Measuring water uptake - potometers
Investigating transpiration
The uptake of water can be measured using a potometer. Under normal circumstances, the rate of water uptake gives a measure of the rate of transpiration.
A simple potometer is a piece of capillary tubing to which a plant has been connected. The water uptake is measured by recording the time taken for a bubble in the tube to move a set distance.
Aim of the experiment
To find the rate of water uptake of a plant.
Method
Image caption, The potometer is filled with water.
Image caption, A shoot is cut from a woody plant. The end of the shoot is cut under water to ensure that the xylem remains water-filled and prevents air locks.
Image caption, The shoot is inserted into the rubber tubing at the end of the potometer.
Image caption, The potometer is raised so that a bubble of air is taken up.
Image caption, The potometer is lowered into the water. The distance travelled by the air bubble is recorded over a period of time.
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Variables
- Independent variable - time
- Dependent variable - the distance moved by the bubble along the capillary tube
- Control variables - temperature, air flow or draughts, adequate supply of water
Risks
Care must be taken when inserting the plant shoot into the rubber tubing attached to the capillary tube and with the scissors used to cut the plant shoot.
Example results
| Time in minutes | Distance moved by bubble in mm |
| 0 | 0 |
| 5 | 16 |
| 10 | 32 |
| 15 | 47 |
| 20 | 64 |
| 25 | 80 |
| 30 | 95 |
| Time in minutes | 0 |
|---|---|
| Distance moved by bubble in mm | 0 |
| Time in minutes | 5 |
|---|---|
| Distance moved by bubble in mm | 16 |
| Time in minutes | 10 |
|---|---|
| Distance moved by bubble in mm | 32 |
| Time in minutes | 15 |
|---|---|
| Distance moved by bubble in mm | 47 |
| Time in minutes | 20 |
|---|---|
| Distance moved by bubble in mm | 64 |
| Time in minutes | 25 |
|---|---|
| Distance moved by bubble in mm | 80 |
| Time in minutes | 30 |
|---|---|
| Distance moved by bubble in mm | 95 |
Analysis of results
Plot a line graph of the data.
The rate of water uptake is best found using the gradient of the graph.
You need to calculate the gradient of the graph - and not take values from the table of results.
Choose any two points on straight line:
- choose as wide an interval along the x-axis as is possible
- try to make sure that these correspond with values of y that you can read accurately
The most accurate results will be obtained if these points are as far apart as possible. Here, the two points on the line, labelled P and Q, are at either end of the line.
Calculate the gradient:
P Value of x = 0 minutes
P Value of y = 0 millimetres
Q Value of x = 30 minutes
Q Value of y = 96 millimetres
\(Gradient\; of\; line\: =\: \frac{increase\: in\: y}{increase\: in\: x }\: =\: \frac{(96-0)\: mm)}{(30-0)\: min)}\: =\: 3.2\: mm/minute\)
The distance moved by the bubble is 3.2 mm/minute.
Note that rate is always a compound measureA compound measure is made up of two or more other measurements, eg rate of water loss is a compound measure because it is made up of water loss - for instance in grams - and time - for instance in minutes.. It is made up of two - or more - measurements. In this case, millimetres per minute.
Question
When will the water uptake of a plant not equal the rate of transpiration?
When it is short of water, eg it has wilted.