This page is the drill floor for the parent derivations . The formulas are already built there; here we hit every kind of question an exam or the real world can throw. First we lay out the full map of cases, then work each one.
If a symbol here feels unfamiliar, it was defined in the parent note — but we re-state each one the moment it appears, so you never have to flip back.
Think of every possible question as a cell in this grid. Our goal: no empty cells . Each worked example below is tagged with the cell it fills.
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Cell class
What makes it tricky
Example
A
Direct plug — v r m s
SI unit trap (M in kg/mol)
Ex 1
B
Direct plug — v ˉ and v p
three speeds, one gas
Ex 2
C
Ratio / scaling (T changes)
speeds ∝ T
Ex 3
D
Ratio / scaling (different gas, same T)
speeds ∝ 1/ M
Ex 4
E
Mean free path — direct
n = P / k B T form, the 2
Ex 5
F
Limiting / degenerate (P → 0 , T → 0 )
what blows up, what vanishes
Ex 6
G
Collision frequency (combine v ˉ and λ )
rate = v ˉ / λ
Ex 7
H
Real-world word problem
vacuum chamber design
Ex 8
I
Exam-style twist (reverse: find T or d )
invert the formula
Ex 9
Constants used throughout (memorise these):
R = 8.314 J mol − 1 K − 1 (gas constant)
k B = 1.38 × 1 0 − 23 J K − 1 (Boltzmann constant, = R / N A )
N A = 6.022 × 1 0 23 mol − 1
Ex 1. Find v r m s of oxygen (O 2 ) at T = 300 K . Molar mass M = 32 g/mol .
Forecast: guess before computing — will it be tens, hundreds, or thousands of m/s? (Room-temperature gas molecules are hundreds of m/s.)
Convert M to SI. M = 32 g/mol = 0.032 kg/mol .
Why this step? The formula v r m s = 3 R T / M uses R in joules, which are kg m 2 s − 2 . If you leave M in grams you divide by a number 1000× too small, so the speed comes out 1000 ≈ 32 × too big. This is the single most common exam error.
Plug in.
v r m s = M 3 R T = 0.032 3 ( 8.314 ) ( 300 ) = 2.338 × 1 0 5
Why this step? v r m s is the "energy-carrying" speed because kinetic energy ∝ v 2 ; it comes straight from 2 1 m v 2 = 2 3 k B T .
Root it. v r m s ≈ 483 m/s .
Verify: Units — J/(kg/mol) = ( kg m 2 s − 2 / mol ) / ( kg/mol ) = m 2 s − 2 = m/s . ✓ Hundreds of m/s, as forecast, and lighter than… well, we'll compare in Ex 4.
Ex 2. For the same O 2 at 300 K , also find the mean speed v ˉ and most probable speed v p .
Forecast: the parent note gives the ordering v p < v ˉ < v r m s . So both new numbers should sit below 483 m/s , with v p lowest.
Mean speed — the ordinary arithmetic average of speed, which controls how often things happen (collisions, effusion):
v ˉ = π M 8 R T = π ( 0.032 ) 8 ( 8.314 ) ( 300 ) ≈ 445 m/s
Why this step? The extra 8/ π instead of 3 comes from integrating v f ( v ) rather than v 2 f ( v ) over the Maxwell-Boltzmann distribution .
Most probable speed — where the distribution f ( v ) peaks, the single most common speed:
v p = M 2 R T = 0.032 2 ( 8.314 ) ( 300 ) ≈ 395 m/s
Why this step? Setting df / d v = 0 gives the factor 2 under the root.
Verify: Ratios should be v p : v ˉ : v r m s = 2 : 8/ π : 3 ≈ 1.414 : 1.596 : 1.732 .
Check: 445/395 = 1.127 and 8/ π / 2 = 1.128 . ✓ Ordering 395 < 445 < 483 holds, as forecast.
Ex 3. The v r m s of a gas is 500 m/s at 300 K . What is it at 1200 K ?
Forecast: temperature is × 4 . Speed goes as T , and 4 = 2 — so guess 1000 m/s .
Write the ratio, cancel constants.
v 1 v 2 = 3 R T 1 / M 3 R T 2 / M = T 1 T 2
Why this step? Because M , R , and the 3 are identical for the same gas, the only thing that survives the division is the temperature ratio. Never re-plug the whole formula when you can take a ratio — fewer chances to slip a unit.
