The Kinetic Theory of Gases
How the unseen storm of molecules — each faster than a bullet, colliding billions of times a second — adds up to the pressure, temperature, and warmth of an ordinary breath of air
- How to count atoms by the mole using Avogadro's number \(N_{A} = 6.02 \times 10^{23}\,\mathrm{mol^{-1}}\), and the ideal gas law in its two forms \(pV = nRT = NkT\).
- The work an ideal gas does — isothermal \(W = nRT\ln(V_{f}/V_{i})\), constant-pressure \(W = p\,\Delta V\), constant-volume \(W = 0\).
- That pressure springs from molecular motion, \(p = nMv_{\text{rms}}^{2}/3V\), giving the rms speed \(v_{\text{rms}} = \sqrt{3RT/M}\).
- That temperature is average translational kinetic energy: \(K_{\text{avg}} = \tfrac{3}{2}kT\).
- The mean free path \(\lambda = 1/(\sqrt{2}\,\pi d^{2}\,N/V)\) and the Maxwell speed distribution with its three speeds \(v_{P} < v_{\text{avg}} < v_{\text{rms}}\).
- The molar specific heats \(C_{V} = \tfrac{f}{2}R\), \(C_{p} = C_{V} + R\), the role of degrees of freedom, and the adiabatic law \(pV^{\gamma} = \text{const}\).
What Is Physics?
A gas is a swarm of atoms or molecules that fill their container and press on its walls. Three everyday quantities describe it — volume, pressure, and temperature — and all three trace back to the same hidden cause: the motion of the molecules. The volume reflects their freedom to roam, the pressure their relentless drumming on the walls, and the temperature their kinetic energy. The kinetic theory of gases is the bridge that connects this unseen molecular motion to the measurable, large-scale behavior of the gas.
Its applications are everywhere: the combustion of vaporized fuel in an engine, the fermentation gas that lifts a loaf of bread, the cork launched from a champagne bottle, the nitrogen a diver must let bleed slowly from the blood to avoid the bends, and the heat traded between ocean and air that shapes weather. Our first step is simply to count: how much gas is in a sample? For that, we use Avogadro's number.
Avogadro's Number
When we think about atoms, it is natural to measure samples in moles, so that equal counts of molecules are being compared. One mole is the number of atoms in a 12 g sample of carbon-12, and that number — determined experimentally — is Avogadro's number:
Ideal Gases
We want to explain a gas's large-scale behavior from its molecules — but which gas? Hydrogen, oxygen, methane, and uranium hexafluoride are all different. Yet experiment reveals something wonderful: confine one mole of any gas in a fixed volume at a fixed temperature and the measured pressures are nearly the same, and the small differences vanish as the density drops. At low enough density, every real gas obeys one law:
Here \(p\) is absolute pressure, \(T\) is in kelvins, \(R = 8.31\,\mathrm{J/mol\cdot K}\) is the gas constant, and \(k = R/N_{A} = 1.38 \times 10^{-23}\,\mathrm{J/K}\) is the Boltzmann constant. The first form counts moles (\(n\)); the second counts molecules (\(N\)). An "ideal" gas is the limit in which molecules are so far apart that they ignore one another — and all real gases approach it at low density.
