Short Term Studies of Nitrate Uptake into Barley Plants Using Ion-Specific Electrodes and ClO(3): II. Regulation of NO(3) Efflux by NH(4)

The influence of NH₄⁺, in the external medium, on fluxes of NO₃⁻ and K⁺ were investigated using barley (Hordeum vulgare cv Betzes) plants. NH₄⁺ was without effect on NO₃⁻ (³⁶ClO₃⁻) influx whereas inhibition of net uptake appeared to be a function of previous NO₃⁻ provision. Plants grown at 10 micromolar NO₃⁻ were sensitive to external NH₄⁺ when uptake was measured in 100 micromolar NO₃⁻. By contrast, NO₃⁻ uptake (from 100 micromolar NO₃⁻) by plants previously grown at this concentration was not reduced by NH₄⁺ treatment. Plants pretreated for 2 days with 5 millimolar NO₃⁻ showed net efflux of NO₃⁻ when roots were transferred to 100 micromolar NO₃⁻. This efflux was stimulated in the presence of NH₄⁺. NH₄⁺ also stimulated NO₃⁻ efflux from plants pretreated with relatively low nitrate concentrations. It is proposed that short term effects on net uptake of NO₃⁻ occur via effects upon efflux. By contrast to the situation for NO₃⁻, net K⁺ uptake and influx of ³⁶Rb⁺-labeled K⁺ was inhibited by NH₄⁺ regardless of the nutrient history of the plants. Inhibition of net K⁺ uptake reached its maximum value within 2 minutes of NH₄⁺ addition. It is concluded that the latter ion exerts a direct effect upon K⁺ influx.     

Short Term Studies of Nitrate Uptake into Barley Plants Using Ion-Specific Electrodes and ClO(3): I. Control of Net Uptake by NO(3) Efflux

A computer-controlled multichannel data acquisition system was employed to obtain continuous measurements of net nitrate or chlorate uptake by roots of intact barley plants (Hordeum vulgare cv Betzes) using nitrate-specific electrodes. Plants, previously grown in solutions maintained at 10 or 200 micromolar NO₃⁻ (low N or high N conditions, respectively), were provided with 200 micromolar NO₃⁻ or ClO₃⁻ during the uptake period. Initial rates of NO₃⁻ uptake were several times higher in low N plants than in high N plants. Within 10 min, uptake in the former plants declined to a new steady rate which was sustained for the remainder of the experiment. No such time-dependent changes were evident in the high N plants. Rates and patterns of net chlorate uptake exhibited almost identical dependence upon previous nitrate provision. NO₃⁻ (³⁶ClO₃⁻) influx, by contrast, appeared to be independent of NO₃⁻ pretreatment prior to influx determination. Nitrate efflux, estimated by several different methods, was strongly correlated with internal nitrate concentration of the roots.     

Nitrate Uptake into Barley (Hordeum vulgare) Plants : A New Approach Using ClO(3) as an Analog for NO(3)

Evidence is presented that chlorate is an extremely good analog for nitrate during nitrate uptake by intact barley (Hordeum vulgare cv. Fergus) roots. The depletion of ClO₃⁻ or NO₃⁻ from uptake media over 2 to 6 hours by seedlings was found to be dependent on combined NO₃⁻ plus ClO₃⁻ concentrations, and total anion uptake was equivalent at different NO₃⁻/ClO₃⁻ ratios. After loading barley seedlings with ³⁶ClO₃⁻ for 6 hours, kinetic parameters were derived from the analysis of efflux of [³⁶Cl] chlorate into unlabeled solution. On the basis of this analysis, the half times for exchange for the cytoplasmic and vacuolar phases were 17 minutes and 20 hours, respectively.     

Regulation of NO(3) Influx in Barley : Studies Using NO(3)

Short-term (10 minutes) measurements of plasmalemma NO₃⁻ influx (_oc) into roots of intact barley plants were obtained using ¹³NO₃⁻. In plants grown for 4 days at various NO₃⁻ levels (0.1, 0.2, 0.5 millimolar), _oc was found to be independent of the level of NO₃⁻ pretreatment. Similarly, pretreatment with Cl⁻ had no effect upon plasmalemma ¹³NO₃⁻ influx. Plants grown in the complete absence of ¹³NO₃⁻ (in CaSO₄ solutions) subsequently revealed influx values which were more than 50% lower than for plants grown in NO₃⁻. Based upon the documented effects of NO₃⁻ or Cl⁻ pretreatments on net uptake of NO₃⁻, these observations suggest that negative feedback from vacuolar NO₃⁻ and/or Cl⁻ acts at the tonoplast but not at the plasmalemma. When included in the influx medium, 0.5 millimolar Cl⁻ was without effect upon ¹³NO₃⁻ influx, but NH₄⁺ caused approximately 50% reduction of influx at this concentration.     

