Describe the mass flow hypothesis
1. Solutes actively transported from companion cells to sieve tubes at source
2. This lowers water potential inside sieve tubes, so water enters tubes by osmosis from xylem + companion cells
3. Creating high pressure inside sieve tubes at source end of phloem
4. At sink, solutes are removed from phloem to be used up
5. This increases water potential inside sieve tubes, so water leaves the tubes by osmosis
6. Lowering pressure inside sieve tubes
7. This creates a pressure gradient from source end to sink end
8. Gradient pushes solutes along sieve tubes towards the sink
9. At sink, solutes are used or stored