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.     

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.     

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.     

Cation pretreatment effects on nitrate uptake, xylem exudate, and malate levels in wheat seedlings

Week-old wheat seedlings absorbed at least 40% NO₃⁻ from NaNO₃ when preloaded with K⁺ than when preloaded with Na⁺ or Ca²⁺. Cultures of Triticum vulgare L. cv. Arthur were grown for 5 days on 0.2 mm CaSO₄, pretreated for 48 hours with either 1 mm CaSO₄, K₂SO₄, or Na₂SO₄, and then transferred to 1 mm NaNO₃. All solutions contained 0.2 mm CaSO₄. Shoots of K⁺-preloaded plants accumulated three times more NO₃⁻ than shoots of the other two treatments. Initially, the K⁺-preloaded plants contained 10-fold more malate than either Na⁺- or Ca²⁺-preloaded seedlings. During the 48-hour treatment with NaNO₃, malate in both roots and shoots of the K⁺-preloaded seedlings decreased. Seedlings preloaded with K⁺ reduced 25% more NO₃⁻ than those preloaded with either Na⁺ or Ca²⁺. These experiments indicate that K⁺ enhanced NO₃⁻ uptake and reduction even though the absorption of K⁺ and NO₃⁻ were separated in time. Xylem exudate of K⁺-pretreated plants contained roughly equivalent concentrations of K⁺ and NO₃⁻, but exudate from Na⁺ and Ca²⁺-pretreated plants contained two to four times more NO₃⁻ than K⁺. Therefore K⁺ is not an obligatory counterion for NO₃⁻ transport in xylem.     

Nitrate uptake by roots as regulated by nitrate assimilation in the shoot of castor oil plants

Ricinus communis was used to test the Ben Zioni-Dijkshoorn hypothesis that NO₃ uptake by roots can be regulated by NO₃ assimilation in the shoot. The rate of the anion charge from assimilated NO₃⁻ (and SO₄²⁻) was followed in its distribution between organic acid anion accumulation and HCO₃⁻ efflux into the nutrient solution. In plants adequately supplied with NO₃⁻, HCO₃⁻ efflux accounted for between 56 and 63% of the anion charge. When the plants were subjected to a low NO₃ regime HCO₃⁻ excretion accounted for only 23% of the charge. A comparison of mature plants growing for a 10-day period at the two levels of NO₃ nutrition revealed that the uptake of NO₃⁻ at the higher level was increased 3-fold, whereas K uptake was unaltered. To trace ion movement within the plant, the ionic constituents of xylem and phloem sap were determined. In xylem sap these constituents were found to be predominantly K⁺, Ca²⁺, and NO₃⁻, whereas in the phloem sap they were mainly K⁺ and organic acid anions. Results have been obtained which may be interpreted as providing direct evidence of NO₃ uptake by roots regulated by NO₃ reduction in the tops, the process being facilitated by the recirculation of K⁺ in the plant.     

Potassium and Phosphate Uptake in Corn Roots: Further Evidence for an Electrogenic H/K Exchanger and an OH/Pi Antiporter

Evidence is presented that K⁺ uptake in corn root segments is coupled to an electrogenic H⁺/K⁺ -exchanging plasmalemma ATPase while phosphate uptake is coupled to an OH⁻/Pi antiporter. The plasmalemma ATPase inhibitor, diethylstilbestrol, or the stimulator, fusicoccin, altered K⁺ uptake directly and phosphate uptake indirectly. On the other hand, mersalyl, an OH⁻/Pi antiporter inhibitor, inhibited phosphate uptake instantly but only slightly affected K⁺ uptake. Collapse of the proton gradient across the membrane by (p-trifluoromethoxy) carbonyl cyanide phenylhydrazone resulted in immediate inhibition of K⁺ uptake but only later inhibited phosphate uptake. Changing the pH of the absorption solution had opposite effects on K⁺ and phosphate uptake. In addition, a 4-hour washing of corn root tissue induced a 5-fold increase in the rate of K⁺ uptake with little or no lag, but only a 2- to 3-fold increase in phosphate uptake with a 30- to 45-minute lag. Collectively these differences strongly support the coupling of an electrogenic H⁺/K⁺ -exchanging ATPase to an OH⁻/Pi antiporter in corn root tissue.     

