000 moln = PV/RT = 10^5 \times 50/(8.314 \times 300) = 2000\,\mathrm{mol}; U=52nRT=1.25×107 JU = \tfrac52 nRT = 1.25 \times 10^{7}\,\mathrm{J}; ΔU=52nR×5=208 kJ\Delta U = \tfrac52 nR \times 5 = 208\,\mathrm{kJ}; 104 s104\,\mathrm{s} at 2 kW2\,\mathrm{kW}.

Exercise 20.9 ★★

A 30 m30\,\mathrm{m} steel rail (α=1.2×10−5 K−1\alpha = 1.2 \times 10^{-5}\,\mathrm{K}^{-1}) between −10∘C-10{}^{\circ}\mathrm{C} and 40∘C40{}^{\circ}\mathrm{C}: length change. A brass ring (α=1.9×10−5 K−1\alpha = 1.9 \times 10^{-5}\,\mathrm{K}^{-1}) of inner diameter 49.95 mm49.95\,\mathrm{mm} must slip over a 50.00 mm50.00\,\mathrm{mm} shaft: by how much must it be heated?

Solution

Solution of Exercise 20.9.

ΔL=αLΔT=1.2×10−5×30×50=18 mm\Delta L = \alpha L\Delta T = 1.2\times10^{-5} \times 30 \times 50 = 18\,\mathrm{mm}. Ring: Δd/d=αΔT=0.05/49.95=10−3\Delta d/d = \alpha\Delta T = 0.05/49.95 = 10^{-3}: ΔT=10−3/1.9×10−5=53 K\Delta T = 10^{-3}/ 1.9\times10^{-5} = 53\,\mathrm{K} (the hole expands like the metal around it).

Exercise 20.10 ★★★

Energy per molecule at 300 K300\,\mathrm{K} (32kBT\tfrac32 k_BT) in joules and eV; molar heat capacities CV,mC_{V,m} of argon and of nitrogen; why is that of nitrogen larger though its molecules are lighter?

Solution

Solution of Exercise 20.10.

32kBT=6.2×10−21 J=0.039 eV\tfrac32 k_BT = 6.2 \times 10^{-21}\,\mathrm{J} = 0.039\,\mathrm{eV}. Argon 32R=12.5 J/(mol K)\tfrac32 R = 12.5\,\mathrm{J}/(\mathrm{mol}\,\mathrm{K}); nitrogen 52R=20.8 J/(mol K)\tfrac52 R = 20.8\,\mathrm{J}/(\mathrm{mol}\,\mathrm{K}): the diatomic molecule also stores energy in rotation (two extra degrees of freedom), whatever its mass.

Exercise 20.11 ★★★

Redo the derivation of the kinetic pressure in the six-direction model, then show that for an isotropic distribution of velocities ⟨vx2⟩=13⟨v2⟩\langle v_x^2\rangle = \tfrac13\langle v^2\rangle and that the pressure formula is unchanged.

Solution

Solution of Exercise 20.11.

Six-direction model: as in the text, P=13n∗mu2P = \tfrac13 n^*mu^2. Isotropy: ⟨vx2⟩=⟨vy2⟩=⟨vz2⟩\langle v_x^2\rangle = \langle v_y^2\rangle = \langle v_z^2\rangle and their sum is ⟨v2⟩\langle v^2\rangle, so each is 13⟨v2⟩\tfrac13\langle v^2\rangle. The flux argument with a distribution gives P=n∗m⟨vx2⟩P = n^*m\langle v_x^2\rangle (molecules with vx>0v_x > 0 hitting the wall, momentum 2mvx2mv_x each, flux n∗vx/2n^*v_x/2 per speed class, averaged), i.e. 13n∗m⟨v2⟩\tfrac13 n^*m\langle v^2\rangle — the same.

Exercise 20.12 ★★★

Root-mean-square speeds of H2_2 and O2_2 at 300 K300\,\mathrm{K} compared with the Earth’s escape velocity, and with the Moon’s (2.4 km/s2.4\,\mathrm{km}/\mathrm{s}). Knowing that the fraction of molecules faster than 3u3u is small but not zero, explain why the Earth has lost its hydrogen and the Moon its whole atmosphere.

Solution

Solution of Exercise 20.12.

H2_2: 1.9 km/s1.9\,\mathrm{km}/\mathrm{s}, O2_2: 0.48 km/s0.48\,\mathrm{km}/\mathrm{s}; Earth 11.2 km/s11.2\,\mathrm{km}/\mathrm{s}, Moon 2.4 km/s2.4\,\mathrm{km}/\mathrm{s}. For O2_2 on Earth, ve/u=23v_e/u = 23: the tail of the distribution beyond that is utterly negligible; for H2_2, ve/u≈6v_e/u \approx 6: a minute but steady fraction escapes each year, and over billions of years the hydrogen is gone. On the Moon, ve/uv_e/u is 55 for O2_2 and 1.21.2 for H2_2: everything leaked away.

