Scaling Phloem Transport: Water Potential Equilibrium and Osmoregulatory Flow
Access StatusFull text of the requested work is not available in DASH at this time ("dark deposit"). For more information on dark deposits, see our FAQ.
MetadataShow full item record
CitationThompson, Matthew V., and N. Michele Holbrook. 2003. Scaling phloem transport: water potential equilibrium and osmoregulatory flow. Plant Cell and Environment 26 (9):1561-1577.
AbstractIn this work, the common assumption that phloem sap is in water potential equilibrium with the surrounding apoplast was examined. With a dimensionless model of phloem translocation that scales with just two dimensionless parameters ((R) over cap and (F) over cap), a 'map' of phloem behaviour as a function of these parameters was produced, which shows that the water potential equilibrium assumption ((R) over cap(F) over cap >> 1) is valid for essentially all realistic values of the relevant scales. When in water potential equilibrium, a further parameter reduction is possible that limits model dependence to a single parameter ((F) over cap), which describes the ratio of the solution's osmotic strength to its axial pressure drop. Due to the locally autonomous nature of individual sieve element/companion cell complexes, it is argued that long-distance integrative control is most efficient when is large ( that is, when the pressure drop is relatively small), permitting the sieve tube to regulate solute loading in response to global changes in turgor. This mode of transport has been called 'osmoregulatory flow.' Limitations on the pressure drop within the transport phloem could require that sieve tubes be shorter than the long axis of the plant, and thus arranged in series and hydraulically isolated from one another.
Citable link to this pagehttp://nrs.harvard.edu/urn-3:HUL.InstRepos:3043428
- FAS Scholarly Articles