Turgor pressure and plant support

In well-watered conditions, plant cells absorb water by osmosis. The vacuole swells, pressing the cytoplasm against the cell wall. The cell wall resists further expansion, and the cell becomes turgid. The collective outward pressure of many turgid cells supports herbaceous (non-woody) plant structures: leaves stay flat and stems stay upright.

This support mechanism is purely hydraulic. Unlike animals, herbaceous plants lack an internal skeleton. Their rigidity depends on water pressure within cells.

Why wilting happens

When transpiration exceeds water uptake: during hot, dry, or windy conditions: cells lose water faster than they can absorb it. The vacuole shrinks, the cell becomes flaccid, and turgor pressure drops. Without turgid cells pushing against cell walls, the plant wilts: leaves droop and stems become limp.

In severe cases, continued water loss leads to plasmolysis, where the cell membrane pulls away from the cell wall entirely. At this point the cell may not recover even if water is restored.

Adaptations to reduce water loss

Plants in dry environments (xerophytes) have structural adaptations to reduce transpiration: thick waxy cuticles that reduce evaporation from the leaf surface; fewer or sunken stomata that reduce the rate of water vapour diffusion; rolled leaves that trap humid air near stomata; and reduced leaf surface area (spines in cacti).

Even in temperate environments, plants close their stomata during drought. This conserves water but reduces carbon dioxide entry, which slows photosynthesis: a trade-off the plant must manage to survive.