20.6 Problem: The air in the room

Problem 20.1

Weekend problem — a classroom of air: counting its molecules, weighing it, timing their flights, and recovering from the same model the lift of a balloon, the thinness of mountain air and the speed of sound

A classroom measures 10×8×2.5 m10 \times 8 \times 2.5\,\mathrm{m}; its air is at P=1.013×105 PaP = 1.013 \times 10^{5}\,\mathrm{Pa}, T=293 KT = 293\,\mathrm{K}, molar mass M=29.0 g/molM = 29.0\,\mathrm{g}/\mathrm{mol}, 79%79\% N2_2 and 21%21\% O2_2 by molecules. R=8.314 J/(mol K)R = 8.314\,\mathrm{J}/(\mathrm{mol}\,\mathrm{K}), kB=1.38×10−23 J/Kk_B = 1.38 \times 10^{-23}\,\mathrm{J}/\mathrm{K}, NA=6.02×1023N_A = 6.02 \times 10^{23}, g=9.81 m/s2g = 9.81\,\mathrm{m}/\mathrm{s}^{2}.

Part I — Counting and weighing.

  1. Amount of air (moles) and number of molecules in the room.
  2. Mass of the air; compare with a person.
  3. Number density n∗n^* and mean distance between molecules (n∗−1/3n^{*-1/3}); compare with the molecular diameter 0.37 nm0.37\,\mathrm{nm}.
  4. Root-mean-square speed of N2_2 and of O2_2; why does the heavier gas move more slowly at the same temperature?
  5. Mean kinetic energy of one molecule; total translational kinetic energy of the room’s air; compare with the kinetic energy of a car at 100 km/h100\,\mathrm{km}/\mathrm{h}.
  6. Mean free path λ≈1/(2πd2n∗)\lambda \approx 1/(\sqrt2\pi d^2n^*) and the mean time between collisions of a molecule.

Part II — Pressure from impacts.

  1. Using the six-direction model with u=500 m/su = 500\,\mathrm{m}/\mathrm{s}, compute the number of impacts per second on 1 cm21\,\mathrm{cm}^{2} of wall.
  2. Compute the momentum delivered per second, and check that it reproduces the atmospheric pressure.
  3. Total force of the air on one wall of 8 m8\,\mathrm{m} by 2.5 m2.5\,\mathrm{m}; why does the wall not move?
  4. The room is warmed to 303 K303\,\mathrm{K} with its windows closed and sealed: new pressure, and the net force on the wall now.
  5. Same warming with a window open: what leaves, and how much?

Part III — Buoyancy.

  1. Density of the room’s air, and of air at 373 K373\,\mathrm{K} at the same pressure.
  2. A hot-air balloon of volume 2800 m32800\,\mathrm{m}^{3} is filled with air at 373 K373\,\mathrm{K}: weight of the hot air, weight of the displaced cold air, and the available lift (Archimedes, Chapter 21).
  3. The envelope, basket, burner and gas weigh 300 kg300\,\mathrm{kg}: how many 75 kg75\,\mathrm{kg} passengers can it lift?
  4. To what temperature should the air be heated to double the lift, and why is that not done (the envelope is nylon)?
  5. A helium balloon of the same volume at 293 K293\,\mathrm{K} (M=4 g/molM = 4\,\mathrm{g}/\mathrm{mol}): lift? Why do tourist balloons use hot air nonetheless?

Part IV — Thin air and the speed of sound.

  1. Partial pressure of oxygen in the room.
  2. At the summit of Everest P=0.33 atmP = 0.33\,\mathrm{atm} and T≈250 KT \approx 250\,\mathrm{K}: number density of oxygen molecules compared with the room’s.
  3. The atmosphere’s pressure falls with height roughly as P(z)=P0e−z/HP(z) = P_0\eu^{-z/H} with H=RT/MgH = RT/Mg (Chapter 21): compute HH for 260 K260\,\mathrm{K} and the height at which P=P0/2P = P_0/2.
  4. The speed of sound in a perfect gas is cs=γRT/Mc_s = \sqrt{\gamma RT/M} with γ=1.4\gamma = 1.4 for air (Chapter 22): compute it at 293 K293\,\mathrm{K} and compare with the rms speed; interpret the closeness.
  5. How does csc_s vary with TT? Speed of sound in the room at 303 K303\,\mathrm{K}, and in helium at 293 K293\,\mathrm{K} (γ=5/3\gamma = 5/3): why does a helium voice sound high?
  6. At the top of Everest, is sound faster or slower than in the room? By how much?
  7. The room’s air is replaced by argon at the same PP and TT: what changes in the count, the mass, the speeds, the internal energy?
  8. Internal energy of the room’s air (U=52nRTU = \tfrac52 nRT) and the energy to warm it by 10 K10\,\mathrm{K} at constant volume.
  9. Summarize in three lines what the kinetic model delivered: which macroscopic quantities it explained, and from which single microscopic average.
Solution

Solution of Problem 20.1.