Effects of Altered Carbohydrate Availability on Whole-Plant Assimilation of NO(3)

An experiment was conducted to investigate the relative changes in NO₃⁻ assimilatory processes which occurred in response to decreasing carbohydrate availability. Young tobacco plants (Nicotiana tabacum [L.], cv NC 2326) growing in solution culture were exposed to 1.0 millimolar ¹⁵NO₃⁻ for 6 hour intervals during a normal 12 hour light period and a subsequent period of darkness lasting 42 hours. Uptake of ¹⁵NO₃⁻ decreased to 71 to 83% of the uptake rate in the light during the initial 18 hours of darkness; uptake then decreased sharply over the next 12 hours of darkness to 11 to 17% of the light rate, coincident with depletion of tissue carbohydrate reserves and a marked decline in root respiration. Changes also occurred in endogenous ¹⁵NO₃⁻ assimilation processes, which were distinctly different than those in ¹⁵NO₃⁻ uptake. During the extended dark period, translocation of absorbed ¹⁵N out of the root to the shoot varied rhythmically. The adjustments were independent of ¹⁵NO₃⁻ uptake rate and carbohydrate status, but were reciprocally related to rhythmic adjustments in stomatal resistance and, presumably, water movement through the root system. Whole plant reduction of ¹⁵NO₃⁻ always was limited more than uptake. The assimilation of ¹⁵N into insoluble reduced-N in roots remained a constant proportion of uptake throughout, while assimilation in the shoot declined markedly in the first 18 hours of darkness before stabilizing at a low level. The plants clearly retained a capacity for ¹⁵NO₃⁻ reduction and synthesis of insoluble reduced-¹⁵N even when ¹⁵NO₃⁻ uptake was severely restricted and minimal carbohydrate reserves remained in the tissue.     

Effect of exogenous and endogenous nitrate concentration on nitrate utilization by dwarf bean

The effect of the exogenous and endogenous NO₃⁻ concentration on net uptake, influx, and efflux of NO₃⁻ and on nitrate reductase activity (NRA) in roots was studied in Phaseolus vulgaris L. cv. Witte Krombek. After exposure to NO₃⁻, an apparent induction period of about 6 hours occurred regardless of the exogenous NO₃⁻ level. A double reciprocal plot of the net uptake rate of induced plants versus exogenous NO₃⁻ concentration yielded four distinct phases, each with simple Michaelis-Menten kinetics, and separated by sharp breaks at about 45, 80, and 480 micromoles per cubic decimeter.

Influx was estimated as the accumulation of ¹⁵N after 1 hour exposure to ¹⁵NO₃⁻. The isotherms for influx and net uptake were similar and corresponded to those for alkali cations and Cl⁻. Efflux of NO₃⁻ was a constant proportion of net uptake during initial NO₃⁻ supply and increased with exogenous NO₃⁻ concentration. No efflux occurred to a NO₃⁻-free medium.

The net uptake rate was negatively correlated with the NO₃⁻ content of roots. Nitrate efflux, but not influx, was influenced by endogenous NO₃⁻. Variations between experiments, e.g. in NO₃⁻ status, affected the values of K_m and V_max in the various concentration phases. The concentrations at which phase transitions occurred, however, were constant both for influx and net uptake. The findings corroborate the contention that separate sites are responsible for uptake and transitions between phases.

Beyond 100 micromoles per cubic decimeter, root NRA was not affected by exogenous NO₃⁻ indicating that NO₃⁻ uptake was not coupled to root NRA, at least not at high concentrations.

