Indirect Measurement: The movement of an air bubble in a capillary tube represents the volume of water absorbed by the plant to replace what was lost to the atmosphere.
Volume Calculation: The volume of water taken up () can be calculated using the formula for a cylinder, where is the internal radius of the capillary tube and is the distance the bubble travels:
Light Intensity: Increased light causes stomata to open wider for diffusion, which simultaneously increases the exit route for water vapor.
Temperature: Higher temperatures increase the kinetic energy of water molecules, accelerating evaporation from the mesophyll cells and increasing the diffusion gradient.
Humidity: High external humidity reduces the water potential gradient between the leaf interior and the air, significantly slowing down the rate of transpiration.
Wind Speed: Moving air removes the 'boundary layer' of saturated air from the leaf surface, maintaining a steep water potential gradient and increasing the rate.
| Feature | Bubble Potometer | Mass Potometer |
|---|---|---|
| Measurement | Distance moved by an air bubble | Change in total mass of the system |
| Proxy | Measures water uptake | Measures actual water loss (mass) |
| Sensitivity | High; good for short-term changes | Lower; requires longer time for measurable change |
| Calculation | Requires tube radius: | Direct mass difference |
Airtightness is Critical: Always mention that the apparatus must be airtight. If air leaks in, the bubble will not move in response to the plant's suction, leading to a zero or erratic reading.
Unit Consistency: Ensure that the radius of the capillary tube and the distance moved are in the same units (e.g., mm) before calculating volume in .
Control Variables: When investigating one factor (e.g., light), emphasize that all other factors (temperature, humidity) must be kept constant to ensure validity.
Repeatability: Suggest performing multiple runs for each condition and calculating a mean to identify anomalies and improve the reliability of the data.