1. V=200 m3V = 200\,\mathrm{m}^{3}: n=PV/RT=1.013×105×200/(8.314×293)=8320 moln = PV/RT = 1.013\times10^5 \times 200/(8.314 \times 293) = 8320\,\mathrm{mol}; N=nNA=5.0×1027N = nN_A = 5.0 \times 10^{27}.

2. m=nM=241 kgm = nM = 241\,\mathrm{kg}: three people.

3. n∗=N/V=2.5×1025 m−3n^* = N/V = 2.5 \times 10^{25}\,\mathrm{m}^{-3}; distance n∗−1/3=3.4 nmn^{*-1/3} = 3.4\,\mathrm{nm}, nine molecular diameters.

4. N2_2: 3×8.314×293/0.028=511 m/s\sqrt{3 \times 8.314 \times 293/0.028} = 511\,\mathrm{m}/\mathrm{s}; O2_2: 478 m/s478\,\mathrm{m}/\mathrm{s}. Same 32kBT\tfrac32 k_BT per molecule: 12mu2\tfrac12 mu^2 fixed, so u∝1/mu \propto 1/\sqrt m.

5. 32kBT=6.1×10−21 J\tfrac32 k_BT = 6.1 \times 10^{-21}\,\mathrm{J}; total N×6.1×10−21=3.0×107 JN \times 6.1\times10^{-21} = 3.0 \times 10^{7}\,\mathrm{J}; a 1000 kg1000\,\mathrm{kg} car at 100 km/h100\,\mathrm{km}/\mathrm{h}: 3.9×105 J3.9 \times 10^{5}\,\mathrm{J} — the room’s molecular motion is eighty cars’ worth.

6. λ=1/(2π×1.37×10−19×2.5×1025)=66 nm\lambda = 1/(\sqrt2\pi \times 1.37\times10^{-19} \times 2.5\times10^{25}) = 66\,\mathrm{nm}; time λ/u=66×10−9/500=1.3×10−10 s\lambda/u = 66\times10^{-9}/500 = 1.3 \times 10^{-10}\,\mathrm{s}.

7. Impacts per second on SS: 16n∗Su=16×2.5×1025×10−4×500=2.1×1023 s−1\tfrac16 n^*Su = \tfrac16 \times 2.5\times 10^{25} \times 10^{-4} \times 500 = 2.1 \times 10^{23}\,\mathrm{s}^{-1}.

8. Each gives 2mu=2×4.8×10−26×500=4.8×10−23 kg m/s2mu = 2 \times 4.8\times10^{-26} \times 500 = 4.8 \times 10^{-23}\,\mathrm{kg}\,\mathrm{m}/\mathrm{s} (m=M/NA=4.8×10−26 kgm = M/N_A = 4.8 \times 10^{-26}\,\mathrm{kg}): force 2.1×1023×4.8×10−23=10 N2.1\times10^{23} \times 4.8\times10^{-23} = 10\,\mathrm{N} on 1 cm21\,\mathrm{cm}^{2}: 1.0×105 Pa1.0 \times 10^{5}\,\mathrm{Pa}. The model reproduces atmospheric pressure.

9. F=PS=1.013×105×20=2.0×106 NF = PS = 1.013\times10^5 \times 20 = 2.0 \times 10^{6}\,\mathrm{N} — two hundred tonnes; the same pressure acts on the other side.

10. P′=P×303/293=1.048×105 PaP' = P \times 303/293 = 1.048 \times 10^{5}\,\mathrm{Pa}; net ΔP S=3.5×103×20=70 kN\Delta P\,S = 3.5 \times10^3 \times 20 = 70\,\mathrm{kN} outward: seven tonnes on the wall.

11. Air flows out until the pressure equalizes: n∝1/Tn \propto 1/T at fixed PP, VV: 8320×(1−293/303)=275 mol8320 \times (1 - 293/303) = 275\,\mathrm{mol}, 8 kg8\,\mathrm{kg} leave.

12. ρ=PM/RT\rho = PM/RT: 1.205 kg/m31.205\,\mathrm{kg}/\mathrm{m}^{3} at 293 K293\,\mathrm{K}; 0.946 kg/m30.946\,\mathrm{kg}/\mathrm{m}^{3} at 373 K373\,\mathrm{K}.

