In soybean (Glycine max L. Merr. cv Kingsoy), N03-assimilation in leaves resulted in production and transport of malate to roots (B Touraine, N Grignon, C Grignon [19881 Plant Physiol 88: 605-612). This paper examines the significance of this phenomenon for the control of N03-uptake by roots. The net N03-uptake rate by roots of soybean plants was stimulated by the addition of K-malate to the external solution. It was decreased when phloem translocation was interrupted by hypocotyl girdling, and partially restored by malate addition to the medium, whereas glucose was ineffective. Introduction of K-malate into the transpiration stream using a split root system resulted in an enrichment of the phloem sap translocated back to the roots. This treatment resulted in an increase in both N03-uptake and C excretion rates by roots. These results suggest that NO3-uptake by roots is dependent on the availability of shoot-borne, phloem-translocated malate. Shoot-to-root transport of malate stimulated N03-uptake, and excretion of HC03-ions was probably released by malate decarboxylation. N03-uptake rate increased when the supply of N03-to the shoot was increased, and decreased when the activity of nitrate reductase in the shoot was inhibited by W042-. We conclude that in situ, N03-reduction rate in the shoot may control N03-uptake rate in the roots via the translocation rate of malate in the phloem.in the xylem (4). A great amount of research has addressed the validity of this model, and more generally the fate of the anion charge released during 13,14,16,23,24). In a previous paper (21), we showed that the cycling scheme occurs in NO3--fed soybean (Glycine max L. Merr. cv Kingsoy) during the vegetative growth phase. The shoot was the site of more than 90% of total NO3-reduction, and most of the OH-equivalents that should have been produced during NO3-assimilation were excreted. Moreover, the excretion rate of OH-equivalents predicted by this calculation was equal to the monitored alkalinization rate of the nutrient solution, and it balanced well the difference between the uptake rates of anions and cations (21). Furthermore, the OH-equivalents excreted by the roots originated from the carboxylates produced in the shoot, which implies that the negative charge released by N03-reduction in the shoot was transported to the roots through the phloem.It has been proposed that the model described above plays a regulatory role: the translocation rate of carboxylates in the phloem would be a means by which N03-reduction rate in the shoot controls NO3-uptake rate by the roots (4, 8). The present paper deals with this hypothesis.
MATERIALS AND METHODSThe close relationship between NO3-uptake by roots and alkalinization of the rhizosphere is well documented (5,15,17,18,21