Osmosis is the movement of water across semi-permeable membranes from an area of higher water potential to an area of lower water potential until dynamic equilibrium is reached
Water potential (ψ) is the pressure created by water molecules measured in kPa, with pure water at 25°C & 100 kPa having a ψ of 0. More solute leads to a more negative ψ
Simple diffusion is a passive process where small, lipid-soluble molecules move directly through the bilayer from high to low concentration without requiring ATP energy
Facilitated diffusion is a passive process where specific channel or carrier proteins transport large and/or polar molecules/ions down their concentration gradient
Channel proteins work by binding specific ions, causing one side of the protein to close and the other to open.
Carrier proteins work by binding complementary molecules, leading to a conformational change that releases the molecule on the other side of the membrane
Fick’s law states that the rate of diffusion is determined by the surface area multiplied by the difference in concentration, divided by the diffusion distance
Active transport is an active process requiring ATP energy to transport molecules/ions against their concentration gradient using specific carrier proteins
Co-transport involves moving a substance against its gradient while coupling it with the movement of another substance down its gradient using symport or antiport proteins