Influence of the level of nitrate nutrition on ion uptake and assimilation, organic Acid accumulation, and cation-anion balance in whole tomato plants

Tomato plants (Lycopersicon esculentum L. var. Ailsa Craig) were grown in water culture in nutrient solution in a series of 10 increasing levels of nitrate nutrition. Using whole plant data derived from analytical and yield data of individual plant parts, the fate of anion charge arising from increased NO₃ assimilation was followed in its distribution between organic anion accumulation in the plant and OH⁻ efflux into the nutrient solution as calculated by excess anion over cation uptake. With increasing NO₃ nutrition the bulk of the anion charge appeared as organic anion accumulation in the plants. OH⁻ efflux at a maximum accounted for only 20% of the anion charge shift. The major organic anion accumulated in response to nitrate assimilation was malate. The increase in organic anion accumulation was paralleled by an increase in cation concentration (K⁺, Ca²⁺, Mg²⁺, Na⁺). Total inorganic anion levels (NO₃⁻, SO₄²⁻, H₂PO₄⁻, Cl⁻) were relatively constant. The effect of increasing NO₃ nutrition in stimulating organic anion accumulation was much more pronounced in the tops than in the roots.     

Electropotential in excised pea epicotyls

In contrast to intact etiolated pea seedling tissue (Pisum sativum L.), excised segments immersed in a complete nutrient solution show marked increases in ion content, largely of K⁺ and NO₃⁻, over a 72-hour period. During this time there is increase in cell electropotential difference, PD. During the initial 6 to 8 hours there is a lag in ion uptake; cell PD, however, increases rapidly from approximately −50 to −100 mv then increases more slowly. The increase in PD precedes and thus may be a prerequisite for the rapid ion accumulation phase. Cell PD increases in either water or nutrient solution but eventually reaches higher levels in the latter. Following water pretreatment of sufficient duration K⁺ accumulation shows no lag period. The lag phase noted here appears dissimilar to that of storage tissues.     

Effects of Helminthosporium carbonum Toxin on Absorption of Solutes by Corn Roots

Susceptible corn roots exposed to the host-selective toxin of Helminthosporium carbonum took up and retained more NO₃⁻, Na⁺, Cl⁻, 3-o-methylglucose, and leucine than did control roots. Stimulatory effects on uptake were more pronounced with freshly cut roots than with roots that were washed and aged. Solutes were accumulated against a concentration gradient, and toxin-treated tissues developed a steeper gradient than did control tissues. Toxin affected both the low and high affinity uptake systems for Na⁺ and Cl⁻. Toxin did not affect uptake of Na₂⁻, K⁺, Ca²⁺, phosphate ion (H₂PO₄⁻ and HPO₄⁻), SO₄⁻, and glutamic acid. No toxin-induced leakage of any solute tested was detected within 5 to 6 hr after initial exposure to toxin. The data suggest that toxin from H. carbonum does not cause the general plasma membrane derangement caused by other host-selective toxins. Instead, H. carbonum toxin may cause specific changes in characteristics of the plasmalemma, which result in increased uptake of certain solutes.     

Studies of Root Function in Zea mays: III. Xylem Sap Composition at Maximum Root Pressure Provides Evidence of Active Transport into the Xylem and a Measurement of the Reflection Coefficient of the Root

The cut ends of excised Zea mays roots were sealed to a pressure transducer and their root pressures recorded. These rose approximately hyperbolically to a maximum value of 4.21 ± 0.34 bar after 30 to 40 minutes. Xylem exudate could not be collected at this pressure since the flow rate was zero. Samples of exudate were collected at lower applied pressures (ΔP), however, and Δπ, the osmotic pressure difference between them and the solution bathing the root, was measured by freezing point depression. A plot of ΔP/Δπ against J_v/Δπ, where J_v is the volume flux, proved to be a straight line whose intercept, equal to σ, the reflection coefficient, was 0.853 ± 0.016. The maximum xylem concentrations of various chemical species were found by a similar extrapolative method and compared with those in the cell sap. This indicated that (a) Ca²⁺, Mg²⁺, NO₃²⁻, SO₄²⁻, and most amino acids move from the cells to the xylem down an electrochemical potential gradient; (b) relative to these ions H⁺, NH₄⁺, glutamine and asparagine are actively transported into the xylem; and (c) H₂PO₄⁻, and K⁺ are actively retained in the symplasm.     

