The Mass Flow Hypothesis Flashcards
The mass flow hypothesis was modelled by Ernst Münch in 1930. His simple model consisted of
Two partially permeable membranes containing solutions with different concentrations of ions (one dilute the other concentrated)
These two membranes were placed into two chambers containing water and were connected via a passageway
The two membranes were joined via a tube
As the membranes were surrounded by water, the water moved by osmosis across the membrane containing the more concentrated solution which forced the solution towards the membrane containing the more dilute solution (where water was being forced out of due to hydrostatic pressure)
The Mass Flow Hypothesis was the model initially used to
explain the movement of assimilates in the phloem tissue
Mass flow hypothesis step 1
Active transport is used to actively load the solutes (e.g. sucrose from photosynthesis) into the sieve tubes of the phloem at the source (e.g. the leaves)
This lowers the water potential inside the sieve tubes, so water enters the tubes by osmosis from the xylem and companion cells
This creates a high pressure inside the sieve tubes at the source end of the phloem
Mass flow step 2 t
At the sink end, solutes are removed from the phloem to be used up
This increases the water potential inside the sieve tubes, so water also leaves the tubes by osmosis
This lowers the pressure inside the sieve tubes
Mass flow step 3
The result is a pressure gradient from the source end to the sink end
This gradient pushes solutes along the sieve tubes to where they are needed