

Transpiration begins with the conversion of water into vapour within the spongy mesophyll of the leaf
Some of the light energy absorbed by leaves is converted into heat, which evaporates the water within the leaf tissue
This vapour diffuses out of the leaf via stomata, creating a negative pressure gradient within the leaf
This negative pressure causes water to be drawn out of xylem vessels and through cell walls by capillary action, generating tension
This tension draws water up the xylem vessels in opposition to gravity – moving in a continuous stream via mass flow
The flow of water through the xylem vessels relies on two key properties of water – cohesion and adhesion
Water molecules are polar and can form hydrogen bonds that function to drag water molecules up the xylem via cohesion
The xylem wall is also polar and forms intermolecular associations with water molecules to generate further tension via adhesion
The water vapour lost from the leaf is replaced by water taken up from the soil by the roots (maintaining a pressure gradient)
Plants may actively pump protons into the soil to displace mineral ions that then diffuse into the roots (indirect active transport)
Water will then be absorbed into the roots via osmosis – moving towards the region with the higher solute concentration
The rate of water uptake will be regulated by specialised water channels (aquaporins) on the root cell membrane
The epidermis of roots may have cellular extensions called root hairs, which further increases the surface area for absorption
Transpiration Stream
