7.2 Transport Mechanisms

Syllabus
9700–2028–2029
Topic
7.2
Level
AS

Learning objectives

Plants transport ions and organic compounds dissolved in water

Water acts as the transport solvent inside plants. Some mineral ions and organic compounds dissolve in it and move as part of xylem sap or phloem sap.

Transport tissue Water-based solution Examples dissolved in water Main context
xylem xylem sap mineral ions absorbed from soil movement from roots towards stems and leaves
phloem phloem sap organic assimilates such as sucrose and amino acids movement from a source to a sink

Dissolving allows ions and polar organic compounds to be carried with bulk water through conducting tissues. The following cards explain how substances enter xylem and how xylem and phloem flow are driven.

This objective states the solvent relationship; it does not require the apoplast/symplast mechanism. Do not treat mineral ions or sucrose as moving through the plant as undissolved solids.

Apoplast and symplast routes converge before xylem entry

Water moves from soil through root hairs and cortex to the endodermis, where the apoplast is blocked and all water entering xylem must cross a cell-surface membrane into the symplast.

Route Where water moves Membrane crossing through cortex
apoplast through cellulose cell walls and spaces between cells not at each cortex cell
symplast through cytoplasm connected by plasmodesmata crosses a membrane when first entering the symplast
  1. Root hairs provide a large absorption surface; water enters cells down a water-potential gradient.
  2. Across cortex, water follows apoplast and/or symplast routes. Vacuoles are not part of the symplast definition.
  3. Suberin in the Casparian strip of endodermal cell walls blocks the apoplast and prevents uncontrolled wall-space entry.
  4. Water and ions cross an endodermal membrane into cytoplasm, enabling selective ion control.
  5. The solution enters xylem. Lignin waterproofs and strengthens xylem vessel walls, supporting the conducting pathway.

Apoplast movement through cellulose walls is not osmosis; symplast means cytoplasm linked by plasmodesmata, not vacuoles. The suberin Casparian strip blocks apoplast flow before the lignified xylem pathway.

Transpiration is evaporation followed by vapour diffusion

Transpiration involves evaporation of water from internal leaf surfaces followed by diffusion of water vapour from the leaf to the atmosphere.

  1. Liquid water reaches mesophyll tissues from leaf xylem and moistens mesophyll cell walls.
  2. Water evaporates from those cell-wall surfaces into the intercellular air spaces.
  3. Water vapour diffuses through the air spaces and out through stomatal pores.
  4. Net diffusion occurs from the more humid leaf interior to the less humid atmosphere while stomata provide an open route.

Evaporation is a liquid-to-vapour phase change at mesophyll surfaces. Diffusion is the subsequent net movement of vapour down its concentration gradient to the atmosphere; together they define transpiration.

Do not call transpiration the whole liquid-water xylem stream, guttation or photosynthesis. The required sequence is internal-surface evaporation followed by vapour diffusion to the atmosphere.

Cohesion transmits transpiration pull through xylem

Evaporation from leaves creates tension in xylem water. Hydrogen-bond cohesion keeps water molecules in a continuous column so transpiration pull is transmitted, while adhesion to cellulose cell walls supports contact with the vessel walls.

  1. Transpiration removes water from leaf surfaces and lowers leaf water potential.
  2. Water is drawn from nearby xylem, creating tension (negative pressure) in the water column.
  3. Hydrogen bonds cause cohesion between water molecules, so pulling one part of the column transmits force through the column towards roots.
  4. Hydrogen-bond adhesion between water and cellulose helps water remain in contact with xylem walls.
  5. Lignified vessel walls resist collapse under tension, allowing upward bulk movement as transpiration pull continues.

Evaporation supplies the pull; cohesion transmits it through water; adhesion supports the column at cellulose walls; lignin supports the vessel. Hydrogen bonding is therefore part of force transmission, not an independent pump.

Do not replace cohesion-tension with root pressure or claim hydrogen bonds actively pump water. The model is transpiration pull transmitted through a cohesive column and supported by adhesion and lignified walls.

Annotate visible xerophyte leaf features with water-loss mechanisms

An annotated transverse-section drawing must reproduce visible xerophytic leaf features and attach each label to a causal explanation of reduced transpiration.

  1. Draw the section's large tissue boundaries and visible stomatal regions with clear unshaded lines and correct proportions.
  2. Label only features present in the source, such as thick cuticle, rolled/folded lamina, sunken stomata, stomatal crypts, hairs, reduced air spaces or succulent water-storage tissue.
  3. Extend each annotation beyond a name: state how the feature changes diffusion distance, exposed area, trapped humidity, air movement or the water-vapour gradient.
  4. Use label lines ending on the exact feature and keep observation separate from mechanism.
  5. Check that the annotation explains reduced water loss rather than merely calling the plant xerophytic.
Visible feature Valid annotation mechanism
thick waxy cuticle increases resistance/diffusion distance for water loss through the epidermis
rolled leaf or stomatal crypt traps humid air and reduces the water-vapour gradient
hairs around stomata reduce air movement and retain a humid boundary layer
sunken stomata place pores away from freely moving dry air
reduced exposed leaf area reduces evaporating surface available for water loss

Do not add features or behaviours not visible in the transverse section, such as claiming night-only stomatal opening from anatomy alone. Not every xerophyte shows every feature; annotate the supplied evidence.

