Osmosis quantified using water potential
Ψ: tendency for water molecules to diffuse from one solution to another
Ψ = Solute Potential + Pressure Potential
Polar solute’s presence restricts water movement as water molecules, cluster around particles
Less ‘free’ water molecules able to diffuse to another solution to another
Pure Water Potential = 0kPa
All solutions have negative Ψ
More solute, more negative
All cell membranes are selectively permeable
Water diffuses in/out of organelles/cells by osmosis
Down water potential gradient