     

Simultaneous Influx and Efflux of Nitrate during Uptake by Perennial Ryegrass

Experiments with intact plants of Lolium perenne previously grown with ¹⁴NO₃⁻ revealed significant efflux of this isotopic species when the plants were transferred to solutions of highly enriched ¹⁵NO₃⁻. The exuded ¹⁴NO₃⁻ was subsequently reabsorbed when the ambient solutions were not replaced. When they were frequently replaced, continual efflux of the ¹⁴NO₃⁻ was observed. Influx of ¹⁵NO₃⁻ was significantly greater than influx of ¹⁴NO₃⁻ from solutions of identical NO₃⁻ concentration. Transferring plants to ¹⁴NO₃⁻ solutions after a six-hour period in ¹⁵NO₃⁻ resulted in efflux of the latter. Presence of Mg²⁺, rather than Ca²⁺, in the ambient ¹⁵NO₃⁻ solution resulted in a decidedly increased rate of ¹⁴NO₃⁻ efflux and a slight but significant increase in ¹⁵NO₃⁻ influx. Accordingly, net NO₃⁻ influx was slightly depressed. A model in accordance with these observations is presented; its essential features include a passive bidirectional pathway, an active uptake mechanism, and a pathway for recycling of endogenous NO₃⁻ within unstirred layers from the passive pathway to the active uptake site.     

Studies of the Regulation of Nitrate Influx by Barley Seedlings Using NO(3)

Using ¹³NO₃⁻, effects of various NO₃⁻ pretreatments upon NO₃⁻ influx were studied in intact roots of barley (Hordeum vulgare L. cv Klondike). Prior exposure of roots to NO₃⁻ increased NO₃⁻ influx and net NO₃⁻ uptake. This `induction' of NO<sub>3</sub><sup>−</sup> uptake was dependent both on time and external NO<sub>3</sub><sup>−</sup> concentration ([NO<sub>3</sub><sup>−</sup>]). During induction influx was positively correlated with root [NO<sub>3</sub><sup>−</sup>]. In the postinduction period, however, NO<sub>3</sub><sup>−</sup> influx declined as root [NO<sub>3</sub><sup>−</sup>] increased. It is suggested that induction and negative feedback regulation are independent processes: Induction appears to depend upon some critical cytoplasmic [NO<sub>3</sub><sup>−</sup>]; removal of external NO<sub>3</sub><sup>−</sup> caused a reduction of <sup>13</sup>NO<sub>3</sub><sup>−</sup> influx even though mean root [NO<sub>3</sub><sup>−</sup>] remained high. It is proposed that cytoplasmic [NO<sub>3</sub><sup>−</sup>] is depleted rapidly under these conditions resulting in `deinduction' of the NO₃⁻ transport system. Beyond 50 micromoles per gram [NO₃⁻], ¹³NO₃⁻ influx was negatively correlated with root [NO₃⁻]. However, it is unclear whether root [NO₃⁻] per se or some product(s) of NO₃⁻ assimilation are responsible for the negative feedback effects.     

Evidence for Cotransport of Nitrate and Protons in Maize Roots : II. Measurement of NO(3) and H Fluxes with Ion-Selective Microelectrodes

We report here on an investigation of net nitrate and proton fluxes in root cells of maize (Zea mays L.) seedlings grown without (noninduced) and with (induced) 0.1 millimolar nitrate. A microelectrode system described previously (IA Newman, LV Kochian, MA Grusak, WJ Lucas [1987] Plant Physiol 84: 1177-1184) was utilized to quantify net ionic fluxes from the measurement of electrochemical potential gradients for NO₃⁻ and H⁺ within the unstirred layer at the root surface. The nitrate-inducibility, pH dependence, and concentration dependence of net NO₃⁻ uptake correlated quite closely with the electrical response of maize roots to nitrate under the same experimental conditions (as described in PR McClure, LV Kochian, RM Spanswick, JE Shaff [1990] Plant Physiol 93: 281-289). Additionally, it was found that potential inhibitors of the plasmalemma H⁺-ATPase (vandate, diethylstilbestrol), which were shown to abolish the electrical response to NO₃⁻ (in PR McClure, LV Kochian, RM Spanswick, JE Shaff [1990] Plant Physiol 93: 281-289), dramatically inhibited NO₃⁻ absorption. These results strongly indicate that the NO₃⁻ electrical response is due to the operation of a NO₃⁻ transport system in the plasmalemma of maize root cells. Furthermore, the results from the H⁺-ATPase inhibitor studies indicate that the NO₃⁻ transport system is linked to the H⁺-ATPase, presumably as a NO₃⁻/H⁺ symport. This is further supported by the pH response of the NO₃⁻ transport system (inhibition at alkaline pH values) and the change in net H⁺ flux from a moderate efflux in the absence of NO₃⁻, to zero net H⁺ flux after exposing the maize root to exogenous nitrate. Although these results can be explained by other interpretations, the simplest model that fits both the electrical responses and the NO₃⁻/H⁺ flux data is a NO₃⁻/H⁺ symport with a NO₃⁻:H⁺ flux stoichiometry >1, whose operation results in the stimulation of the H⁺-ATPase due to the influx of protons through the cotransport system.     

