The influence of ammonium and chloride on potassium and nitrate absorption by barley roots depends on time of exposure and cultivar

Net uptakes of K⁺ and NO₃⁻ were monitored simultaneously and continuously for two barley (Hordeum vulgare) cultivars, Prato and Olli. The cultivars had similar rates of net K⁺ and NO₃⁻ uptake in the absence of NH₄⁺ or Cl⁻. Long-term exposure (over 6 hours) to media which contained equimolar mixtures of NH₄⁺, K⁺, Cl⁻, or NO₃⁻ affected the cultivars very differently: (a) the presence of NH₄⁺ as NH₄Cl stimulated net NO₃⁻ uptake in Prato barley but inhibited net NO₃⁻ uptake in Olli barley; (b) Cl⁻ inhibited net NO₃⁻ uptake in Prato but had little effect in Olli; and (c) NH₄⁺ as (NH₄)₂SO₄ inhibited net K⁺ uptake in Prato but had little effect in Olli. Moreover, the immediate response to the addition of an ion often varied significantly from the long-term response; for example, the addition of Cl⁻ initially inhibited net K⁺ uptake in Olli barley but, after a 4 hour exposure, it was stimulatory. For both cultivars, net NH₄⁺ and Cl⁻ uptake did not change significantly with time after these ions were added to the nutrient medium. These data indicate that, even within one species, there is a high degree of genotypic variation in the control of nutrient absorption.     

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.     

The Influence of Nitrate and Chloride Uptake on Expressed Sap pH, Organic Acid Synthesis, and Potassium Accumulation in Higher Plants

The influence of NO₃⁻ uptake and reduction on ionic balance in barley seedlings (Hordeum vulgare, cv. Compana) was studied. KNO₃ and KCl treatment solutions were used for comparison of cation and anion uptake. The rate of Cl⁻ uptake was more rapid than the rate of NO₃⁻ uptake during the first 2 to 4 hours of treatment. There was an acceleration in rate of NO₃⁻ uptake after 4 hours resulting in a sustained rate of NO₃⁻ uptake which exceeded the rate of Cl⁻ uptake. The initial (2 to 4 hours) rate of K⁺ uptake appeared to be independent of the rate of anion uptake. After 4 hours the rate of K⁺ uptake was greater with the KNO₃ treatment than with the KCl treatment, and the solution pH, cell sap pH, and organic acid levels with KNO₃ increased, relative to those with the KCl treatment. When absorption experiments were conducted in darkness, K⁺ uptake from KNO₃ did not exceed K⁺ uptake from KCl. We suggest that the greater uptake and accumulation of K⁺ in NO₃⁻-treated plants resulted from (a) a more rapid, sustained uptake and transport of NO₃⁻ providing a mobile counteranion for K⁺ transport, and (b) the synthesis of organic acids in response to NO₃⁻ reduction increasing the capacity for K⁺ accumulation by providing a source of nondiffusible organic anions.     

Potassium Transport in Corn Roots : IV. Characterization of the Linear Component

A detailed examination was conducted on the linear, or first-order kinetic component for K⁺(⁸⁶Rb⁺) influx into root segments of both low- and high-salt grown corn seedlings (Zea mays [A632 × Oh 43]). In tissue from both low- and high-salt grown roots, replacement of Cl⁻ in the uptake solution by either SO₄²⁻, H₂PO₄⁻, or NO₃⁻ caused a significant (50-60%) and specific inhibition of the linear component of K⁺ influx. The anion transport inhibitor, 4,4′-diisothiocyano-2,2′-disulfonic acid, was found to abolish saturable Cl⁻ influx in corn roots while causing a significant (50-60%) and specific inhibition of the linear K⁺ uptake system; this inhibition was identical to that observed when Cl⁻ was replaced by other anions in the K⁺ uptake solution. Additionally, the quaternary ammonium cation, tetraethylammonium, which has been shown to block K⁺ channels in nerve axons, also caused a dramatic (70%) and specific inhibition of the linear component of K⁺ influx, but this was obtained only in high-salt roots. The reasons for this difference are discussed with respect to the differing abilities of low- and high-salt roots to absorb tetraethylammonium.

