7.2.8—Mass flow in phloem
- Syllabus
- 9700–2028–2029
- Objective
- 7.2.8
- Level
- AS
The pressure-flow hypothesis explains phloem mass flow: active sucrose loading at a source lowers the water potential of phloem sap, water enters by osmosis and raises source turgor pressure, and unloading at a sink lowers pressure there. Sap therefore moves in bulk down a hydrostatic pressure gradient.
Chain cue: source loading → lower phloem water potential → water entry → high source turgor → mass flow → sink unloading → water exit/lower sink pressure.
Mass flow is not diffusion of sucrose molecules one by one, and ATP is used locally to establish loading/pressure differences rather than to push every molecule along the whole tube. This card explains the pressure-flow model; it does not claim exact pressure values or make all phloem movement globally one-way. Staff-only visual brief: source and sink with water arrows, pressure labels and a single-direction sieve-tube arrow; show a second tube in the opposite direction only to represent different source-sink pairs. Do not generate or bind an image.