Relative Content of NO(3) and Reduced N in Xylem Exudate as an Indicator of Root Reduction of Concurrently Absorbed NO(3)

It is unclear if the relative content of NO₃⁻ and reduced N in xylem exudate provides an accurate estimate of the percentage reduction of concurrently absorbed NO₃⁻ in the root. Experiments were conducted to determine whether NO₃⁻ and reduced N in xylem exudate of vegetative, nonnodulated soybean plants (Glycine max [L.] Merr., `Ransom') originated from exogenous recently absorbed ¹⁵NO₃⁻ or from endogenous ¹⁴N pools. Plants either were decapitated and exposed to ¹⁵NO₃⁻ solutions for 2 hours or were decapitated for the final 20 minutes of a 50-minute exposure to ¹⁵NO₃⁻ in the dark and in the light. Considerable amounts of ¹⁴NO₃⁻ and reduced ¹⁴N were transported into the xylem, but almost all of the ¹⁵N was present as ¹⁵NO₃⁻. Dissimilar changes in transport of ¹⁴NO₃⁻, reduced ¹⁴N and ¹⁵NO₃⁻ during the 2 hours of sap collection resulted in large variability over time in the percentage of total N in the exudate which was reduced N. Over a 20-minute period the rate of ¹⁵N transport into the xylem of decapitated plants was only 21 to 36% of the ¹⁵N delivered to the shoot of intact plants. Based on the proportion of total ¹⁵N which was found as reduced ¹⁵N in exudate and in intact plants in the dark, it was estimated that 5 to 17% of concurrently absorbed ¹⁵NO₃⁻ was reduced in the root. This was much less than the 38 to 59% which would have been predicted from the relative content of total NO₃⁻ and total reduced N in the xylem exudate.     

Effect of Phloem-Translocated Malate on NO(3) Uptake by Roots of Intact Soybean Plants

In soybean (Glycine max L. Merr. cv Kingsoy), NO₃⁻ assimilation in leaves resulted in production and transport of malate to roots (B Touraine, N Grignon, C Grignon [1988] Plant Physiol 88: 605-612). This paper examines the significance of this phenomenon for the control of NO₃⁻ uptake by roots. The net NO₃⁻ 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 NO₃⁻ 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 NO₃⁻ uptake, and excretion of HCO₃⁻ ions was probably released by malate decarboxylation. NO₃⁻ uptake rate increased when the supply of NO₃⁻ to the shoot was increased, and decreased when the activity of nitrate reductase in the shoot was inhibited by WO₄²⁻. We conclude that in situ, NO₃⁻ reduction rate in the shoot may control NO₃⁻ uptake rate in the roots via the translocation rate of malate in the phloem.     

