Water movement up a plant increases as the transpiration rate increases. Water evaporates from the spaces between cells in the leaf through the stomata, it moves down the waterpotential gradient so for water to leave through stomata there has to be less water in the atmosphere than in the leaf
Factors that affect transpiration rate: LIGHT INTENSITY
Stomata open when it is light to let in CO2 for photosynthesis, when it is dark no photosynthesis is happening so the stomata close
Little transpiration happens at night/darkness
Factors that affect transpiration rate: TEMPERATURE
In warmer conditions water particles have more kinetic energy so they are able to evaporate from the surface of the leaf faster, this increases the water potential gradient between the inside and outside of the leaf so the transpiration rate is increased
Factors that affect transpiration rate: HUMIDITY
If the air around plants is dry, the water potential gradient is increased so transpiration occurs faster
In humid environments, the water potential gradient is reduced as there is a lot more water in the atmosphere so the rate of transpiration decreases
Factors that affect transpiration rate: AIR MOVEMENT
Lots of wind blows water molecules away from the stomataincreasing the waterpotential gradient and therefore increasing the transpiration rate
High Transpiration rate:
High light intensity
High temperature
High wind
Low humidity
Low Transpiration rate:
High humidity
Low light intensity
Low temperature
Low/no wind
Using a potometer:
A potometer can measure water uptake by the plant and can be used to estimate how different factors affect the transpiration rate
eg using a fan, creating a humid environment, using different light intensities
It is almost impossible to measure transpiration because it is extremely difficult to condense and collect all water vapour that leaves all the parts of a plant
However, what we can measure is the amount of water that is taken up in a given time by a part of the plant such as a leafy shoot - the rate of uptake is almost the same as the rate at which transpiration is occurring
Can then measure water uptake by the same shoot under different conditions
Considerations when measuring transpiration rate:
The shoot must be cut underwater
Prevent air entering the xylem (so the water column remains unbroken)
Considerations when measuring transpiration rate:
Shoot cut on an angle
Increase surfacearea available to uptake water
Considerations when measuring transpiration rate:
End of the capillarytube must stay submerged in water
The diameter of the capillary tube should be known/measured
Considerations when measuring transpiration rate:
This is only an estimate as it assumes all water taken up is lost in transpiration but some water is used up in reactions eg photosynthesis, some produced by respiration, some used to support the plant (stored in vacuoles)
To measure the rate of transpiration:
A leafy shoot is cut underwater, using a rubber tube the leaf shoot is fitted to the potometer under water
Potometer is removed from under the water to allow an air bubble to form at the end of the capillary tube
Start point of the air bubble must be recorded
Using a stopwatch, the time it takes for the bubble to move a certain distance can be recorded - the rate is an estimate of transpiration rate
Measuring rate of transpiration: Restart/repeat the experiment
Once the air bubble nears the junction of the reservoir tube and the capillary tube, the tap on the reservoir is opened and the syringe is pushed down until the bubble is pushed back to the start of the scale on the capillary tube