Early changes of water diffusional transfer in maize roots under the influence of water stress |
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Affiliation: | 1. Laboratoire Charles Coulomb (L2C) BioNanoNMRI UMR 5221 CNRS, Université Montpellier 2, France;2. Laboratoire de Technologie des Matériaux et de Génie des Procédés (LTMGP), Faculté des Sciences exactes, Université A. MIRA de Béjaïa, 06000 Béjaïa, Algérie;3. Institut Charles Gerhardt Montpellier, UMR 5253 CNRS UM2, Chimie Moléculaire et Organisation du Solide, Université Montpellier 2, France;4. INRA UR 1115 Plantes et Systèmes Horticoles, Domaine Saint-Paul, site Agroparc, 84914 Avignon, 8400 France;5. Medecine Nucléaire et IRM fonctionnelle, CHU de Montpellier, 34000 France;6. FKF-SDU, campusvej 55, DK5230 Odense, Danmark;7. CIRAD/INRIA/INRA, Virtual Plants Team, UMR AGAP, Avenue Agropolis, TA 108/02, 34398 Montpellier Cedex 5, France |
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Abstract: | The time dependent response of the hydrodynamic root system to PEG-induced water stress was studied in intact maize Zea mays L. seedlings at intervals varying from several seconds to 3 h by detecting diffusional water transfer with the use of pulsed NMR. In order to establish the contribution of water transfer through aquaporins in response to water stress, the transmembrane water transport in control roots and roots treated with aquaporin blocker was detected. Changes in diffusional water transfer under stress were shown to depend on the duration of osmotic treatment, and include the series of heterogeneous processes. A transient pulsed jump in diffusional water transfer detected several seconds after beginning the osmotic treatment is associated with the spread of the wave of hydraulic pressure along the root. It is proposed that early responses of the hydrodynamic system of maize roots to PEG-induced water stress lies in the unequal change in water permeability of the plasmalemma and tonoplast resulting from the changes in aquaporin activity and perhaps in the escalation of water transfer along the cell vacuome. |
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