Diffusion Coefficient Calculator

Calculate the diffusion coefficient for chemistry and transport calculations using common input values.

Enter values to calculate diffusion coefficient
Formula Used
Fick's First Law: D = |J| × L / |ΔC|
Input Guidance

Fick's First Law: Enter flux (J), concentration difference (ΔC, non-zero), and distance (L, positive).

Mean Square Displacement: Enter displacement (x, non-negative), time (t, positive), and dimensionality (1, 2, or 3).

Example: For Fick's law, J=2.5, ΔC=0.5, L=0.1 → D = 2.5×0.1/0.5 = 0.5

What Is the Diffusion Coefficient Calculator?

This calculator computes the diffusion coefficient (D) for chemical species in a given medium. The diffusion coefficient quantifies how quickly a substance spreads through a solvent or gas due to random molecular motion. It is a fundamental parameter in transport phenomena, reaction kinetics, and materials science.

You can input temperature, viscosity, molecular radius, and other relevant parameters to obtain an estimated diffusion coefficient in units such as cm²/s or m²/s. The tool supports common models including the Stokes-Einstein equation for spherical particles in dilute solutions.

How the Diffusion Coefficient Is Calculated

The calculator primarily uses the Stokes-Einstein relation:

D = kBT / (6πηr)

Where:

This model assumes the diffusing species is a rigid sphere moving through a continuous fluid under laminar conditions. For non-spherical molecules or concentrated solutions, the calculated value serves as an approximation.

How to Use the Calculator

  1. Select the input units for temperature, viscosity, and radius.
  2. Enter the temperature of the system.
  3. Enter the dynamic viscosity of the solvent at that temperature.
  4. Enter the hydrodynamic radius of the diffusing molecule or particle.
  5. Click calculate to obtain the diffusion coefficient.

The result updates instantly. You can switch between metric and cgs unit systems as needed.

Example Calculation

Consider a protein with a hydrodynamic radius of 3.5 nm diffusing in water at 298 K. Water viscosity at this temperature is approximately 0.89 cP.

Using the Stokes-Einstein equation:

D = (1.38 × 10⁻²³ × 298) / (6 × 3.1416 × 0.00089 × 3.5 × 10⁻⁹)

D ≈ 6.9 × 10⁻¹¹ m²/s

This value is typical for a moderate-sized protein in aqueous solution. The calculator performs this conversion automatically.

Understanding Your Results

The diffusion coefficient indicates how far a particle travels over time. A higher D means faster spreading. Typical ranges include:

If your result falls outside these ranges, verify your input values. Temperature and viscosity have a strong influence on the calculated coefficient.

Common Mistakes When Using Diffusion Coefficients

Limitations of the Stokes-Einstein Model

The calculator uses the Stokes-Einstein relation, which has known limitations:

For concentrated solutions, non-ideal systems, or anisotropic diffusion, more advanced models such as the Wilke-Chang or Hayduk-Laudie correlations may be required.

Practical Applications

FAQ

What units does the calculator support?

You can input temperature in Kelvin or Celsius, viscosity in Pa·s or cP, and radius in meters, nanometers, or micrometers. The diffusion coefficient is reported in both m²/s and cm²/s.

Can I use this for gases?

The Stokes-Einstein equation is designed for liquids. For gas-phase diffusion, use the Chapman-Enskog theory or empirical correlations. This calculator is intended for liquid-phase systems.

How accurate is the calculated value?

Accuracy depends on how well your system matches the model assumptions. For dilute solutions of spherical particles, the error is typically within 10–20%. For non-ideal systems, the result should be treated as an order-of-magnitude estimate.

What if I don't know the hydrodynamic radius?

You can estimate the radius from molecular weight using the formula r ≈ 0.066 × M1/3 (for proteins in nm, M in Da). For small molecules, experimental values from databases or literature are preferred.

Why does viscosity matter so much?

Viscosity appears in the denominator of the Stokes-Einstein equation. A small change in viscosity produces a proportional change in the diffusion coefficient. Always use the viscosity at the correct temperature for reliable results.