Transpiration
Transpiration
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Transpiration rate, the movement of water within plants, is influenced by FOUR different factors:
More light INCREASES transpiration. This is because the STOMATA OPEN UP in bright conditions to allow more gas exchange for photosynthesis.
Higher temperatures INCREASE transpiration because they increase the energy of the water molecules, and makes them move FASTER. This means the rate of DIFFUSION and EVAPORATION of the water molecules out of the stomata increases.
Good air circulation around a leaf INCREASES transpiration. This is because the air removes water vapour from the surface of the leaf and keeps the concentration of water outside lower than the inside. This increase in CONCENTRATION GRADIENT makes DIFFUSION faster.
Higher humidity levels outside the leaf DECREASES transpiration. This is because it means there is a high water concentration OUTSIDE the leaf, which results in a LOW CONCENTRATION GRADIENT which results in slower DIFFUSION.
You can estimate the rate of transpiration by measuring the how much water is taken up by a plant. This is because you can assume that water uptake by the plant is directly related to water loss by the leaves.
The GREATER the distance that the air bubble moves in a period of time, the FASTER the rate of transpiration. Record this distance at regular intervals to calculate the rate.
Transpiration rate, the movement of water within plants, is influenced by FOUR different factors:
More light INCREASES transpiration. This is because the STOMATA OPEN UP in bright conditions to allow more gas exchange for photosynthesis.
Higher temperatures INCREASE transpiration because they increase the energy of the water molecules, and makes them move FASTER. This means the rate of DIFFUSION and EVAPORATION of the water molecules out of the stomata increases.
Good air circulation around a leaf INCREASES transpiration. This is because the air removes water vapour from the surface of the leaf and keeps the concentration of water outside lower than the inside. This increase in CONCENTRATION GRADIENT makes DIFFUSION faster.
Higher humidity levels outside the leaf DECREASES transpiration. This is because it means there is a high water concentration OUTSIDE the leaf, which results in a LOW CONCENTRATION GRADIENT which results in slower DIFFUSION.
You can estimate the rate of transpiration by measuring the how much water is taken up by a plant. This is because you can assume that water uptake by the plant is directly related to water loss by the leaves.
The GREATER the distance that the air bubble moves in a period of time, the FASTER the rate of transpiration. Record this distance at regular intervals to calculate the rate.