Diffusion Equation:
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The diffusion coefficient (D) measures how quickly particles diffuse in a fluid. In water, it depends on temperature, viscosity, and particle size according to the Stokes-Einstein equation.
The calculator uses the Stokes-Einstein equation:
Where:
Explanation: The equation relates the random motion of particles in a fluid to temperature and resistance from viscosity.
Details: The diffusion coefficient is crucial for understanding molecular transport in biological systems, chemical reactions, and industrial processes.
Tips: Enter temperature in Kelvin, viscosity in Pascal-seconds (0.00089 Pa·s for water at 25°C), and particle radius in meters. All values must be positive.
Q1: What is typical diffusion coefficient in water?
A: For small molecules at 25°C, typically 10⁻⁹ to 10⁻¹⁰ m²/s. For example, glucose is ~6.7×10⁻¹⁰ m²/s.
Q2: How does temperature affect diffusion?
A: Diffusion increases with temperature (directly proportional in this equation).
Q3: What is the hydrodynamic radius?
A: The effective radius of a particle including any solvation shell or hydration layer.
Q4: What are limitations of this equation?
A: Best for spherical particles in dilute solutions. May not apply for very small particles or complex shapes.
Q5: How to measure viscosity?
A: Use a viscometer or look up standard values (water is ~0.89 mPa·s at 25°C).