1. Water Potential Gradient: When the soil surrounding a plant has a lower water potential (meaning it has less water available) than the plant's cells, a water potential gradient is established. This gradient drives water movement from the plant's cells towards the soil.
2. Osmosis: This movement of water from areas of higher water potential (plant cells) to lower water potential (soil) occurs through the process of osmosis. Water passes through the cell membranes and cell walls, following the concentration gradient.
3. Loss of Turgor Pressure: As water leaves the plant cells, the pressure inside the cells decreases. This loss of turgor pressure causes the cells to become flaccid and lose their rigidity.
4. Wilting: The loss of turgor pressure in the plant's cells, particularly in the stems and leaves, leads to the drooping and wilting of the plant.
In summary: Wilting occurs because of osmosis driven by a water potential gradient between the plant and its surrounding environment. This gradient causes water to move out of the plant's cells, leading to a loss of turgor pressure and the plant's characteristic wilting appearance.