Work Done by an Ideal Gas
Put an ideal gas in a piston-cylinder and let it expand at constant temperature — an isothermal process, traced on a p–V diagram by a curve called an isotherm. Starting from the general \(W = \int p\,dV\) and substituting \(p = nRT/V\), the constant \(T\) comes out of the integral:
Pressure, Temperature, and RMS Speed
Now the first true kinetic-theory result. Picture \(n\) moles in a cubical box, molecules ricocheting off the walls like balls in a court. Each elastic bounce off a wall reverses one velocity component and delivers momentum \(2mv_{x}\); the molecule returns every \(2L/v_{x}\) seconds. Sum the resulting force over all molecules, divide by the wall area, and the macroscopic pressure emerges from microscopic speeds:
| Gas | M (10⁻³ kg/mol) | vrms (m/s) |
|---|---|---|
| Hydrogen (H₂) | 2.02 | 1920 |
| Helium (He) | 4.0 | 1370 |
| Water vapor (H₂O) | 18.0 | 645 |
| Nitrogen (N₂) | 28.0 | 517 |
| Oxygen (O₂) | 32.0 | 483 |
| Carbon dioxide (CO₂) | 44.0 | 412 |
Translational Kinetic Energy
Follow a single molecule as collisions keep changing its speed. Its average translational kinetic energy is \(K_{\text{avg}} = \tfrac{1}{2}mv_{\text{rms}}^{2}\). Substitute \(v_{\text{rms}} = \sqrt{3RT/M}\), recognize that \(M/m = N_{A}\), and the molar mass and molecular mass cancel beautifully to leave something universal:
At a given temperature, every ideal-gas molecule has the same average translational kinetic energy — regardless of its mass. A heavy molecule simply moves more slowly to compensate. So when you measure a gas's temperature, you are really measuring the average translational kinetic energy of its molecules. This is the deep meaning of temperature.
Mean Free Path
A molecule does not fly straight across the room; it zigzags, colliding constantly. The mean free path \(\lambda\) is the average distance it travels between collisions. It should shrink when the gas is crowded (large \(N/V\)) and when molecules are fat (large diameter \(d\)) — and because what matters is a molecule's cross-sectional target area, it falls off as \(d^{2}\):
The Distribution of Molecular Speeds
The rms speed is a single summary, but molecules actually carry a whole spread of speeds. In 1852 James Clerk Maxwell found the distribution. The function \(P(v)\) is a probability density: \(P(v)\,dv\) is the fraction of molecules with speeds in a band \(dv\) around \(v\), and the total area under the curve is 1.
The Molar Specific Heats of an Ideal Gas
For a monatomic ideal gas, the internal energy is just the translational kinetic energy of its atoms, \(E_{\text{int}} = \tfrac{3}{2}nRT\) — a function of temperature alone. From this we derive two molar specific heats: \(C_{V}\) (heat per mole per degree at constant volume) and \(C_{p}\) (at constant pressure).
| Molecule | Ideal prediction | Real example |
|---|---|---|
| Monatomic | \(\tfrac{3}{2}R = 12.5\) | He 12.5 · Ar 12.6 |
| Diatomic | \(\tfrac{5}{2}R = 20.8\) | N₂ 20.7 · O₂ 20.8 |
| Polyatomic | \(3R = 24.9\) | CO₂ 29.7 |
Degrees of Freedom and Molar Specific Heats
The prediction \(C_{V} = \tfrac{3}{2}R\) nails monatomic gases but falls short for diatomic and polyatomic ones — because those molecules can also store energy in rotation (and, at high temperatures, vibration). Maxwell's equipartition theorem explains it: every independent way a molecule can store energy — every degree of freedom — holds, on average, \(\tfrac{1}{2}kT\) per molecule (\(\tfrac{1}{2}RT\) per mole).
A monatomic atom has only 3 translational degrees (\(f = 3\)). A diatomic molecule adds 2 rotational degrees (\(f = 5\)) — it cannot rotate about its own long axis. Polyatomic molecules get all 3 rotational degrees (\(f = 6\)). Each extra storage channel raises \(C_V\), matching experiment.
The Adiabatic Expansion of an Ideal Gas
In an adiabatic process no heat crosses the boundary (\(Q = 0\)) — achieved either by good insulation or by acting so fast there is no time for heat flow, as in a sound wave. Starting from the first law with \(dE_{\text{int}} = nC_{V}\,dT\) and integrating, one finds the gas tracks a steeper curve than an isotherm:
Putting It to Work
Problem. A cylinder holds 12 L of oxygen at 20 °C and 15 atm. The temperature is raised to 35 °C and the volume reduced to 8.5 L. Find the final pressure (assume ideal).
