We have examined the long-term effects of NO3− concentrations on NO3− (15NO3−) fluxes and cellular pool sizes in roots of intact 30-d-old wheat (Triticum aestivum cv. Courtot) grown hydroponically. Compartmental analysis was performed under steady-state conditions at five different levels of NO3− concentration (from 0.1 up to 5 mol m−3 taking into account metabolism and secretion into the xylem (Devienne et al., 1994). Nitrate and reduced nitrogen levels in the tissues were largely independent of external NO3− concentration although below 1.5 mol m−3 NO3−; concentration limited plant growth. In the chamber, marked diurnal variations in net uptake occurred and, in the light, higher NO3− concentrations yielded higher NO3− uptake rates. After transfer of the plants to the laboratory, the increase in net uptake linked to elevation of NO3−; concentrations was even larger (from 0.1 to 8.8μmol h−1 g−1 FW) as a result of a marked increase (× 10–11) in the unidirectional influx at the plasmalemma while NO3− efflux was less enhanced (× 4–5). Under these conditions, influx into the vacuole was also higher (× 2–4) while efflux from the vacuole was little affected (× 1–3). NO3− concentrations within the cell compartments were estimated under the clas sical assumptions. The vacuolar concentration was a little modified by NO3− availability whereas that in the cytosol increased from about 10 mol m−3 to about 20 mol m−3 indicating that (1) the absolute value for the cytosol was high and (2) it displayed only a small increase despite very large changes in NO3− fluxes. NO3− distribution within the cells did not seem to involve an active accumulation of NO3− in the vacuole.
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Devienne et al. (1994) studied this question.
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