Water Flow Across the Sieve-Tube Boundary: Estimating Turgor and Some Implications for Phloem Loading and Unloading. III. Phloem in the Leaf

The theory described in Part I of this series is applied hereto the loading of water and sucrose into the sieve-element-companion-cell(se-cc) complexes of minor veins. It is concluded that symplasticphloem loading cannot account for large increases in osmoticpressure from mesophyll to se-cc complex or the dilution ofsieve tube sap which is evident in leaves. By contrast, loadingfrom the free space into a symplastically isolated se-cc complexcan account for both these observations. Within the se-cc complex,sucrose and water will be transported from the companion cellsto the sieve elements by a pressure-driven flow of solutionthrough the cytoplasmic annuli of plasmodesmata. The associatedchanges in turgor and osmotic pressure are small, and so these-cc complex can be regarded as a single compartment with respectto water potential. The assumption that this compartment isat water flux equilibrium will lead to significant overestimatesof turgor gradients. However, if the trans-membrane water potentialdifference and the external water potential are taken into account,the correlation of such gradients with sieve-element dimensionsand / or transport velocities provides one means of testingthe Munch hypothesis of phloem transport Phloem, turgor, osmotic pressure, plasmodesmata, Münch hypothesis, Phloem loading