Endogenous NO(3) in the Root as a Source of Substrate for Reduction in the Light

An experiment was conducted to investigate the reduction of endogenous NO₃⁻, which had been taken up by plants in darkness, during the course of the subsequent light period. Vegetative, nonnodulated soybean plants (Glycine max [L]. Merrill, `Ransom') were exposed to 1.0 millimolar <sup>15</sup>NO<sub>3</sub><sup>−</sup> for 12 hours in darkness and then returned to a solution containing 1.0 millimolar <sup>14</sup>NO<sub>3</sub><sup>−</sup> for the 12 hours `chase' period in the light. Another set of plants was exposed to ¹⁵NO₃⁻ during the light period to allow a direct comparison of contributions of substrate from the endogenous and exogenous sources. At the end of the ¹⁵NO₃⁻ exposure in the dark, 70% of the absorbed ¹⁵NO₃⁻ remained unreduced, and 83% of this unreduced NO₃⁻ was retained in roots. The pool of endogenous ¹⁵NO₃⁻ in roots was depleted at a steady rate during the initial 9 hours of light and was utilized almost exclusively in the formation of insoluble reduced-N in leaves. Unlabeled endogenous NO₃⁻, which had accumulated in the root prior to the previous dark period, also was depleted in the light. When exogenous ¹⁵NO₃⁻ was supplied during the light period, the rate of assimilation progressively increased, reflecting an increased rate of uptake and decreased accumulation of NO₃⁻ in the root tissue. The dark-absorbed endogenous NO₃⁻ in the root was the primary source of substrate for whole-plant NO₃⁻ reduction in the first 6 hours of the light period, and exogenous NO₃⁻ was the primary source of substrate thereafter. It is concluded that retention of NO₃⁻ in roots in darkness and its release in the following light period is an important whole-plant regulatory mechanism which serves to coordinate delivery of substrate with the maximal potential for NO₃⁻ assimilation in photosynthetic tissues.     

Assimilation of NO(3) Taken Up by Plants in the Light and in the Dark

An experiment was conducted to determine the extent that NO₃⁻ taken up in the dark was assimilated and utilized differently by plants than NO₃⁻ taken up in the light. Vegetative, nonnodulated soybean plants (Glycine max L. Merrill, `Ransom') were exposed to ¹⁵NO₃⁻ throughout light (9 hours) or dark (15 hours) phases of the photoperiod and then returned to solutions containing ¹⁴NO₃⁻, with plants sampled subsequently at each light/dark transition over 3 days. The rates of ¹⁵NO₃⁻ absorption were nearly equal in the light and dark (8.42 and 7.93 micromoles per hour, respectively); however, the whole-plant rate of ¹⁵NO₃⁻ reduction during the dark uptake period (2.58 micromoles per hour) was 46% of that in the light (5.63 micromoles per hour). The lower rate of reduction in the dark was associated with both substantial retention of absorbed ¹⁵NO₃⁻ in roots and decreased efficiency of reduction of ¹⁵NO₃⁻ in the shoot. The rate of incorporation of ¹⁵N into the insoluble reduced-N fraction of roots in darkness (1.10 micromoles per hour) was somewhat greater than that in the light (0.92 micromoles per hour), despite the lower rate of whole-plant ¹⁵NO₃⁻ reduction in darkness.

A large portion of the ¹⁵NO₃⁻ retained in the root in darkness was translocated and incorporated into insoluble reduced-N in the shoot in the following light period, at a rate which was similar to the rate of whole-plant reduction of ¹⁵NO₃⁻ acquired during the light period. Taking into account reduction of NO₃⁻ from all endogenous pools, it was apparent that plant reduction in a given light period (~13.21 micromoles per hour) exceeded considerably the rate of acquisition of exogenous NO₃⁻ (8.42 micromoles per hour) during that period. The primary source of substrate for NO₃⁻ reduction in the dark was exogenous NO₃⁻ being concurrently absorbed. In general, these data support the view that a relatively small portion (<20%) of the whole-plant reduction of NO₃⁻ in the light occurred in the root system.

     

Decrease of pH Gradients in Tonoplast Vesicles by NO(3) and Cl: Evidence for H-Coupled Anion Transport

Chloride or nitrate decreased a pH gradient (measured as [¹⁴C]methylamine accumulation) in tonoplast-enriched vesicles. The ΔpH decrease was dependent on the anion concentration. These effects are independent of the anion-sensitive H⁺-ATPase of the tonoplast, since the pH gradient (acid inside) was imposed artificially using a pH jump or a K⁺ gradient and nigericin. 4,4′-Diisothiocyano-2,2′-stilbene disulfonic acid partially prevented the decrease in pH gradient induced by Cl⁻. Two possible models to account for this anion-dependent decrease of ΔpH are: (a) H⁺ loss is accompanied by Cl⁻ or NO₃⁻ efflux from the vesicles via H⁺/anion symport systems on the tonoplast and (b) H⁺ loss is accompanied by Cl⁻ or NO₃⁻ uptake into the vesicles via H⁺/anion antiport systems. Depending on the requirements and conditions of the cell, these two systems would serve to either mobilize Cl⁻ and NO₃⁻ stored in the vacuole for use in the cytoplasm or to drive anions into the vacuole. Chloride or nitrate also decreased a pH gradient in fractions containing plasma membrane and Golgi, implying that these membranes may have similar H⁺-coupled anion transport systems.     