Solution. Write \(pV = nRT\) for both states and divide; with \(n\) and \(R\) cancelling, only the temperatures need converting to kelvins (293 K and 308 K).
Volume and pressure units cancel in the ratio, so liters and atmospheres are fine — but temperature must be absolute, because the conversion to kelvins adds a constant that does not cancel.
Problem. One mole of oxygen (ideal) expands isothermally at \(T = 310\,\mathrm{K}\) from 12 L to 19 L. How much work does the gas do?
Solution. Constant temperature means \(W = nRT\ln(V_{f}/V_{i})\).
Positive, as it must be for an expansion. Reverse the process — compress 19 L back to 12 L — and the gas does −1180 J, meaning an external agent must do 1180 J on it.
Problem. Find the rms speed of oxygen molecules (\(M = 0.0320\,\mathrm{kg/mol}\)) at 300 K.
Solution. Apply \(v_{\text{rms}} = \sqrt{3RT/M}\) directly.
For comparison, the same gas has \(v_{\text{avg}} \approx 445\,\mathrm{m/s}\) and \(v_{P} \approx 395\,\mathrm{m/s}\) — neatly confirming the ordering \(v_{P} < v_{\text{avg}} < v_{\text{rms}}\).
Problem. For oxygen at 300 K and 1.0 atm (\(d = 290\,\mathrm{pm}\)), find (a) the mean free path and (b) the collision frequency if the average speed is 450 m/s.
Solution. Use \(N/V = p/kT\) from the ideal gas law, substitute into \(\lambda = 1/(\sqrt{2}\,\pi d^{2}\,N/V)\), then \(f = v/\lambda\).
The path is about 380 molecular diameters — and the molecule suffers roughly 4 billion collisions every second, with under a nanosecond of free flight between them. That is why perfume diffuses so slowly despite its speed.
Problem. A bubble of 5.00 mol of helium (monatomic, ideal) is warmed by \(\Delta T = 20.0\,\mathrm{C^{\circ}}\) at constant pressure. Find (a) the heat \(Q\), (b) the internal-energy change, and (c) the work done.
Solution. Constant pressure uses \(Q = nC_{p}\Delta T\) with \(C_{p} = \tfrac{5}{2}R\); internal energy uses \(\Delta E_{\text{int}} = nC_{V}\Delta T\) with \(C_{V} = \tfrac{3}{2}R\); work follows from the first law.
Of the ~2080 J supplied, about 1250 J raises the internal energy (here, pure translational kinetic energy) and ~831 J becomes the work of expansion. The work can also be gotten directly as \(W = nR\,\Delta T\) — the same 831 J.
Problem. One mole of oxygen (diatomic, \(\gamma = 1.40\)) at 310 K and 12 L expands to 19 L. Find the final temperature if the expansion is (a) adiabatic, and (b) a free expansion (from \(p_{i} = 2.0\,\mathrm{Pa}\)).
Solution. Adiabatic uses \(T_{i}V_{i}^{\gamma-1} = T_{f}V_{f}^{\gamma-1}\); a free expansion changes nothing about the molecules' kinetic energy, so \(T_{f} = T_{i}\).
The adiabatic expansion cools the gas by 52 K because it does work at no heat cost; the free expansion leaves the temperature untouched because the gas does no work and exchanges no heat.
Chapter Summary
\(N_{A} = 6.02\times10^{23}\,\mathrm{mol^{-1}}\), \(n = N/N_{A} = M_{\text{sam}}/M\), \(M = mN_{A}\).
\(pV = nRT = NkT\), with \(R = 8.31\,\mathrm{J/mol\cdot K}\), \(k = 1.38\times10^{-23}\,\mathrm{J/K}\).
Isothermal \(W = nRT\ln(V_{f}/V_{i})\); const-p \(W = p\Delta V\); const-V \(W = 0\).
\(p = nMv_{\text{rms}}^{2}/3V\), \(v_{\text{rms}} = \sqrt{3RT/M}\).
