
The net drift of particles from a starting point due to random motion.Diffusion is the process by which particles spread out from regions of high concentration to regions of low concentration, driven by their random thermal motion. It is a fundamental transport mechanism in physics, chemistry, and biology, governing everything from the spread of a drop of ink in water to the movement of oxygen across cell membranes. The concept is central to understanding how systems evolve toward equilibrium, as the second law of thermodynamics dictates that entropy tends to increase, and diffusion is a prime example of this tendency in action.
The modern mathematical treatment of diffusion was developed by Adolf Fick in 1855, who formulated the laws that bear his name. Earlier observations, such as those by Robert Brown on pollen grains in water, provided qualitative evidence of random motion, later explained by Albert Einstein in 1905 as a consequence of molecular collisions.
At the microscopic level, particles in a fluid or gas are in constant, random motion due to their thermal energy. When there is a concentration gradient, more particles are moving from the high-concentration side to the low-concentration side simply because there are more of them there. This net flux is described by Fick's laws of diffusion, which relate the flux to the concentration gradient and a diffusion coefficient that depends on particle size, temperature, and the medium. Over time, the gradient smooths out until the concentration is uniform, though individual particles continue their random walk.
Diffusion is exploited in countless technologies, including the doping of semiconductors in microchip manufacturing, the controlled release of drugs from polymer matrices, and the separation of isotopes via gaseous diffusion. It also plays a critical role in understanding atmospheric mixing, ocean currents, and the behavior of pollutants.
The time it takes for a particle to diffuse a given distance scales with the square of that distance, so doubling the distance quadruples the time — a reason why diffusion is efficient over tiny scales but hopelessly slow over macroscopic ones.