Phloem translocation moves assimilates from a source to a sink

Phloem translocation is the transport of assimilates from a source, where they are available, to a sink, where they are stored or used. Phloem sap is a solution containing mainly sucrose as well as water and other dissolved substances such as amino acids, hormones and minerals.

  • Source: A green leaf or green stem can produce sugars by photosynthesis and export them as sucrose. A storage organ can also act as a source when stored material is mobilised for new growth.
  • Sink: A developing seed, fruit, root or other storage/growing region receives assimilates for use or storage. The same organ can change from source to sink as development or demand changes.
  • Pathway: Sieve-tube elements carry the phloem sap. Companion cells support the associated sieve-tube elements and the loading/unloading interface; the detailed proton-gradient loading mechanism belongs to the next card.
  • Direction: Assimilates can move upwards or downwards in phloem because direction follows the current source-to-sink relationship. A plant therefore cannot be classified as having one fixed “up” or “down” phloem direction.
  • Energy boundary: Loading at the source and unloading at the sink require metabolic energy. That local active work is distinct from the subsequent bulk movement through the sieve tube.

Reasoning cue: identify the current source and sink → identify the assimilate in phloem sap → trace the sieve-tube pathway → state why direction and loading demand are context-dependent.

Phloem is not simply a downward sugar tube and is not the same transport system as xylem. Source/sink status is functional and can change; pressure-driven mass flow is explained in the later card. Do not use ATP as if it directly pushes every assimilate along the whole plant. No image is needed for this card.

Companion cells load sucrose into phloem using a proton gradient

Companion cells load assimilates such as sucrose into phloem sieve tubes. The route may be symplastic and passive, or—when sucrose takes the apoplastic route—may use ATP-dependent proton pumping and H⁺–sucrose co-transport.

  1. Create the gradient: In a modified companion cell (transfer cell), a proton pump uses ATP to move H⁺ from the cytoplasm into the cell wall. This creates a high H⁺ concentration outside the cell.
  2. Use the gradient: H⁺ moves back down its concentration gradient through a co-transporter protein. The same transport step carries sucrose into the companion cell against sucrose’s concentration gradient.
  3. Enter the sieve tube: Sucrose moves from the companion cell into the associated sieve-tube element through plasmodesmata. Companion-cell membrane infoldings increase transport surface area, while many mitochondria supply ATP for the proton pump.
  4. Recognise the alternative: If sucrose uses the symplastic route, it can move through cytoplasm and plasmodesmata by diffusion; the exact route is not presented as universal.
  5. Pressure boundary: Loading raises the solute concentration in phloem and can lower its water potential, setting up water-entry and turgor consequences that the next mass-flow card connects to bulk movement. This card stops at loading/unloading rather than explaining the whole pressure-flow model.

Chain cue: ATP → proton pump → H⁺ gradient → H⁺–sucrose co-transport → companion cell → plasmodesmata → sieve tube.

Do not invent a named transporter or say ATP pushes every sucrose molecule along the entire plant. ATP powers the local proton pump; co-transport loads sucrose, while later mass flow is the long-distance process. Unloading occurs at sinks and may use apoplastic or symplastic routes, but its full pressure-flow consequence belongs to 4595. No image is generated for this card.

A hydrostatic pressure gradient drives phloem mass flow

Phloem sap moves in bulk from source to sink down a hydrostatic pressure gradient. Loading creates high pressure at the source; unloading helps create lower pressure at the sink.

  1. Sucrose is loaded into sieve tubes at a source, lowering phloem water potential.
  2. Water enters from nearby xylem by osmosis, raising hydrostatic/turgor pressure at the source.
  3. The pressure difference drives bulk movement of water and dissolved assimilates through the sieve tube towards the sink.
  4. Sucrose is unloaded at the sink for use or storage, raising phloem water potential.
  5. Water leaves, hydrostatic pressure falls, and the source-to-sink pressure gradient is maintained.
  6. Each sieve tube flows one way at a time, but different tubes may carry sap in opposite directions for different source-sink pairs.

Local active loading establishes a water-potential and pressure difference; the long-distance step is mass flow of the whole solution down hydrostatic pressure, not individual sucrose diffusion or direct ATP pushing.

Mass flow is bulk solution movement, and phloem is not globally one-way. ATP supports loading/unloading processes; it does not propel each assimilate molecule along the whole sieve tube.