Our present results indicate that the linear component of K⁺ influx may occur by a passive process involving transmembrane K⁺ channels. Fluxes through these K⁺ channels may be partly coupled to a saturating Cl⁻ influx mechanism.

     

Calcium uptake by excised maize roots and interactions with alkali cations

Ca²⁺ uptake was studied in short-term experiments using 5-day-old excised maize roots. This tissue readily absorbs Ca²⁺, and inhibition by dinitrophenol and low temperature shows that the process is metabolically mediated. The uptake of Ca²⁺, like that of other cations, is influenced by the counter ion, the pH and concentration of the ambient solution, and the presence of other cations. The rate of uptake from various salts decreases in the following order: NO₃⁻ > Cl⁻ = Br⁻ > SO₄²⁻. K⁺ and H⁺ greatly interfere with Ca²⁺ absorption, while Li⁺ and Na⁺ have only slight effects.     

Nitrate Reduction in Roots as Affected by the Presence of Potassium and by Flux of Nitrate through the Roots

Dark-grown, detopped corn seedlings (cv. Pioneer 3369A) were exposed to treatment solutions containing Ca(NO₃)₂, NaNO₃, or KNO₃; KNO₃ plus 50 or 100 millimolar sorbitol; and KNO₃ at root temperatures of 30, 22, or 16 C. In all experiments, the accelerated phase of NO₃⁻ transport had previously been induced by prior exposure to NO₃⁻ for 10 hours. The experimental system allowed direct measurements of net NO₃⁻ uptake and translocation, and calculation of NO₃⁻ reduction in the root. The presence of K⁺ resulted in small increases in NO₃⁻ uptake, but appreciably stimulated NO₃⁻ translocation out of the root. Enhanced translocation was associated with a marked decrease in the proportion of absorbed NO₃⁻ that was reduced in the root. When translocation was slowed by osmoticum or by low root temperatures, a greater proportion of absorbed NO₃⁻ was reduced in the presence of K⁺. Results support the proposition that NO₃⁻ reduction in the root is reciprocally related to the rate of NO₃⁻ transport through the root symplasm.     

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.

     

Early effects of salinity on nitrate assimilation in barley seedlings

The effect of NaCl and Na₂SO₄ salinity on NO₃⁻ assimilation in young barley (Hordeum vulgare L. var Numar) seedlings was studied. The induction of the NO₃⁻ transporter was affected very little; the major effect of the salts was on its activity. Both Cl⁻ and SO₄²⁻ salts severely inhibited uptake of NO₃⁻. When compared on the basis of osmolality of the uptake solutions, Cl⁻ salts were more inhibitory (15-30%) than SO₄²⁻ salts. At equal concentrations, SO₄²⁻ salts inhibited NO₃⁻ uptake 30 to 40% more than did Cl⁻ salts. The absolute concentrations of each ion seemed more important as inhibitors of NO₃⁻ uptake than did the osmolality of the uptake solutions. Both K⁺ and Na⁺ salts inhibited NO₃⁻ uptake similarly; hence, the process seemed more sensitive to anionic salinity than to cationic salinity.

Unlike NO₃⁻ uptake, NO₃⁻ reduction was not affected by salinity in short-term studies (12 hours). The rate of reduction of endogenous NO₃⁻ in leaves of seedlings grown on NaCl for 8 days decreased only 25%. Nitrate reductase activity in the salt-treated leaves also decreased 20% but its activity, determined either in vitro or by the `anaerobic' in vivo assay, was always greater than the actual in situ rate of NO₃⁻ reduction. When salts were added to the assay medium, the in vitro enzymic activity was severely inhibited; whereas the anaerobic in vivo nitrate reductase activity was affected only slightly. These results indicate that in situ nitrate reductase activity is protected from salt injury. The susceptibility to injury of the NO₃⁻ transporter, rather than that of the NO₃⁻ reduction system, may be a critical factor to plant survival during salt stress.

