Water and solute transport along developing maize roots |
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Authors: | Jürgen Frensch Theodore C. Hsiao Ernst Steudle |
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Affiliation: | (1) Lehrstuhl für Pflanzenökologie, Universität Bayreuth, D-95440 Bayreuth, Germany;(2) Department of Land Air and Water Resources, Hydrologic Science, University of California, 95616 Davis, CA, USA |
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Abstract: | ![]() Hydraulic and osmotic properties were measured along developing maize (Zea mays L.) roots at distances between 15 and 465 mm from the root tip to quantify the effects of changes in root structure on the radial and longitudinal movement of water and solutes (ions). Root development generated regions of different hydraulic and osmotic properties. Close to the root tip, passive solute permeability (root permeability coefficient, Psr) was high and selectivity (root reflection coefficient, sr) low, indicative of an imperfect semipermeable root structure. Within the apical 100–150 mm, Psr decreased by an order of magnitude and sr increased significantly. Root hydraulic conductivity (Lpr) depended on the nature of the force (hydrostatic and osmotic). Osmotic Lpr was smaller by an order of magnitude than hydrostatic Lpr and decreased with increasing distance from the root tip. Throughout the root, responses in turgor of cortical cells and late metaxylem to step changes in xylem pressure applied to the base of excised roots were measured at high spatial resolution. The resulting profiles of radial and longitudinal propagation of pressure showed that the endodermis had become the major hydraulic barrier in older parts of the root, i.e. at distances from the apex ä 150 mm. Other than at the endodermis, no significant radial hydraulic resistance could be detected. The results permit a detailed analysis of the root's composite structure which is important for its function in collecting and translocating water and nutrients.Abbreviations and Symbols CPP cell pressure probe - IT root segments with intact tips; - Lpr root hydraulic conductivity - Lprh hydrostatic hydraulic conductivity of root - Lpro osmotic hydraulic conductivity of root - Papp hydrostatic pressure applied to cut end of root - Pc cell turgor - Pc, cor turgor of cortical cell - Pc,xyl turgor of late metaxylem vessel - Pro stationary root pressure - Pr0,seal stationary root pressure of sealed root segment - Psr solute permeability coefficient of root - RPP root pressure probe - TR root segments with tip removed - sr reflection coefficient of rootDedicated to Professor Andreas Sievers on the occasion of his retirement |
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Keywords: | Hydraulic conductivity Permeability coefficient Reflection coefficient Root development (solute transport, water transport) Turgor Zea |
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