Transpiration is the driving force of water movement inside a plant. As water evaporates from the leaves, water is drawn from the soil, transporting dissolved nutrients through the plant and into the plant cells for photosynthesis. Photosynthesis is the process during which plants use sun energy, water and gases such as carbon dioxide to produce its own source of energy, glucose.
In the process, oxygen is produced. Secondly, transpiration is needed to cool the plant, similar to humans sweating on warm days. Finally, transpiration is needed to maintain the water pressure inside plant cells. This water pressure is called turgor pressure. It helps to keep the cells rigid in order to support the plant.
Transpiration depends on the temperature, wind and the difference of water vapour pressure inside and outside the plant. The following factors also affect the transpiration rate:
Climatological factors such as air temperature, air humidity and wind. For example in dry windy conditions, transpiration will be faster than during cool moist days.
Factors such as soil water content: The lower the soil water content, the slower the water supply to the plant roots. In clay soil, small pores between sand particles, and saline soils, high salt content, the rate of transpiration is also lower.
Transpiration rate is also influenced by the type of crop the development stage of the crop. Xerophytic plants (drought tolerant) reduce transpiration rates, by only opening stomata during the night. Often, these plants have hair on their leaves to reduce the effect of sunlight and wind. Some crops can even close stomata under extreme water stress conditions.
Root rot diseases reduce the ability of roots to absorb water and therefore reduce the rate of transpiration.
Plants under net covers transpire less. This is because of better protection against wind and direct sunlight as well as the higher humidity under the nets.In the Napa Valley in California, electric heaters with big fans blow hot air over vineyards to limit frost.
The transpiration rate of plants can be measured using various methods: The traditional method is to measure differences in soil water content at the plant roots by instruments such as tensiometers, resistance blocks and neutron probes.
Transpiration rate can also be measured by keeping track of weight changes in lysimeters with the soil surface covered in mulch to eliminate soil evaporation. More advanced ways of measuring transpiration rate include probes placed permanently in the ground with links via radio or cell phone, to computers as well as infra-red measurement and satellite imagery.
To measure transpiration in tree crops is to measure sap flow in the trunk by noting differences in trunk diameter or by placing micro-measuring devices in or on the tree trunk.Source Water Research Commission