Graham's Law of Diffusion Calculator

Calculate relative diffusion and effusion rates of gases using Graham's law with molecular weight comparisons, isotope separation, and gas identification.

Rate Ratio (Gas1/Gas2)
1.0000
Graham's law: Rate₁/Rate₂ = √(M₂/M₁)
Time Ratio (Gas1/Gas2)
1.0000
Time for equal amounts to effuse: t₁/t₂ = √(M₁/M₂)
v_rms Gas 1
2,726.3 m/s
Root-mean-square speed = √(3RT/M)
v_rms Gas 2
2,726.3 m/s
Root-mean-square speed = √(3RT/M)
v_mean Gas 1
2,511.8 m/s
Mean molecular speed = √(8RT/πM)
v_mean Gas 2
2,511.8 m/s
Mean molecular speed = √(8RT/πM)
Separation Factor
1.000000
Single-stage enrichment factor for isotope/gas separation
Stages for 90% purity
Approximate cascade stages needed for 90% enrichment

Speed Comparison (v_rms)

Gas 1 (M=1.0)
2,726 m/s
Gas 2 (M=1.0)
2,726 m/s

Identify Unknown Gas from Effusion Data

Enter effusion times for Gas 1 (known) and the unknown gas through the same orifice under identical conditions.

Molecular Speeds at 298 K

GasM (g/mol)v_rms (m/s)v_mean (m/s)v_mp (m/s)Relative to N₂
H₂2.021,920.11,769.01,567.83.727×
He4.001,362.61,255.41,112.62.645×
CH₄16.04680.7627.2555.81.321×
NH₃17.03660.6608.7539.41.282×
Ne20.18606.9559.1495.51.178×
N₂28.01515.1474.6420.61.000×
O₂32.00481.9444.0393.50.936×
Ar39.95431.3397.4352.20.837×
CO₂44.01411.0378.6335.50.798×
SO₂64.07340.6313.8278.10.661×
Cl₂70.90323.8298.3264.40.629×
SF₆146.06225.6207.8184.20.438×
Planning notes, formulas, and examples

About the Graham's Law of Diffusion Calculator

Graham's law of effusion, formulated by Scottish chemist Thomas Graham in 1848, states that the rate of effusion (or diffusion) of a gas is inversely proportional to the square root of its molar mass. Mathematically, for two gases: Rate₁/Rate₂ = √(M₂/M₁). This elegant relationship is a direct consequence of kinetic molecular theory — lighter molecules move faster at the same temperature because they have the same average kinetic energy as heavier ones.

This law has profound practical applications: it explains why hydrogen gas escapes from containers faster than any other gas, why helium balloons deflate faster than air-filled ones, and why uranium isotope enrichment by gaseous diffusion through porous membranes is possible (albeit inefficient). The uranium enrichment process exploits the tiny mass difference between UF₆ containing ²³⁵U versus ²³⁸U isotopes.

This calculator computes relative rates, absolute velocities (root-mean-square and most probable speeds), effusion times, and helps identify unknown gases from experimental effusion data. It includes presets for common gas pairs, isotope systems, and a comprehensive reference table of molecular speeds.

When This Page Helps

This calculator quickly compares gas effusion rates, calculates molecular speeds at any temperature, and solves for unknown molar masses from experimental effusion data — useful for chemistry students, researchers, and engineers working with gas systems.

How to Use the Inputs

  1. Enter the molar masses of the two gases you want to compare.
  2. Optionally enter the temperature to calculate absolute molecular speeds.
  3. Use presets to load common gas pairs (H₂ vs O₂, He vs Ar, UF₆ isotopes, etc.).
  4. If you measured an effusion time, enter it to calculate the unknown gas's molar mass.
  5. Review the rate ratio, velocity comparison, and effusion time ratio.
  6. Check the reference table for molecular speeds of common gases at your temperature.
  7. Use the isotope separation data to understand enrichment factors.
Formula used
Graham's Law: Rate₁/Rate₂ = √(M₂/M₁), where M = molar mass (g/mol). RMS speed: v_rms = √(3RT/M), where R = 8.314 J/(mol·K), T = temperature (K). Most probable speed: v_mp = √(2RT/M). Mean speed: v_mean = √(8RT/(πM)).

Example Calculation

Result: H₂ effuses 3.98× faster than O₂

Rate ratio = √(32.0/2.016) = √15.87 = 3.98. At 298 K, H₂ has v_rms = 1920 m/s while O₂ has v_rms = 482 m/s, confirming the 3.98:1 speed ratio.

Tips & Best Practices

  • Graham's law is exact for ideal gases at low pressures where intermolecular forces are negligible.
  • For real gases at high pressures, deviations from Graham's law occur due to intermolecular interactions.
  • To identify an unknown gas, measure its effusion time relative to a known gas under identical conditions.
  • The separation factor for isotopes is very small — practical enrichment requires hundreds of cascade stages.
  • RMS speed at room temperature ranges from ~200 m/s (heavy gases) to ~1900 m/s (H₂).
  • Graham's law also approximately predicts the relative rates of gas leaks through small holes in containers.

Historical Context and Thomas Graham

Thomas Graham (1805–1869) was a Scottish chemist who studied gas movement through porous plugs and small orifices. His 1848 publication established that lighter gases pass through porous barriers faster, with rates inversely proportional to the square root of their densities. This empirical finding preceded kinetic molecular theory by over a decade and was later explained by Maxwell and Boltzmann's statistical mechanics.

Kinetic Molecular Theory Connection

Graham's law follows directly from the equipartition theorem: at temperature T, every gas molecule has average translational kinetic energy E = 3/2 kT, regardless of mass. Setting ½m₁v₁² = ½m₂v₂² gives v₁/v₂ = √(m₂/m₁). Since effusion rate is proportional to molecular speed (faster molecules hit the orifice more often), the rate ratio equals the speed ratio.

Modern Applications

Beyond the historical uranium enrichment application, Graham's law is relevant in modern technology: helium leak detection for vacuum systems, natural gas pipeline leak estimation, semiconductor fabrication (CVD gas delivery), and respiratory physiology (understanding gas exchange rates in the lungs). It's also fundamental to understanding why certain gases permeate through polymer membranes faster than others.

Sources & Methodology

Last updated:

Frequently Asked Questions

  • Effusion is gas escape through a tiny hole (smaller than the mean free path); diffusion is spreading through another gas. Graham's law applies exactly to effusion and approximately to diffusion.