Insert temperatures (in kelvin — always kelvin for these ratios).
v 2 = 500 300 1200 = 500 4 = 1000 m/s
Verify: 4 = 2 , so 500 → 1000 . ✓ Matches forecast. Note: if the problem gave T in °C you would have to add 273 first — a favourite trap.
Ex 4. At the same temperature, compare v r m s of helium (M = 4 g/mol ) and oxygen (M = 32 g/mol ).
Forecast: helium is 8× lighter. Speed goes as 1/ M , and 8 ≈ 2.83 — so helium should be about 2.8× faster.
Ratio at fixed T .
v O 2 v He = M He M O 2 = 4 32 = 8 ≈ 2.83
Why this step? At the same T every molecule has the same average kinetic energy 2 3 k B T (this is the Equipartition theorem ). Same energy 2 1 m v 2 with smaller mass means bigger speed — lighter gas flies faster.
Use Ex 1's oxygen value v O 2 = 483 m/s at 300 K :
v He = 2.83 × 483 ≈ 1367 m/s
Verify: Direct plug: 3 ( 8.314 ) ( 300 ) /0.004 = 1.871 × 1 0 6 ≈ 1368 m/s . ✓ (rounding). This is why helium leaks and escapes Earth's gravity faster than heavier gases — link to Diffusion and effusion .
Ex 5. Find the mean free path λ of nitrogen at STP: T = 273 K , P = 1.01 × 1 0 5 Pa , molecular diameter d = 3.7 × 1 0 − 10 m .
Forecast: the parent note quoted ~68 nm for air — nitrogen is basically air, so expect the same ballpark.
Use the pressure form directly.
λ = 2 π d 2 P k B T
Why this step? Substituting number density n = P / k B T (from the Ideal gas law ) lets us skip computing n as a separate messy number.
Plug the numbers.
λ = 2 π ( 3.7 × 1 0 − 10 ) 2 ( 1.01 × 1 0 5 ) ( 1.38 × 1 0 − 23 ) ( 273 )
Numerator = 3.767 × 1 0 − 21 . Denominator = 2 π ( 1.369 × 1 0 − 19 ) ( 1.01 × 1 0 5 ) = 6.14 × 1 0 − 14 .
λ ≈ 6.1 × 1 0 − 8 m = 61 nm
Why the 2 ? Targets are moving too. The average relative speed between two molecules is 2 v ˉ , which raises the collision rate by 2 and shortens the flight by 2 .
Verify: Units — m 2 ⋅ Pa J = m 2 ⋅ N/m 2 J = N J = m . ✓ 61 nm ≈ 165× the molecular diameter — gas is mostly empty space. ✓ (Matches parent's ~68 nm for the slightly different d of air.)
Ex 6. What happens to v r m s and λ in these extreme limits? (a) T → 0 ; (b) P → 0 (perfect vacuum) at fixed T ; (c) P → ∞ .
Forecast: cold gas freezes → speeds die. Empty space → nothing to hit → flights get huge. Crush the gas → nowhere to fly.
(a) T → 0 . v r m s = 3 R T / M → 0 = 0 .
Why? All three speeds share the T factor, so v p , v ˉ , v r m s → 0 together. Zero thermal energy means (classically) no motion. Meanwhile λ = 2 π d 2 P k B T → 0 if P is held fixed — but real gas would liquefy first, so this is an idealised limit.
(b) P → 0 at fixed T . λ = 2 π d 2 P k B T → ∞ .
Why? Fewer molecules per volume (n = P / k B T → 0 ) means almost nothing to collide with — a molecule can cross the whole chamber uninterrupted. This is exactly the "molecular flow" regime used in vacuum technology (Ex 8). Note v r m s is unchanged — it depends only on T , not on P .
(c) P → ∞ . λ → 0 .
Why? Squeeze infinitely → infinite crowding → zero flight between hits.
Verify: Limits are consistent with λ ∝ 1/ P and v r m s ∝ T (independent of P ). Sanity: doubling P halves λ but leaves v r m s alone. ✓
Ex 7. How many collisions per second does one nitrogen molecule make at STP? Use v ˉ = 445 m/s (from Ex 2-style, close enough for N 2 ) and λ = 6.1 × 1 0 − 8 m (Ex 5).
