Transpiration

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Transpiration is the evaporation of water from plants, especially leaves. It is a type of translocation and part of the water cycle. The amount of water lost by a plant depends on its size, the light intensity, temperature, humidity, wind speed, and soil water supply.

How transpiration works[change | change source]

Leaf surfaces are dotted with openings called stomata, which act rather like pores. In most plants there are more on the undersides of the leaves than on the top. The stomata are bordered by guard cells that open and close the pore.

Transpiration happens because the plant opens its stomata. When it does, oxygen and water vapour flow out, and carbon dioxide flows in. The carbon dioxide is used in photosynthesis, and the oxygen is produced by photosynthesis.

Transpiration also pulls water through the plant. This brings with it the mineral nutrients from roots to shoots. Water moves out of the leaves into the atmosphere. This exerts a pull on the water column, which brings the water up against gravity. Water gets into the plant at the roots by osmosis, and it transports dissolved mineral nutrients to the upper parts of the plant through the xylem. A fully grown tree may lose several hundred gallons of water through its leaves on a hot, dry day. About 90% of the water that enters a plant's roots is used for this process.

Desert plants and conifers have adaptations which reduce water loss. Examples are: thick cuticles, reduced leaf areas, sunken stomata and hairs. All these reduce transpiration and conserve water. Many cacti do photosynthesis in succulent stems, rather than leaves. The surface area of even a fat stem is far less that the total surface of leaves in a tree. Also, stomata of desert plants are usually closed during the day and open at night, when transpiration is lower.

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