1. At the source, sucrose is actively transported into the phloem by companion cells that use ATP to transport hydrogen ions into the surrounding tissue, creating a diffusion gradient, which causes the H+ ions to diffuse back into the companion cells via co-transporter proteins with sucrose molecules, causing the concentration of sucrose in the companion cells to increase.
2. sucrose lowers the water potential causing water to enter via osmosis from the xylem, increasing the hydrostatic pressure.
3. As a result water moves down the sieve tube from an area of high hydrostatic pressure to an area of low hydrostatic pressure.
4. Eventually, sucrose is removed from the sieve tube elements by diffusion or active transport into the surrounding cells, thus increasing the water potential in the sieve tube. This in turn means that water leaves the sieve tube by osmosis back into the xylem, and as a result reduces the pressure in the phloem at the sink.