Regulation of NO(3) Assimilation by Anion Availability in Excised Soybean Leaves

The regulation of NO₃⁻ assimilation by xylem flux of NO₃⁻ was studied in illuminated excised leaves of soybean (Glycine max L. Merr. cv Kingsoy). The supply of exogenous NO₃⁻ at various concentrations via the transpiration stream indicated that the xylem flux of NO₃⁻ was generally rate-limiting for NO₃⁻ reduction. However, NO₃⁻ assimilation rate was maintained within narrow limits as compared with the variations of the xylem flux of NO₃⁻. This was due to considerable remobilization and assimilation of previously stored endogenous NO₃⁻ at low exogenous NO₃⁻ delivery, and limitation of NO₃⁻ reduction at high xylem flux of NO₃⁻, leading to a significant accumulation of exogenous NO₃⁻. The supply of ¹⁵NO₃⁻ to the leaves via the xylem confirmed the labile nature of the NO₃⁻ storage pool, since its half-time for exchange was close to 10 hours under steady state conditions. When the xylem flux of ¹⁵NO₃⁻ increased, the proportion of the available NO₃⁻ which was reduced decreased similarly from nearly 100% to less than 50% for both endogenous ¹⁴NO₃⁻ and exogenous ¹⁵NO₃⁻. This supports the hypothesis that the assimilatory system does not distinguish between endogenous and exogenous NO₃⁻ and that the limitation of NO₃⁻ reduction affected equally the utilization of NO₃⁻ from both sources. It is proposed that, in the soybean leaf, the NO₃⁻ storage pool is particularly involved in the short-term control of NO₃⁻ reduction. The dynamics of this pool results in a buffering of NO₃⁻ reduction against the variations of the exogenous NO₃⁻ delivery.     

Uptake and Assimilation of NO(3) and NH(4) by Nitrogen-Deficient Perennial Ryegrass Turf

Assimilation of NO₃⁻ and NH₄⁺ by perennial ryegrass (Lolium perenne L.) turf, previously deprived of N for 7 days, was examined. Nitrogen uptake rate was increased up to four- to five-fold for both forms of N by N-deprivation as compared to N-sufficient controls, with the deficiency-enhanced N absorption persisting through a 48 hour uptake period. Nitrate, but not NH₄⁺, accumulated in the roots and to a lesser degree in shoots. By 48 hours, 53% of the absorbed NO₃⁻ had been reduced, whereas 97% of the NH₄⁺ had been assimilated. During the early stages (0 to 8 hours) of NO₃⁻ uptake by N-deficient turf, reduction occurred primarily in the roots. Between 8 and 16 hours, however, the site of reduction shifted to the shoots. Nitrogen form did not affect partitioning of the absorbed N between roots (40%) and shoots (60%) but did affect growth. Compared to NO₃⁻, NH₄⁺ uptake inhibited root, but not shoot, growth. Total soluble carbohydrates decreased in both roots and shoots during the uptake period, principally the result of fructan metabolism. Ammonium uptake resulted in greater total depletion of soluble carbohydrates in the root compared to NO₃⁻ uptake. The data indicate that N assimilation by ryegrass turf utilizes stored sugars but is also dependent on current photosynthate.     

Effects of a localized supply of nitrate on NO3 - uptake rate and growth of roots in Lolium multiflorum Lam.

Roots of higher plants are usually exposed to varying spatial and temporal changes in concentrations of soil mineral nitrogen. A split root system was used to see how Lolium multiflorum Lam. roots adapt to such variations to cope with their N requirements. Plants were grown in hydroponic culture with their root system split in two spatially separated compartments allowing them to be fed with or without KNO₃. Net NO₃ ^- uptake, ¹⁵NO₃ ^- influx and root growth were studied in relation to time. Within less than 24 h following deprivation of KNO₃ to half the roots, the influx in NO₃ ^- fed roots was observed to increase (about 200% of the influx measured in plant uniformly NO₃ ^- supplied control plant) thereby compensating the whole plant for the lack of uptake by the N deprived roots. Due to the large NO₃ ^- concentrations in the roots, the NO₃ ^- efflux was also increased so that the net uptake rate increased only slightly (35% maximum) compared with the values obtained for control plants uniformly supplied with NO₃ ^-. This increase in net NO₃ ^- uptake rate was not sufficient to compensate the deficit in N uptake rate of the NO₃ ^- deprived split root in the short term. Over a longer period (>1 wk), root growth of the part of the root system locally supplied with NO₃ ^- was stimulated. An increase in root growth was mainly responsable for the greater uptake of nitrate in Lolium multiflorum so that it was able to fully compensate the deficit in N uptake rate of the NO₃ ^- deprived split root.     