     

Potential-dependent anion transport in tonoplast vesicles from oat roots

Potential-dependent anion movement into tonoplast vesicles from oat roots (Avena sativa L. var Lang) was monitored as dissipation of membrane potentials (Δψ) using the fluorescence probe Oxonol V. The potentials (positive inside) were generated with the H⁺-pumping pyrophosphatase, which is K⁺ stimulated and anion insensitive. The relative rate of ΔΨ dissipation by anions was used to estimate the relative permeabilities of the anions. In decreasing order they were: SCN⁻ (100) > NO₃⁻ (72) = Cl⁻ (70) > Br⁻ (62) > SO₄²⁻ (5) = H₂PO₄⁻ (5) > malate (3) = acetate (3) > iminodiacetate (2). Kinetic studies showed that the rate of Δψ dissipation by Cl⁻ and NO₃⁻, but not by SCN⁻, was saturable. The K_m values for Cl⁻ and NO₃⁻ uptake were about 2.3 and 5 millimolar, respectively, suggesting these anions move into the vacuole through proteinaceous porters. In contrast to a H⁺-coupled Cl⁻ transporter on the same vesicles, the potential-dependent Cl⁻ transport was insensitive to 4,4′-diisothiocyano-2,2′-stilbene disulfonate. These results suggest the existence of at least two different mechanisms for Cl⁻ transport in these vesicles. The potentials generated by the H⁺-translocating ATPase and H⁺-pyrophosphatase were nonadditive, giving support to the model that both pumps are on tonoplast vesicles. No evidence for a putative Cl⁻ conductance on the anion-sensitive H⁺-ATPase was found.     

Active extrusion of protons into deionized water by roots of intact maize plants

The investigations were focussed on the question as to whether roots of intact maize plants (Zea mays L. cv Blizzard) release protons into deionized H₂O. Plants in the six to seven leaf stage depressed the pH of deionized H₂O from 6 to about 4.8 during an experimental period of 4 hours. Only one-third of the protons released could be ascribed to the solvation of CO₂ in H₂O. The main counter anions released were Cl⁻, NO₃⁻, and SO₄²⁻. At low temperature (2°C), the H⁺ release was virtually blocked while a relatively high amount of K⁺ was released. The presence of K⁺, Na⁺, Ca²⁺, and Mg²⁺ in the external solution increased the H⁺ secretion significantly. Addition of vanadate to the outer medium inhibited the H⁺ release while fusicoccin had a stimulating effect. Substituting the nutrient solution of deionized H₂O resulted in a substantial increase of the membrane potential difference from −120 to −190 millivolts. The experimental results support the conclusion that the H⁺ release by roots of intact maize plants is an active process driven by a plasmalemmalocated ATPase. Since the net H⁺ release was not associated with a net uptake of K⁺, it is unlikely to originate from a K⁺/H⁺ antiport.     

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.     

Mechanism of Stimulation and Inhibition of Tonoplast H-ATPase of Beta vulgaris by Chloride and Nitrate

The H⁺-ATPase of tonoplast vesicles isolated from red beet (Beta vulgaris L.) storage tissue was studied with respect to the kinetic effects of Cl⁻ and NO₃⁻. N-Ethylmaleimide (NEM) was employed as a probe to investigate substrate binding and gross conformational changes of the enzyme. Chloride decreased the K_m of the enzyme for ATP but caused relatively little alteration of the V_max. Nitrate increased K_m only. Michaelis-Menten kinetics applied throughout with respect to ATP concentration. Nitrate yielded similar kinetics of inhibition in both the presence and absence of Cl⁻. Other monovalent anions that specifically increased the K_m of the ATPase for ATP were, in order of increasing K_i, SCN⁻, ClO₄⁻, and ClO₃⁻. Sulfate, although inhibitory, manifested noncompetitive kinetics with respect to ATP concentration. ADP, like NO₃⁻, was a competitive inhibitor of the ATPase but ADP and NO₃⁻ did not interact cooperatively nor did either interfere with the inhibitory action of the other. It is concluded that NO₃⁻ does not show competitive kinetics because of its stereochemical similarity to the terminal phosphoryl group of ATP. NEM was an irreversible inhibitor of the tonoplast ATPase. Both Mg·ADP and Mg·ATP protected the enzyme from inactivation by NEM but Mg·ADP was the more potent of the two. Chloride and NO₃⁻ exerted little or no effect on the protective actions of Mg·ADP and Mg·ATP suggesting that neither Cl⁻ nor NO₃⁻ are involved in substrate binding.     

