Simple diffusion and Fick's law
Passive movement down a gradient — and the equation that controls its rate.
Simple diffusion is the net movement of particles (molecules or ions) from a region of higher concentration to a region of lower concentration — that is, down a concentration gradient — as a result of their random kinetic motion. It is passive: the energy comes from the kinetic energy of the particles themselves, not from ATP.
Across the cell-surface membrane, only certain substances can diffuse directly through the phospholipid bilayer:
- Small, non-polar (lipid-soluble) molecules — oxygen (), carbon dioxide () and other lipophilic molecules dissolve in the hydrophobic tail region and pass straight through.
- Large molecules and charged/polar particles (glucose, amino acids, ions) cannot cross the bilayer freely — they need transport proteins (facilitated diffusion or active transport).
Fick's law summarises what controls the rate of diffusion:
So the rate increases when:
- the surface area of the membrane is larger (e.g. microvilli, alveoli, root hair cells),
- the concentration difference (gradient) across the membrane is steeper (maintained by blood flow or ventilation), or
- the diffusion distance is shorter (e.g. a single squamous epithelial cell wall in the alveolus).
Fick's law is the basis for almost every "explain why this exchange surface is efficient" question — flat lungs, folded gut, thin gills all map onto one of the three terms.
- Simple diffusion = net passive movement down a concentration gradient; no ATP.
- Only small, non-polar/lipid-soluble molecules (O₂, CO₂) cross the bilayer directly.
- rate ∝ (surface area × concentration difference) ÷ diffusion distance.