Studies of the Uptake of Nitrate in Barley: I. Kinetics of NO(3) Influx

¹³NO₃⁻ was used to investigate patterns of NO₃⁻ influx into roots of barley plants (Hordeum vulgare L. cv Klondike) previously grown with (`induced') or without (`uninduced') a source of external NO₃⁻ ([NO₃⁻]₀). In both induced and uninduced plants, ¹³NO₃⁻ influx was biphasic in the range from 0.005 to 50 moles per cubic meter [NO₃⁻]₀. In the low concentration range (<1 mole per cubic meter for induced plants and <0.3 mole per cubic meter for uninduced plants), influx was saturable and V_max and K_m values for influx either increased or decreased according to NO₃⁻ pretreatment. By contrast, ¹³NO₃⁻ influx in the high concentration range revealed a strictly linear concentration dependence. These fluxes appeared to be mediated by a constitutive, rather than an inducible, transport system.     

Intracellular pH Regulation during NO(3) Assimilation in Shoot and Roots of Ricinus communis

Ricinus communis L. was used to test the Dijkshoorn-Ben Zioni hypothesis that NO₃⁻ uptake by roots is regulated by NO₃⁻ assimilation in the shoot. The fate of the electronegative charge arising from total assimilated NO₃⁻ (and SO₄²⁻) was followed in its distribution between organic anion accumulation and HCO₃⁻ excretion into the nutrient solution. In plants adequately supplied with NO₃⁻, HCO₃⁻ excretion accounted for about 47% of the anion charge, reflecting an excess nutrient anion over cation uptake. In vivo nitrate reductase assays revealed that the roots represented the site of about 44% of the total NO₃⁻ reduction in the plants. To trace vascular transport of ionic and nitrogenous constituents within the plant, the composition of both xylem and phloem saps was thoroughly investigated. Detailed dry tissue and sap analyses revealed that only between 19 and 24% of the HCO₃⁻ excretion could be accounted for from oxidative decarboxylation of shoot-borne organic anions produced in the NO₃⁻ reduction process. The results obtained in this investigation may be interpreted as providing direct evidence for a minor importance of phloem transport of cation-organate for the regulation of intracellular pH and electroneutrality, thus practically eliminating the necessity for the Dijkshoorn-Ben Zioni recycling process.     

Influx,efflux and net uptake of nitrate in Quercus suber seedlings

Nitrate influx, efflux and net nitrate uptake were measured for the slow-growing Quercus suber L. (cork-oak) to estimate the N-uptake efficiency of its seedlings when grown with free access to nitrate. We hypothesise that nitrate influx, an energetically costly process, is not very efficiently controlled so as to avoid losses through efflux, because Q. suber has relatively high respiratory costs for ion uptake. Q. suber seedlings were grown in a growth room in hydroponics with 1 mM NO₃ ^-. Seedlings were labelled with ¹⁵NO₃ ^- in nutrient solution for 5 min to measure influx and for 2 h for net uptake. Efflux was calculated as the difference between influx and net uptake. Measurements were made in the morning, afternoon and night. The site of nitrate reduction was estimated from the ratio of NO₃ ^- to amino acids in the xylem sap; the observed ratio indicated that nitrate reduction occurred predominantly in the roots. Nitrate influx was always much higher than net acquisition and both tended to be lower at night. High efflux occurred both during the day and at night, although the proportion of ¹⁵NO₃ ^- taken up that was loss through efflux was proportionally higher during the night. Efflux was a significant fraction of influx. We concluded that the acquisition system is energetically inefficient under the conditions tested. This revised version was published online in June 2006 with corrections to the Cover Date.