Toward a Realistic Representation of Sucrose Transport in the Phloem of Plants
-
Published:2023-03
Issue:3
Volume:128
Page:
-
ISSN:2169-8953
-
Container-title:Journal of Geophysical Research: Biogeosciences
-
language:en
-
Short-container-title:JGR Biogeosciences
Author:
Nakad Mazen1ORCID,
Domec Jean‐Christophe23ORCID,
Sevanto Sanna4,
Katul Gabriel13ORCID
Affiliation:
1. Department of Civil and Environmental Engineering Duke University Durham NC USA
2. UMR 1391 INRA‐ISPA Bordeaux Sciences Agro Gradignan France
3. Nicholas School of the Environment Duke University Durham NC USA
4. Earth and Environmental Sciences Division Los Alamos National Laboratory Los Alamos NM USA
Abstract
AbstractThe significance of phloem hydrodynamics to plant mortality and survival, which impacts ecosystem‐scale carbon and water cycling, is not in dispute. The phloem provides the conduits for products of photosynthesis to be transported to different parts of the plant for consumption or storage. The Mnch pressure flow hypothesis (PFH) is the leading framework to mathematically represent this transport. It assumes that osmosis provides the necessary pressure differences to drive water and sucrose within the phloem. Mathematical models utilizing the PFH approximate the phloem by a relatively rigid slender semi‐permeable tube. However, the phloem consists of living cells that contract and expand in response to pressure fluctuations. The effect of membrane elasticity on osmotically driven sucrose front speed has rarely been considered and frames the scope here. Laboratory experiments were conducted to elucidate the elastic‐to‐plastic pressure‐deformation relation in membranes and their effect on sucrose front speeds. It is demonstrated that membrane elasticity acts to retard the sucrose front speed. The retardation emerges because of two effects: (a) part of the osmotic pressure is diverted to perform mechanical work to expand the membrane instead of pressurizing water, and (b) expansion of the membrane reduces the sucrose concentration driving osmotic potential due to volume increases and concomitant dilution effects. These results offer a novel perspective about the much discussed presence of sieve plates throughout the phloem acting as structural expansion dampers.
Funder
National Science Foundation
U.S. Department of Energy
Los Alamos National Laboratory
Publisher
American Geophysical Union (AGU)
Subject
Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry
Cited by
2 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献