Water Movement in Plants

Long-distance water movement is crucial to the survival of land plants. Al­though plants vary considerably in their tolerance of water deficits, they all have their limits, beyond which survival is no longer possible. About 85 per­cent of the fresh weight of leaves can be water. On a dry, warm, sunny day, a leaf can evaporate 100 percent of its water weight in just an hour. Water loss from the leaves must be compensated for by the uptake of water from the soil. Water transport is also important for the uptake of essential min­eral nutrients from the soil. Shortages of mineral nutrients such as nitro­gen, potassium, and phosphorus are often limiting to plant growth, which is why fertilizers are often added to the soil to improve plant productivity and appearance.

The Cohesion-Tension Theory

The major mechanism for long-distance water transport is described by the cohesion-tension theory, whereby the driving force of transport is transpi­ration, that is, the evaporation of water from the leaf surfaces. Water mol­ecules cohere (stick together), and are pulled up the plant by the tension, or pulling force, exerted by evaporation at the leaf surface.

Water will always move toward a site with lower water potential, which is a measure of the chemical free energy of water. By definition, pure wa­ter has a water potential of 0 MegaPascals (MPa). In contrast, at 20 percent relative humidity, the water potential of the atmosphere is -500 MPa. This difference signifies that water will tend to evaporate into the atmosphere. The water within plants also has a negative potential, indicating water will tend to evaporate into the air from the leaf. The leaves of crop plants often function at -1 MPa, and some desert plants can tolerate leaf water poten­tials as low as -10 MPa. The water in plants can exist at such low water po­tentials due to the cohesive forces of water molecules. The chemical structure of water molecules is such that they cohere very strongly. By the cohesion-tension theory, when sunlight strikes a leaf, the resultant evapo­ration first causes a drop in leaf water potential. This causes water to move from stem to leaf, lowering the water potential in the stem, which in turn causes water to move from root to stem, and soil to root. This serves to pull water up through the xylem tissue of the plant.

From Root to Leaf

Plants have root hairs and often mycorrhizal fungi at the root surface, both of which serve to filter the soil water as it enters the plant. Mycorrhizae are symbiotic associations between plant roots and fungi. The root cells and mycorrhizal fungi both actively uptake certain mineral nutrients. Mycorrhizae can be particularly important for the uptake of phosphate. The active uptake of minerals by living cells of the root and the subsequent transfer of minerals to the xylem can result in positive root pressures, with water potentials above 0 MPa. This occurs only under certain conditions, such as at night or during rainstorms, when water loss from the leaves is minimal. Such positive root pressures disappear with the onset of leaf tran­spiration.

Water molecules move from the soil into living cells of the root, and eventually into the transport cells of the xylem, known as tracheids and vessels. These xylem cells are dead and hollow, allowing rapid water trans­port. They also have hardened cell walls to help them resist the tendency to collapse as water is sucked through them. Both tracheids and vessels have pits on the sides of their walls, which include porous areas for side- to-side transport. Unlike tracheids, a vessel is composed of many cells stacked end to end, with perforations between cells, allowing for more ef­ficient transport.

The long-distance transport of the water molecule occurs first within the xylem cells of the root, then the xylem of the stem and branch, and then into the xylem of a leaf midrib and vein. Driven by transpiration, the water molecule is pulled from the nonliving tracheids and vessels of the xylem in the living cells of the leaf mesophyll (middle layer) and to the surface of mesophyll cell walls. The water molecule then evaporates into a leaf inter­cellular air space and finally out of a stomatal pore and into the atmosphere. Though photosynthetic action consumes some water, only a small fraction of the water that travels through the plant is used directly for the photo­synthetic reaction, which occurs in leaf mesophyll cells. Instead, most wa­ter is lost by transpiration through the stomates.

The Role of Stomates

Leaves of land plants are covered with a waxy cuticle that prevents water loss and gas exchange. The stomates at the leaf surface have guard cells that open and close the stomate to regulate the uptake of carbon dioxide and release of oxygen, as required for photosynthesis. They also serve to regulate water loss from transpiration. During the day, the stomates nor­mally open up in response to sunlight, allowing for photosynthetic gas ex­change, but also allowing for transpiration. At night, the stomates normally close, preventing unnecessary water loss. When excessive water loss oc­curs during the day, drops in leaf water potential can cause stomates to close. Were it not for stomate closure in response to water stress, the leaves would suffer excessive water loss, the leaf cell membranes and photosyn­thetic apparatus would be destroyed, and “cavitation” would occur in the xylem cells. Cavitation, which is a break in the water column, occurs when air is pulled into the xylem vessel or tracheid. This can make the xylem cell unable to conduct water. Plants vary considerably in their vulnerabil­ity to cavitation, but for most plants, stomate closure can prevent cavita­tion from occurring.

The transpirational water loss allows for uptake of mineral nutrients from the soil. However, much of the water loss that land plants exhibit can be viewed as a “necessary evil.” The stomates must open up to allow for photosynthesis to occur, and during the process of letting carbon diox­ide into the leaf, water vapor is lost to the atmosphere. When the stom­ates close to prevent excess water loss, photosynthesis is compromised.

References

Holbrook, N. M., M. J. Burns, and C. B. Field. “Negative Xylem Pressures in Plants: A Test of the Balancing Pressure Technique.” Science 270 (1995): 1183-1192.

Raven, Peter H., Ray F. Evert, and Susan E. Eichhorn. Biology of Plants, 6th ed. New York: W. H. Freeman and Company, 1999.

Taiz, Lincoln, and Eduardo Zeiger. Plant Physiology, 2nd ed. Sunderland, MA: Sinauer Associates, 1998.