Your browser does not support JavaScript! (M)
Water site headerMasthead Island, Great Barrier Reef Print-me keygo to Water Visitor Book contributions
Go to my page Water Structure and Science


Diffusion, particles of a soluble material spread out


Diffusion, particles of a soluble material spread out to uniformly distribute themselves


Diffusion is the net movement of particles from a region of high chemical potential to a region of low chemical potential.

V Osmotic pressure

V Brownian motion

V Diffusion

"...the irregular movement of the particles produced by the thermal molecular movement"

Albert Einstein, 1905  


Diffusion b is the net movement of particles (for example, molecules) from a region of high chemical potential (for example, high concentration) to a region of low chemical potential (for example, low concentration) due to random thermal movement, see above right. Such diffusion also involves the movement of water in the opposite direction. The movement is due to the statistical outcome of random Brownian motion and eventually will result in similar concentrations throughout the solution (see the right-hand vessel on the above right).


The diffusive flux (J, the amount of substance moving through a unit area A per unit time t, mol ˣ m-2 ˣ s-1 ) is governed by Fick's first law:


Ficks 1st law

flux= -diffusivity x change in concentration with distance


where D is the diffusivity (m2 ˣ s-1 ), is the change in concentration (ideally, mol ˣ m-3), and dx is the change in position (m). The diffusion direction is from higher concentration to lower concentration, such that dφ/dx is always negative, and the diffusive flux always positive, in the diffusion direction. Thus, the particle flux is proportional to the concentration gradient.


In a diffusion process, the concentration of a substance in the region of higher concentration gradually decreases, and the concentration of the substance in the region of lower concentration gradually increases. With time, the concentrations gradients dissipate within the bulk. Diffusion increases entropy (randomness), leading to a lower energy state. Eventually, equilibrium is established with a uniform distribution throughout. The concentration change with time is described by Fick's second law:


Ficks second law


D is described by the Stokes-Einstein equation for translational diffusion [806], a


Diffusivity= boltzman constantxtemperature/(6 x pi x viscosity x particle radius)


where KB is the Boltzmann constant (J ˣ K-1; kg ˣ m2 ˣ s-2 ˣ K-1), T is the temperature (K), η is the dynamic viscosity (Pa ˣ s; kg ˣ m-1 ˣ s-1), r is the averaged particle radius (m), R is the gas constant (J ˣ mol-1 ˣ K-1; kg ˣ m2 ˣ s-2 ˣ K-1 ˣ mol-1) and N is the Avogadro constant (mol-1; surprisingly, this may be estimated from this simple equation). The 6πηr term comes from Stokes law for the drag of a slow-moving sphere with radius R having a velocity V due to a force F:


F = drag ˣ V


where drag = 6πηr (kg ˣ s-1), F is the force (N, kg ˣ m ˣ s-2) and V is the particle velocity (m ˣ s-1 ). The drag term includes both the fluid-particle friction (viscous shear stress, 4πηr) and the creation of a pressure difference in the fluid each side of the particle in the direction of flow (2πηr).


'Diffusion' should not be confused with 'advection' or 'convection'. Advection is the movement due to the velocity of the fluid. Convection applies to the movement of a fluid due, for example, to thermal gradients.

[Back to Top to top of page]



a It has been proposed that this equation should also be associated with the Australian, William Sutherland, who published before Einstein. W. Sutherland, A dynamical theory for non-electrolytes and the molecular mass of albumin, Philosophical Magazine, 6 (1905) 781-785.. [Back]


b The word 'diffusion' is derived from the Latin word 'diffusionem' meaning to "spread out". [Back]



Home | Site Index | Water activity | Brownian motion | Osmotic pressure | LSBU | Top


This page was established in 2006 and last updated by Martin Chaplin on 3 October, 2018

Creative Commons License
This work is licensed under a Creative Commons Attribution
-Noncommercial-No Derivative Works 2.0 UK: England & Wales License