B3.1.9—Transpiration
Transpiration is water loss from leaves, driven by evaporation and diffusion through stomata and altered by humidity, temperature, wind and light.
- Syllabus
- First assessment 2025
- Objective
- B3.1.9
- Level
- HL
Transpiration is water loss from leaves, driven by evaporation and diffusion through stomata and altered by humidity, temperature, wind and light.

Coverage 2012–2025 · Updated 15 Jul 2026
Transpiration is water loss from a plant: water evaporates from moist mesophyll cell walls and the vapour diffuses through leaf air spaces and out through stomata.
Gas exchange exposes moist internal surfaces to the atmosphere, so stomatal opening for carbon dioxide entry also permits water-vapour loss. A steeper water-vapour gradient or more open stomata increases the rate.
Higher temperature increases evaporation; lower humidity steepens the vapour gradient; wind removes the humid boundary layer; light commonly promotes stomatal opening. Water stress can close stomata and reduce transpiration.
A warm, dry, windy leaf usually transpires faster than a cool leaf in still, humid air because evaporation is faster and the external boundary layer is continually replaced.
A potometer measures water uptake as an estimate, not transpiration directly; water may also be used in growth or photosynthesis. State which factor changes evaporation, gradient or stomatal aperture.
This objective is assessed through structured response, commonly using Explain / Outline / Suggest.
Explain / Outline / Suggest / Define / Compare
Build the answer around this relationship: Transpiration involves evaporation from leaf surfaces followed by diffusion through stomata.
Assuming a potometer directly measures water lost rather than estimating it from water uptake.
Representative question
Explain how abiotic factors affect the rate of transpiration in terrestrial plants.
a. less transpiration/water loss as (atmospheric) humidity rises;
b. air spaces inside leaf are saturated/nearly saturated (with water vapour);
c. smaller concentration gradient with higher atmospheric humidity;
d. more transpiration/water loss as temperature rises/with more heat;
e. faster diffusion / more kinetic energy (of water molecules);
f. faster evaporation (due to more latent heat available);
g. more transpiration/water loss as wind (speed) increases;
h. humid air/water vapour blown away from the leaf;
i. increasing the concentration gradient (of water vapour);
j. more transpiration/water loss in the light;
k. light causes stomata to open / stomata closed in darkness;
I. Iow CO2 concentration inside leaf in bright light so stomata open wider;
Accept any of the points if clearly made on an annotated graph.
Core gas-exchange answers link exchange surfaces to diffusion gradients. For animals, exchange surfaces are explained by diffusion properties, ventilation, and blood flow. For plants, leaves allow carbon dioxide entry and oxygen/water vapour exit while controlling water loss through stomata. Spirometry, transpiration, and stomatal density data provide evidence of gradient and surface-area effects.