Osmosis and water potential
Water moves down its own potential gradient.
Osmosis is the net movement of water molecules across a partially (selectively) permeable membrane, from a region of higher water potential to a region of lower water potential. It is a special case of diffusion — only the solvent (water) moves, because solute particles cannot cross the membrane freely.
Water potential (Ψ, the Greek letter "psi") is a measure of the tendency of water to move out of a system. It is measured in units of pressure — kilopascals (kPa).
Water potential has two components:
- Solute potential () — also called osmotic potential. Dissolving solutes lowers water potential, so is always zero or negative. The more solute, the more negative .
- Pressure potential () — the physical (hydrostatic) pressure on the water. In a plant cell, the cell wall pushes back on the swollen contents, giving a positive .
Key reference point: pure water at standard atmospheric pressure has a water potential of exactly zero (). Because solutes only ever make Ψ more negative, the water potential of any solution is negative.
Direction of movement. Water moves from higher (less negative) Ψ → lower (more negative) Ψ until the two are equal (equilibrium). So a cell with a more negative Ψ than its surroundings will gain water by osmosis.
- Osmosis: net water movement across a partially permeable membrane.
- , measured in kPa.
- Pure water: ; solutes make Ψ more negative.
- Water moves from higher Ψ → lower (more negative) Ψ.