\(K_{\text{avg}} = \tfrac{3}{2}kT\) — temperature is average translational KE.
\(\lambda = 1/(\sqrt{2}\,\pi d^{2}\,N/V)\) — shrinks with crowding and molecular size.
Maxwell's \(P(v)\); \(v_{P} < v_{\text{avg}} < v_{\text{rms}}\).
\(C_{V} = \tfrac{f}{2}R\), \(C_{p} = C_{V} + R\), \(\Delta E_{\text{int}} = nC_{V}\Delta T\).
\(pV^{\gamma} = \text{const}\), \(TV^{\gamma-1} = \text{const}\), \(\gamma = C_{p}/C_{V}\).
Problems
Take \(R = 8.31\,\mathrm{J/mol\cdot K}\), \(N_{A} = 6.02\times10^{23}\,\mathrm{mol^{-1}}\), and \(1\,\mathrm{atm} = 1.01\times10^{5}\,\mathrm{Pa}\). Always convert temperatures to kelvins. For specific-heat problems, decide first whether the gas is monatomic (\(f=3\)) or diatomic (\(f=5\)), and remember \(\Delta E_{\text{int}} = nC_{V}\Delta T\) holds for every path.
- Gold has a molar mass of 197 g/mol. In a 2.50 g sample, find (a) the number of moles and (b) the number of atoms.
- A quantity of ideal gas at 10.0 °C and 100 kPa occupies 2.50 m³. (a) How many moles are present? (b) If the pressure is raised to 300 kPa and the temperature to 30.0 °C, what volume does it occupy?
- An automobile tire has a volume of \(1.64\times10^{-2}\,\mathrm{m^{3}}\) and holds air at a gauge pressure of 165 kPa at 0.00 °C. Find the gauge pressure when the temperature rises to 27.0 °C and the volume grows to \(1.67\times10^{-2}\,\mathrm{m^{3}}\). (Atmospheric pressure 101 kPa.)
- Suppose 1.80 mol of an ideal gas is compressed isothermally at 30 °C from 3.00 m³ to 1.50 m³. (a) How much energy is transferred as heat, and (b) is it to or from the gas?
- Compute the rms speed of a nitrogen molecule (N₂, \(M = 28.0\,\mathrm{g/mol}\)) at 20.0 °C. At what temperatures is the rms speed (b) half and (c) twice that value?
- Determine the average translational kinetic energy of an ideal-gas molecule at (a) 0.00 °C and (b) 100 °C, and (c) the kinetic energy per mole at 0.00 °C.
- The mean free path of nitrogen at 0.0 °C and 1.0 atm is \(0.80\times10^{-5}\,\mathrm{cm}\), with \(2.7\times10^{19}\) molecules/cm³. What is the molecular diameter?
- The speeds of ten molecules are 2.0, 3.0, 4.0, …, 11 km/s. Find their (a) average speed and (b) rms speed.
- What is the internal energy of 1.0 mol of an ideal monatomic gas at 273 K?
- The temperature of 3.00 mol of an ideal diatomic gas (rotation, no oscillation) rises 40.0 C° at constant pressure. Find (a) the heat added, (b) the change in internal energy, (c) the work done, and (d) the increase in rotational kinetic energy.
- Under constant pressure, the temperature of 2.00 mol of an ideal monatomic gas is raised 15.0 K. Find (a) the work \(W\), (b) the heat \(Q\), and (c) the change \(\Delta E_{\text{int}}\).
- We give 70 J as heat to a diatomic gas (rotation, no oscillation), which expands at constant pressure. By how much does its internal energy increase?
- A certain gas occupies 4.3 L at 1.2 atm and 310 K, then is compressed adiabatically to 0.76 L (\(\gamma = 1.4\)). Find (a) the final pressure and (b) the final temperature.
- An ideal monatomic gas at 330 K and 6.00 atm expands from 500 cm³ to 1500 cm³. If isothermal, find (a) the final pressure and (b) the work done; if adiabatic, find (c) the final pressure and (d) the work done.