Author： Plassard C. Meslem M. Souche G. Jaillard B.
Publisher： Springer Publishing Company
ISSN： 0032-079X
Source： Plant and Soil, Vol.211, Iss.1, 1999-01, pp. : 29-39
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Abstract
Two methods for measuring proton fluxes along intact maize roots grown with NH_4^+ or NO_3^- at pH 6.5 were compared. Videodensitometric measurement of changes in a pH-indicator dye by video camera was used to map pH around roots and determine the amounts of protons released by various root regions. This method was compared with potentiometric determination of the concentration of H^+ in the unstirred layer at the root surface using ion-selective microelectrodes. With NH_4^+ the roots released large amounts of H^+ in preferential regions where the rate of flux can reach 1.4 or even 2.5 nmol m^-1 s^-1. Videodensitometry indicated a first region of root acidification in the subapical zone, but this was more difficult to localize with microelectrodes. With NO_3^- both methods showed that the roots released small amounts of H^+ and that the apical region took up H^+ in the first 10 mm then sometimes released H^+ over the following 10 mm of root. The H^+ flux profiles obtained by both methods were in good agreement in terms of both order of magnitude of the fluxes and spatial differences along the root. These results suggest that videodensitometry, which is easier to use than potentiometry, can be used to screen different plant species or cultivars under various experimental conditions. The microelectrode technique is indispensable, however, for studying the underlying mechanisms of net H^+ fluxes.
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