Anion-Sensitive, H-Pumping ATPase of Oat Roots : Direct Effects of Cl, NO(3), and a Disulfonic Stilbene

To understand the mechanism and molecular properties of the tonoplast-type H⁺-translocating ATPase, we have studied the effect of Cl⁻, NO₃⁻, and 4,4′-diisothiocyano-2,2′-stilbene disulfonic acid (DIDS) on the activity of the electrogenic H⁺-ATPase associated with low-density microsomal vesicles from oat roots (Avena sativa cv Lang). The H⁺-pumping ATPase generates a membrane potential (Δψ) and a pH gradient (ΔpH) that make up two interconvertible components of the proton electrochemical gradient (μh⁺). A permeant anion (e.g. Cl⁻), unlike an impermeant anion (e.g. iminodiacetate), dissipated the membrane potential ([¹⁴C]thiocyanate distribution) and stimulated formation of a pH gradient ([¹⁴C]methylamine distribution). However, Cl⁻-stimulated ATPase activity was about 75% caused by a direct stimulation of the ATPase by Cl⁻ independent of the proton electrochemical gradient. Unlike the plasma membrane H⁺-ATPase, the Cl⁻-stimulated ATPase was inhibited by NO₃⁻ (a permeant anion) and by DIDS. In the absence of Cl⁻, NO₃⁻ decreased membrane potential formation and did not stimulate pH gradient formation. The inhibition by NO₃⁻ of Cl⁻-stimulated pH gradient formation and Cl⁻-stimulated ATPase activity was noncompetitive. In the absence of Cl⁻, DIDS inhibited the basal Mg,ATPase activity and membrane potential formation. DIDS also inhibited the Cl⁻-stimulated ATPase activity and pH gradient formation. Direct inhibition of the electrogenic H⁺-ATPase by NO₃⁻ or DIDS suggest that the vanadate-insensitive H⁺-pumping ATPase has anion-sensitive site(s) that regulate the catalytic and vectorial activity. Whether the anion-sensitive H⁺-ATPase has channels that conduct anions is yet to be established.     

Charge Balance in NO(3)-Fed Soybean: Estimation of K and Carboxylate Recirculation

Soybeans (Glycine max L. Merr., cv Kingsoy) were grown on media containing NO₃⁻ or urea. The enrichments of shoots in K⁺, NO₃⁻, and total reduced N (N_r), relative to that in Ca²⁺, were compared to the ratios K⁺/Ca²⁺,NO₃⁻/Ca²⁺, and N_r/Ca²⁺ in the xylem saps, to estimate the cycling of K⁺, and N_r. The net production of carboxylates (R⁻) was estimated from the difference between the sums of the main cations and inorganic anions. The estimate for shoots was compared to the theoretical production of R⁻ associated with NO₃⁻ assimilation in these organs, and the difference was attributed to export of R⁻ to roots. The net exchange rates of H⁺ and OH⁻ between the medium and roots were monitored. The shoots were the site of more than 90% of total NO₃⁻ reduction, and N_r was cycling through the plants at a high rate. Alkalinization of the medium by NO₃⁻-fed plants was interrupted by stem girdling, and not restored by glucose addition to the medium. It was concluded that the majority of the base excreted in NO₃⁻ medium originated from R⁻ produced in the shoots, and transported to the roots together with K⁺. As expected, cycling of K⁺ and reduced N was favoured by NO₃⁻ nutrition as compared to urea nutrition.     