13. Hot air 0.946×2800×9.81=26.0 kN0.946 \times 2800 \times 9.81 = 26.0\,\mathrm{kN}; displaced cold air 1.205×2800×9.81=33.1 kN1.205 \times 2800 \times 9.81 = 33.1\,\mathrm{kN}; lift 7.1 kN7.1\,\mathrm{kN} (725 kg725\,\mathrm{kg}).

14. 725−300=425 kg725 - 300 = 425\,\mathrm{kg}: five passengers.

15. Lift ∝ρc−ρh=ρc(1−293/T)\propto \rho_c - \rho_h = \rho_c(1 - 293/T): doubling 1−293/373=0.2151 - 293/373 = 0.215 needs T=293/0.57=514 KT = 293/0.57 = 514\,\mathrm{K} (240∘C240{}^{\circ}\mathrm{C}), well above what nylon tolerates (about 120∘C120{}^{\circ}\mathrm{C}).

16. Helium ρ=1.205×4/29=0.166 kg/m3\rho = 1.205 \times 4/29 = 0.166\,\mathrm{kg}/\mathrm{m}^{3}: lift (1.205−0.166)×2800×9.81=28.5 kN(1.205 - 0.166) \times 2800 \times 9.81 = 28.5\,\mathrm{kN} (2.9 t2.9\,\mathrm{t}), four times more — but helium is expensive and lost at every landing, while hot air is free and its lift can be adjusted with the burner.

17. 0.21×1.013×105=2.1×104 Pa0.21 \times 1.013\times10^5 = 2.1 \times 10^{4}\,\mathrm{Pa}.

18. nO2∗=PO2/kBTn^*_{\mathrm{O}_2} = P_{\mathrm{O}_2}/k_BT: room 2.1×104/(1.38×10−23×293)=5.3×1024 m−32.1\times10^4/ (1.38\times10^{-23} \times 293) = 5.3 \times 10^{24}\,\mathrm{m}^{-3}; Everest 0.21×0.33×1.013×105/(1.38×10−23×250)=2.0×1024 m−30.21 \times 0.33 \times 1.013\times10^5/(1.38\times10^{-23} \times 250) = 2.0 \times 10^{24}\,\mathrm{m}^{-3}: 38%38\% of the room’s.

19. H=RT/Mg=8.314×260/(0.029×9.81)=7.6 kmH = RT/Mg = 8.314 \times 260/(0.029 \times 9.81) = 7.6\,\mathrm{km}; P0/2P_0/2 at Hln⁡2=5.3 kmH\ln 2 = 5.3\,\mathrm{km}.

20. cs=1.4×8.314×293/0.029=343 m/sc_s = \sqrt{1.4 \times 8.314 \times 293/0.029} = 343\,\mathrm{m}/\mathrm{s}, against u=503 m/su = 503\,\mathrm{m}/\mathrm{s} for the mixture: cs/u=γ/3=0.68c_s/u = \sqrt{\gamma/3} = 0.68. Sound is a disturbance carried by the molecules themselves, so it travels at a speed of the order of theirs — a little less, since only the component along the propagation matters.

21. cs∝Tc_s \propto \sqrt T: 343303/293=349 m/s343\sqrt{303/293} = 349\,\mathrm{m}/\mathrm{s}. Helium: (5/3)×8.314×293/0.004=1010 m/s\sqrt{(5/3) \times 8.314 \times 293/0.004} = 1010\,\mathrm{m}/\mathrm{s}: the resonances of the vocal tract scale with csc_s, so every formant is three times higher.

22. Colder: 343250/293=317 m/s343\sqrt{250/293} = 317\,\mathrm{m}/\mathrm{s}, 8%8\% slower; the pressure does not enter.

23. Same NN (same PP, VV, TT); mass ×40/29=333 kg\times 40/29 = 333\,\mathrm{kg}; speeds ×29/40\times\sqrt{29/40}: u=428 m/su = 428\,\mathrm{m}/\mathrm{s}; U=32nRTU = \tfrac32 nRT instead of 52\tfrac52: 60%60\%.

24. U=52×8320×8.314×293=5.1×107 JU = \tfrac52 \times 8320 \times 8.314 \times 293 = 5.1 \times 10^{7}\,\mathrm{J}; ΔU=52nR×10=1.7×106 J\Delta U = \tfrac52 nR \times 10 = 1.7 \times 10^{6}\,\mathrm{J}.

25. One average, ⟨v2⟩\langle v^2\rangle, fixes the pressure (13n∗m⟨v2⟩\tfrac13 n^*m\langle v^2\rangle), defines the temperature (12m⟨v2⟩=32kBT\tfrac12 m\langle v^2\rangle = \tfrac32 k_BT), gives the equation of state and the internal energy, and sets the scale of the speed of sound.

Terms defined in this chapter

See all 431 terms in the glossary