Multiple Choice
1. C Wind's mechanism is boundary layer removal. In still air, water vapour transpired through stomata partially saturates the thin air layer immediately outside, reducing the effective gradient. Wind constantly sweeps this away, maintaining drier air at the stomatal pore. This is analogous to how a fan dries laundry faster, it removes the humid air immediately adjacent to the wet surface.
2. A Transpiration rate depends on the water potential gradient between leaf air spaces (near-saturated, ~99% humidity) and the outside atmosphere. At 95% humidity, the gradient is 99 − 95 = ~4 percentage points. At 30% humidity, the gradient is 99 − 30 = 69 percentage points, approximately 17 times larger. Transpiration rate reflects this proportional difference.
3. D The key limitation of a potometer is that it measures water uptake, not transpiration directly. At higher temperatures, photosynthesis rate also increases, meaning more water is incorporated into carbohydrates and other metabolic processes. This additional non-transpiratory water use would cause the potometer to slightly overestimate transpiration's specific contribution to water uptake. This is a valid methodological limitation specific to temperature experiments.
4. B Sunken stomata in crypts create a still-air micro-environment within the pit. Transpired water vapour accumulates there rather than being dispersed, forming a humid boundary layer immediately outside the pore. This reduces the effective water potential gradient, the driving gradient is between the pore and the humid crypt air, not between the pore and dry bulk air. The waxy cuticle blocks the cuticular pathway (not boundary layer); CAM changes timing (not boundary layer); succulents store water (not boundary layer).
5. A Elevated CO₂ signals guard cells to close stomata. CO₂ enters guard cells and is converted to bicarbonate, which triggers signalling pathways leading to K⁺ efflux from guard cells. Losing K⁺ raises guard cell water potential, water exits by osmosis, turgor falls, and the stomatal pore narrows or closes. This is the reverse of light-induced stomatal opening and is an adaptive response to high CO₂, when CO₂ is abundant, there is less need for open stomata to capture more.
Q6, Model Answer
On a hot, dry, windy day, all three environmental factors combine to dramatically increase transpiration rate relative to a cool, humid, still day.
High temperature increases the kinetic energy of water molecules in the leaf mesophyll, accelerating evaporation into leaf air spaces and increasing the water vapour concentration inside the leaf. Additionally, warm air has greater capacity to hold water vapour, so even at the same absolute humidity, warm air is further from saturation, the atmosphere can absorb much more water vapour, creating a larger gradient driving diffusion through stomata.
Low humidity means the atmosphere has very low water vapour concentration, the water potential difference between the near-saturated leaf interior (~99% humidity) and the dry outside air (~20–30% humidity) is very large, driving rapid diffusion of water vapour through open stomata.
Wind removes the humid boundary layer that would otherwise accumulate just outside the stomata in still conditions. By constantly replacing this humid air with dry bulk air, wind maintains the maximum possible gradient at the stomatal pore throughout the day.
Together, these factors push transpiration rate far above the rate of water uptake from soil via roots, causing a progressive water deficit in leaf and stem cells. As water leaves cells faster than it is replaced, turgor pressure falls, the cells become flaccid, and the plant wilts.
Q7, Model Answer
The claim is inaccurate. A potometer measures the rate of water uptake by the cut shoot, not transpiration directly.
Water uptake includes all water absorbed by the shoot, which is then used for: (1) transpiration, evaporation through stomata and cuticle (the dominant pathway, ~95%+ of uptake), (2) photosynthesis, water split in the light-dependent reactions, (3) cell expansion and growth, water retained in vacuoles of growing cells.
Therefore, the potometer slightly overestimates transpiration rate, particularly at conditions that stimulate photosynthesis (bright light, high temperature) where non-transpiratory water use increases. A more accurate statement is that the potometer measures water uptake as an indirect indicator of transpiration rate, valid because transpiration accounts for the vast majority of water uptake in a leafy shoot under normal conditions.
Q8, Model Answer
In a xerophyte with sunken stomata, the pores are positioned in recessed pits or crypts below the level of the leaf surface. Water vapour transpired through the stomata accumulates within the crypt rather than being swept away into bulk air. This creates a humid still-air boundary layer immediately outside the stomatal pore, with water vapour concentration significantly higher than the dry bulk atmosphere outside the leaf.
The water potential gradient driving diffusion of water vapour is determined by the difference in water vapour concentration between the leaf air spaces (near-saturated, ~99%) and the air immediately outside the stomatal pore. With sunken stomata, the relevant comparison is between the leaf interior and the humid crypt air, not between the leaf interior and the dry bulk atmosphere. This smaller gradient reduces the driving force for diffusion, slowing transpiration rate.
In effect, the crypt creates a microenvironment that mimics the effect of high humidity outside the leaf, reducing the apparent water potential gradient even when the bulk atmosphere is dry. This adaptation is particularly effective in calm conditions; strong wind may partially disrupt the crypt boundary layer.