Characteristics of Injury and Recovery of Net NO3? Transport of Barley Seedlings from Treatments of NaCl

The nature of the injury and recovery of nitrate uptake (net uptake) from NaCl stress in young barley (Hordeum vulgare L, var CM 72) seedlings was investigated. Nitrate uptake was inhibited rapidly by NaCl, within 1 minute after exposure to 200 millimolar NaCl. The duration of exposure to saline conditions determined the time of recovery of NO₃⁻ uptake from NaCl stress. Recovery was dependent on the presence of NO₃⁻ and was inhibited by cycloheximide, 6-methylpurine, and cerulenin, respective inhibitors of protein, RNA, and sterol/fatty acid synthesis. These inhibitors also prevented the induction of the NO₃⁻ uptake system in uninduced seedlings. Uninduced seedlings exhibited endogenous NO₃⁻ transport activity that appeared to be constitutive. This constitutive activity was also inhibited by NaCl. Recovery of constitutive NO₃⁻ uptake did not require the presence of NO₃⁻.     

Electrodiffusion,Barrier, and Gating Analysis of DIDS-insensitive Chloride Conductance in Human Red Blood Cells Treated with Valinomycin or Gramicidin

Current-voltage curves for DIDS-insensitive Cl⁻ conductance have been determined in human red blood cells from five donors. Currents were estimated from the rate of cell shrinkage using flow cytometry and differential laser light scattering. Membrane potentials were estimated from the extracellular pH of unbuffered suspensions using the proton ionophore FCCP. The width of the Gaussian distribution of cell volumes remained invariant during cell shrinkage, indicating a homogeneous Cl⁻ conductance among the cells. After pretreatment for 30 min with DIDS, net effluxes of K⁺ and Cl⁻ were induced by valinomycin and were measured in the continued presence of DIDS; inhibition was maximal at ∼65% above 1 μM DIDS at both 25°C and 37°C. The nonlinear current-voltage curves for DIDS-insensitive net Cl⁻ effluxes, induced by valinomycin or gramicidin at varied [K⁺]_o, were compared with predictions based on (1) the theory of electrodiffusion, (2) a single barrier model, (3) single occupancy, multiple barrier models, and (4) a voltage-gated mechanism. Electrodiffusion precisely describes the relationship between the measured transmembrane voltage and [K⁺]_o. Under our experimental conditions (pH 7.5, 23°C, 1–3 μM valinomycin or 60 ng/ml gramicidin, 1.2% hematocrit), the constant field permeability ratio P_K/P_Cl is 74 ± 9 with 10 μM DIDS, corresponding to 73% inhibition of P_Cl. Fitting the constant field current-voltage equation to the measured Cl⁻ currents yields P _Cl = 0.13 h⁻¹ with DIDS, compared to 0.49 h⁻¹ without DIDS, in good agreement with most previous studies. The inward rectifying DIDS-insensitive Cl⁻ current, however, is inconsistent with electrodiffusion and with certain single-occupancy multiple barrier models. The data are well described either by a single barrier located near the center of the transmembrane electric field, or, alternatively, by a voltage-gated channel mechanism according to which the maximal conductance is 0.055 ± 0.005 S/g Hb, half the channels are open at −27 ± 2 mV, and the equivalent gating charge is −1.2 ± 0.3.     

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.     

Organic Acids and Ionic Balance in Xylem Exudate of Wheat during Nitrate or Sulfate Absorption

Experiments were designed to study the importance of organic acids as counterions for K⁺ translocation in the xylem during excess cation uptake. A comparison was made of xylem exudate from wheat seedlings treated 72 hours with either 1.0 millimolar KNO₃ or 0.5 millimolar K₂SO₄, both in the presence of 0.2 millimolar CaSO₄. Exudation from KNO₃ plants had twice the volume and twice the K⁺ and Ca²⁺ fluxes or rate of delivery to shoots, as K₂SO₄ plants. Malate flux was 25% higher in K₂SO₄ than in KNO₃ exudate. Malate was the principal anion accompanying K⁺ or Ca²⁺ in K₂SO₄ treatment, while in the KNO₃ treatment, NO₃⁻ was the principal anion. The contribution of SO₄²⁻ was negligible in both treatments. In a second experiment, exudate was collected every 4 hours during the daytime throughout a 72-hour treatment with KNO₃. Malate was the only anion present in exudate at first, just after the CaSO₄ pretreatment had ended. Malate concentration decreased and NO₃⁻ concentration increased with time and these concentrations were negatively correlated. By 62 hours, NO₃⁻ represented 80% of exudate anions. K⁺ and NO₃⁻ concentrations in exudate were strongly correlated with K⁺ and NO₃⁻ uptake, respectively. The first 36 hours of absorption from KNO₃ solution resembled the continuous absorption of K₂SO₄, in that malate was the principal counterion for translocation of K⁺.     

