Part 4: Water and Assimilate Movement Study Guide
Introduction to Water and Assimilate Movement
Translocation: This is the process by which assimilates, which are produced or taken up by a plant, are moved around the plant's system.
Assimilate: A substance that the plant takes up or accumulates. These are moved from the source to the sink.
Source: The location where assimilates are made or taken into the plant (e.g., a healthy, sunlit, fully expanded leaf).
Sink: The location where assimilates are needed, such as a developing flower, roots, or shoot apical meristems.
Usage and Storage: Assimilates are used to synthesize substances the plant needs immediately for growth and function, or they can be stored for future use.
Vascular Bundles: These are the plant's transport system, reaching throughout the entire organism. They can be imagined as bundles of straws winding through roots, stems, and leaves. They are composed of two primary tissues:
Xylem: Tissues responsible for transferring water () and minerals throughout the plant, primarily moving them upward from the roots.
Phloem: Tubes within the roots, stems, and leaves that facilitate the translocation of assimilates.
Signaling: Vascular bundles are also used to send signals throughout the plant. These signals may include:
Plant hormones.
Turgor (water pressure) signals.
Electrical signals.
Example of Signaling: Roots can signal drought stress to leaves by releasing abscisic acid into the vascular bundles. This triggers the closing of stomata to reduce water loss.
Assimilates: Types and Storage
Photoassimilates: These are specifically the sugars produced by leaves through the process of photosynthesis. Since energy is required for growth, the phloem carries these sugars to all growth areas including leaves, stems, roots, flowers, and fruits.
Mineral Assimilates: These are taken up from the soil through the roots. They enter the root along with water via osmosis.
Storage Methods:
Sucrose: Photoassimilates stored within the vacuoles of cells.
Starch: Photoassimilates stored over longer periods in the roots and stems.
Storage Structures: Some plants possess specialized structures for storage:
Thickened stems.
Crowns.
Tubers (e.g., starch-rich potatoes).
Sources and Sinks
Source Definition: A plant organ that produces more assimilates than it consumes. Example: A healthy, fully expanded, sunlit leaf.
Sink Definition: A plant organ that consumes more assimilates than it produces. Examples: Roots, shoot apical meristems (growth tips), new expanding leaves, developing flowers, seeds, and fruits.
Organ Transitions: Organs can change roles depending on their developmental stage. A young developing leaf is a sink because it requires large amounts of energy to grow; once it is fully grown and photosynthesizing, it becomes a source.
Assimilate Partitioning: The process by which the plant distributes assimilates among various organs based on their "sink strength."
Pressure Flow: The specific mechanism by which assimilates move from sources to sinks.
The Pressure Flow Hypothesis (Sugar Transport)
Translocation is facilitated by a six-stage pressure flow mechanism:
Stage 1: At the sources, sugar molecules are moved into phloem cells. This action increases the solute concentration within those cells.
Stage 2: Water () follows the sugars into the phloem cells via osmosis. The resulting increase in water volume creates high turgor pressure.
Stage 3: This high pressure forces the water and dissolved sugars along the phloem tubes toward the sinks.
Stage 4: At the sinks, sugars are actively removed from the phloem cells to be used for growth or storage.
Stage 5: As the solute concentration outside the phloem cells becomes higher than inside, water follows the sugars out of the phloem by osmosis.
Stage 6: The exit of water creates an area of lower pressure at the sink, which effectively "sucks" more sugars and water along the phloem from the high-pressure source area.
Sink Strength and Resource Competition
Sink Strength: This refers to the relative ability of a sink organ to attract assimilates. It varies throughout an organ's life depending on its growth rate or activity level.
Determinants of Sink Strength: An organ has high sink strength if it is very active (e.g., rapid growth) or if it is large (e.g., a massive root system).
Plant Investment: High resource investment in a sink is beneficial because that sink eventually provides critical functions:
Stability and structure (roots and stems).
Transitioning into a source (maturing leaves).
Reproduction (seeds, flowers, fruit).
Future energy storage (tubers).
Competition: Sinks compete for limited assimilates. In a young plant, the growing shoot and growing root compete for sugars. The plant must balance this distribution correctly; if one organ takes too many resources, the other suffers, and the plant's overall success is compromised. The shoot is necessary for producing future photoassimilates, while the root is essential for water and nutrient uptake.
Water Relations of Plant Cells
Movement Mechanisms: While water moves primarily through xylem tubes, it also moves between individual cells via osmosis.
Osmosis Definition: The movement of water across a semi-permeable membrane from an area of low solute concentration to an area of high solute concentration (alternatively: from high water concentration to low water concentration).
Directional Control: Plants can force osmosis in specific directions by actively pumping solutes across membranes. Water is naturally drawn to the area of higher solute concentration, allowing the plant to control internal water distribution.
Transpiration
Definition: The movement of water from the roots to the leaves against the force of gravity. Any water not utilized during photosynthesis evaporates through the stomata.
Process Steps:
Water enters roots via osmosis.
Water travels through xylem tubes, moving from higher water potential in the roots to lower water potential in the leaves.
Water evaporates through the stomata into the atmosphere.
Factors Affecting Transpiration Rates:
Temperature:
Increase in temperature leads to an increase in transpiration.
Decrease in temperature leads to a decrease in transpiration.
Soil Water Content:
Increase in soil water leads to an increase in transpiration.
Decrease in soil water leads to a decrease in transpiration.
Light Levels:
Increase in light levels leads to an increase in transpiration.
Decrease in light levels leads to a decrease in transpiration.
Wind Speed:
Increase in wind speed leads to an increase in transpiration.
Decrease in wind speed leads to a decrease in transpiration.
Humidity:
Increase in humidity leads to a decrease in transpiration.
Decrease in humidity leads to an increase in transpiration.