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Exercises · Q10

Q.What role does root pressure play in water movement in plants?

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Root pressure is a positive hydrostatic pressure that develops within the xylem of roots as a direct consequence of the active (energy-requiring) absorption of mineral ions and, secondarily, water by living root cells.

How it develops:

  • Root cells actively pump mineral ions from the soil solution into the stele (the central vascular cylinder), using ATP-driven transport processes; this accumulation of ions lowers the water potential inside the xylem of the root relative to the surrounding soil water.
  • Water then follows passively by osmosis, moving from the soil (higher water potential) into the root xylem (lower water potential).
  • Because the xylem vessels form a relatively confined space and water continues to be drawn in, this build-up of water generates a measurable positive pressure in the xylem sap — this is root pressure.

Role in water movement:

  • Root pressure can push the water column a limited distance upward through the stem, and this effect is most pronounced at night or in the early morning, when stomata are largely closed and transpiration is minimal, so the pressure that builds up in the root is not immediately relieved/pulled away by transpirational demand from the leaves.
  • Under these low-transpiration conditions, root pressure alone is directly responsible for the well-known phenomenon of guttation — the appearance of small droplets of liquid water (containing minerals) exuded from special pores called hydathodes, typically found at the tips and margins of leaves in certain plants (e.g., grasses, garden nasturtium, tomato).
  • In small or short herbaceous plants, root pressure can be a meaningful contributor to overall water movement, occasionally being enough on its own to push water some distance up the plant body.

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