Mass flow is the primary mechanism by which sugars (mainly sucrose) are transported in the phloem of plants. This process relies on a hydrostatic pressure gradient established between a source (where sugars are produced) and a sink (where sugars are utilized or stored).
Hydrostatic Pressure Gradient
The movement of phloem sap is driven by differences in hydrostatic pressure. Hydrostatic pressure is the pressure exerted by a fluid at a given depth. In the phloem, the pressure is higher at the source and lower at the sink. This pressure difference creates the driving force for mass flow.
Process of Mass Flow
Loading at the Source: Sugars (primarily sucrose) are actively loaded into the sieve tubes at the source. This process requires energy and is often mediated by companion cells. The loading of sugars increases the solute concentration within the sieve tubes.
Water Uptake: The increased solute concentration lowers the water potential within the sieve tubes. This causes water to move into the sieve tubes by osmosis from the surrounding xylem.
Pressure Build-up at the Source: The influx of water increases the turgor pressure within the sieve tubes at the source, leading to a higher hydrostatic pressure.
Flow Through the Phloem: The high pressure at the source drives the phloem sap through the sieve tubes towards the sink. The sap moves due to the pressure gradient.
Unloading at the Sink: At the sink, sugars are actively unloaded from the sieve tubes. This process also requires energy and is often mediated by companion cells. The unloading of sugars increases the water potential within the sieve tubes.
Water Removal: Water moves out of the sieve tubes by osmosis into the surrounding sink tissues. This reduces the turgor pressure within the sieve tubes at the sink, leading to a lower hydrostatic pressure.
Mathematical Representation
The hydrostatic pressure ($P$) in a fluid is given by the equation:
$$P = \rho g h$$
where:
$\rho$ is the density of the fluid (phloem sap).
$g$ is the acceleration due to gravity.
$h$ is the height of the fluid column above a reference point.
In the context of mass flow, the pressure difference ($ \Delta P $) between the source and the sink is crucial for driving the movement of phloem sap.
Table Summarizing Mass Flow
Stage
Location
Process
Effect on Water Potential
Effect on Hydrostatic Pressure
Loading
Source
Active transport of sugars into sieve tubes
Decreases
Increases
Water Uptake
Source
Osmosis of water into sieve tubes
Increases
Increases
Flow
Phloem
Movement of phloem sap due to pressure gradient
N/A
N/A
Unloading
Sink
Active transport of sugars out of sieve tubes
Increases
Decreases
Water Removal
Sink
Osmosis of water out of sieve tubes
Decreases
Decreases
Suggested diagram: A diagram illustrating the source and sink of phloem, showing the direction of sugar movement and the hydrostatic pressure gradient.