Forecast: it flies 445 m each second and each flight is only ~61 nm long — so the number of flights (collisions) will be enormous , billions per second.
Collision frequency = distance travelled per second ÷ distance per flight.
Z = λ v ˉ = 6.1 × 1 0 − 8 445
Why this step? In one second a molecule covers v ˉ metres; each collision ends a flight of length λ , so the count is simply their ratio. We use v ˉ (not v r m s ) because collision rate is governed by the ordinary average speed.
Compute. Z ≈ 7.3 × 1 0 9 s − 1 .
Verify: 7.3 × 1 0 9 collisions per second — about 7 billion. ✓ Enormous, as forecast. Time between collisions ≈ 1/ Z ≈ 1.4 × 1 0 − 10 s . Units: m m/s = s − 1 . ✓
Ex 8. A vacuum chamber is 0.5 m across. Engineers want the mean free path to exceed the chamber size (so molecules hit walls, not each other — "molecular flow"). At T = 300 K , d = 3.7 × 1 0 − 10 m , what pressure is needed?
Forecast: normal air has λ ∼ 60 nm. We need λ ≥ 0.5 m — about 1 0 7 × bigger. Since λ ∝ 1/ P , we need pressure about 1 0 7 × smaller than atmospheric, i.e. deep vacuum.
Set the condition λ = 0.5 m and solve for P .
λ = 2 π d 2 P k B T ⇒ P = 2 π d 2 λ k B T
Why this step? We invert the mean-free-path formula because the unknown is now P , not λ .
Plug in.
P = 2 π ( 3.7 × 1 0 − 10 ) 2 ( 0.5 ) ( 1.38 × 1 0 − 23 ) ( 300 )
Numerator = 4.14 × 1 0 − 21 . Denominator = 2 π ( 1.369 × 1 0 − 19 ) ( 0.5 ) = 3.04 × 1 0 − 19 .
P ≈ 1.36 × 1 0 − 2 Pa
Verify: Ratio to atmospheric: 1.36 × 1 0 − 2 /1.01 × 1 0 5 ≈ 1.3 × 1 0 − 7 — about ten-million-fold lower, as forecast. ✓ This is why high-vacuum equipment (~1 0 − 2 Pa and below) enters the molecular-flow regime.
Ex 9. At what temperature does hydrogen (M = 2 g/mol ) have v r m s equal to Earth's escape speed, 11.2 km/s ? (This is why Earth loses hydrogen to space.)
Forecast: escape speed is ~11 200 m/s — over 20× a typical room-temperature v r m s . Since v r m s ∝ T , we'll need T far above room temperature (thousands of K), but not absurdly so, because even a fraction of molecules in the high-speed tail escape at lower T .
Invert v r m s = 3 R T / M for T .
T = 3 R M v r m s 2
Why this step? The unknown is now T ; squaring both sides removes the root, then rearrange.
Plug in (M = 0.002 kg/mol , v r m s = 11200 m/s ):
T = 3 ( 8.314 ) ( 0.002 ) ( 11200 ) 2 = 24.94 ( 0.002 ) ( 1.2544 × 1 0 8 )
T ≈ 1.006 × 1 0 4 K ≈ 10 , 000 K
Verify: Reverse-check: 3 ( 8.314 ) ( 10060 ) /0.002 = 1.254 × 1 0 8 ≈ 11 , 200 m/s . ✓ Thousands of K, as forecast. (In reality hydrogen escapes at much lower T because the fast tail of the Maxwell-Boltzmann distribution leaks out continuously.)
Recall Which speed for which job?
Energy / KE calculations ::: use v r m s
Collision rate, effusion, "how often" ::: use v ˉ
Peak of the distribution ::: v p
Distance between collisions ::: λ = 1/ ( 2 nπ d 2 )
Collisions per second ::: Z = v ˉ / λ
Recall Scaling shortcuts (avoid re-plugging)
Same gas, T changes ::: v ∝ T (ratio kills all constants)
Same T , different gas ::: v ∝ 1/ M
Fixed T , P changes ::: λ ∝ 1/ P ; v r m s unchanged
M in kg/mol (0.032, not 32). T in kelvin . P in pascal . Miss any one and you're off by a big power of ten.