Mass Flow of Sucrose through Sieve Tubes
As the sucrose and hydrogen ions are transported into the sieve tube elements, the sieve tubes now have a lower water potential.
This stimulates water movement from the xylem, into the phloem via osmosis - increasing the hydrostatic pressure within this sieve tube element.
Sucrose is then actively transported into the sieve tube elements (due to the hydrostatic pressure gradient) closer to the sink, decreasing the hydrostatic pressure in the other sieve tube elements.
From there, the sieve tube elements transport the sucrose into the sink via active transport. Water also moves into these sieve tubes via osmosis due to the water potential gradient.
The sink can then break down the sucrose in respiration or store the sucrose for later respiratory functions