Extra- and Intracellular pH and Membrane Potential Changes Induced by K, Cl, H(2)PO(4), and NO(3) Uptake and Fusicoccin in Root Hairs of Limnobium stoloniferum

Short-term ion uptake into roots of Limnobium stoloniferum was followed extracellularly with ion selective macroelectrodes. Cytosolic or vacuolar pH, together with the electrical membrane potential, was recorded with microelectrodes both located in the same young root hair. At the onset of chloride, phosphate, and nitrate uptake the membrane potential transiently decreased by 50 to 100 millivolts. During Cl⁻ and H₂PO₄⁻ uptake cytosolic pH decreased by 0.2 to 0.3 pH units. Nitrate induced cytosolic alkalinization by 0.19 pH units, indicating rapid reduction. The extracellular medium alkalinized when anion uptake exceeded K⁺ uptake. During fusicoccin-dependent plasmalemma hyperpolarization, extracellular and cytosolic pH remained rather constant. Upon K⁺ absorption, FC intensified extracellular acidification and intracellular alkalinization (from 0.31 to 0.4 pH units). In the presence of Cl⁻ FC induced intracellular acidification. Since H⁺ fluxes per se do not change the pH, recorded pH changes only result from fluxes of the stronger ions. The extra- and intracellular pH changes, together with membrane depolarization, exclude mechanisms as K⁺/A⁻ symport or HCO₃⁻/A⁻ antiport for anion uptake. Though not suitable to reveal the actual H⁺/A⁻ stoichiometry, the results are consistent with an H⁺/A⁻ cotransport mechanism.     

Effect of ammonium on nitrate utilization by roots of dwarf bean

The effect of exogenous NH₄⁺ on NO₃⁻ uptake and in vivo NO₃⁻ reductase activity (NRA) in roots of Phaseolus vulgaris L. cv Witte Krombek was studied before, during, and after the apparent induction of root NRA and NO₃⁻ uptake. Pretreatment with NH₄Cl (0.15-50 millimolar) affected neither the time pattern nor the steady state rate of NO₃⁻ uptake.

When NH₄⁺ was given at the start of NO₃⁻ nutrition, the time pattern of NO₃⁻ uptake was the same as in plants receiving no NH₄⁺. After 6 hours, however, the NO₃⁻ uptake rate (NUR) and root NRA were inhibited by NH₄⁺ to a maximum of 45% and 60%, respectively.

The response of the NUR of NO₃⁻-induced plants depended on the NH₄Cl concentration. Below 1 millimolar NH₄⁺, the NUR declined immediately and some restoration occurred in the second hour. In the third hour, the NUR became constant. In contrast, NH₄⁺ at 2 millimolar and above caused a rapid and transient stimulation of NO₃⁻ uptake, followed again by a decrease in the first, a recovery in the second, and a steady state in the third hour. Maximal inhibition of steady state NUR was 50%. With NO₃⁻-induced plants, root NRA responded less and more slowly to NH₄⁺ than did NUR.

Methionine sulfoximine and azaserine, inhibitors of glutamine synthetase and glutamate synthase, respectively, relieved the NH₄⁺ inhibition of the NUR of NO₃⁻-induced plants. We conclude that repression of the NUR by NH₄⁺ depends on NH₄⁺ assimilation. The repression by NH₄⁺ was least at the lowest and highest NH₄⁺ levels tested (0.04 and 25 millimolar).