Q.Discuss theories of water translocation.
Three theories explain ascent of sap: root pressure theory (living root activity), capillarity theory (physical capillary forces), and cohesion-tension theory (transpiration pull on a cohesive water column) — the last...
Root pressure theory (Priestley; vital theory). Living root cells generate a hydrostatic pressure (root pressure, typically +1 to +2 bars) that pushes water from the pericycle into the xylem and upward, demonstrated by exudation from a freshly cut stem. It fails, however, for trees taller than 20 m, for tall gymnosperms (near-zero root pressure), and for actively transpiring plants (where xylem sap is actually under tension, not positive pressure).
Capillarity theory (Bohem, 1863; physical force theory). Xylem vessels act like fine capillary tubes, and cohesion, adhesion and surface tension raise water a few centimetres by capillary action alone. It fails because tracheids have closed end-walls (unlike a truly hollow capillary tube), a root-cortex barrier separates xylem from soil water, and tall trees actually have wider (not narrower) xylem vessels than predicted.
Cohesion-tension theory (Dixon and Jolly, 1894; transpiration pull theory). A continuous, cohesive water column fills the xylem from root to leaf tip; transpiration from leaf mesophyll cells creates a suction (transpiration pull) transmitted down this column, pulling water upward passively. This is the most widely accepted theory today, though gas bubbles (cavitation) can break the water column, and it originally underrated the efficiency of vessels relative to tracheids. Observations such as ascent of sap continuing when leaves are coated with vaseline, or in leafless deciduous plants, show living cellular activity also plays some role alongside these physical forces.
Root pressure theory, capillarity theory, and cohesion-tension (transpiration pull) theory together explain ascent of sap; cohesion-tension is the most widely accepted, though each has objections and none is fully sufficient alone.
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