Cadmium alteration of root physiology and potassium ion fluxes

Segments of oat (Avena sativa L.) roots which had been exposed to 1 millimolar CdSO₄ in quarter-strength Hoagland No. 1 solution exhibited decreased respiratory rates, ATP levels, membrane-bound ATPase activity, and reduced K⁺ fluxes. Respiration and ATP levels were decreased after a 2-hour treatment with 1 millimolar CdSO₄ to 65 and 75%, respectively, of control rates. A membrane-bound, Mg²⁺-dependent, K⁺-stimulated acid ATPase was rapidly inhibited to 12% of control activity in the presence of 1 millimolar CdSO₄. Potassium uptake into root segments was inhibited to 80% of control values after 30 minutes in the presence of CdSO₄. A 2-hour pretreatment of root segments with CdSO₄ inhibited K⁺ uptake to 15% of control values. Cytoplasmic K⁺ efflux was inhibited with 1 millimolar CdSO₄.

The rates and the degree of Cd²⁺ inhibition of the parameters listed above suggest that one of the first sites of Cd²⁺ action is the plasmalemma K⁺ carrier (ATPase) in oat roots.

     

Localization of inorganic ions by precipitative freeze dissolution

Summary A new method for localization of inorganic diffusible ions in tissue is introduced. It has been applied to localization of Tl⁺ and Rb⁺ in barley roots and is probably also suited for Cs⁺, Ca²⁺, Cl^–, Br^–, PO ₄ ^3– and perhaps K⁺. Its principle consists of dissolution of the ice from frozen tissue in a concentrated aqueous solution of a precipitating agent that is kept at a temperature just above its melting point.     

Studies on molybdenum absorption and transport in bean and rice

The patterns of molybdenum (MoO₄²⁻) absorption and transport were investigated in intact bean (Phaseolus vulgaris L.) and rice (Oryza sativa L. cv. I.R.8) plants. The mobility of MoO₄²⁻ absorbed by roots and by leaves was compared with that of a freely mobile element, Rb⁺. Although MoO₄²⁻ absorption by bean roots was nearly as high as that of Rb⁺, its transport to the shoot was considerably less. When MoO₄²⁻ was fed to one of the primary leaves, most of it was transported to the stem and root. Evidence obtained here showed that MoO₄²⁻ was mobile. Experiments with intact rice seedlings revealed large differences in the absorption and transport of MoO₄²⁻ between the plants grown in CaSO₄ and those in Hoagland solution. Molybdate uptake by excised rice roots was suggested to be an active process since it was greatly inhibited by a metabolic inhibitor. The presence of Mn²⁺, Zn²⁺, Cu²⁺, CI⁻, or SO₄²⁻ in the absorption medium reduced MoO₄²⁻ uptake which was markedly enhanced by the presence of Fe²⁺.     

Ion transport in isolated protoplasts from tobacco suspension cells: I. General characteristics

An investigation was conducted into the feasibility of using enzymically isolated protoplasts from suspension-cultured cells of Nicotiana glutinosa L. to study ion transport. Transport of K⁺ (⁸⁶Rb), ³⁶Cl⁻, H₂³²PO₄⁻ and ⁴⁵Ca²⁺ from 1 millimolar salt solutions was determined after separation of intact protoplasts from nonabsorbed tracers by centrifugation through a Ficoll step gradient. Influx of K⁺, Cl⁻, and H₂PO₄⁻ measured over a 30-minute period was reduced (up to 99%) by respiratory inhibitors such as 5 micrograms per milliliter oligomycin, 0.1 millimolar dinitrophenol, 0.1 millimolar cyanide, or N₂ gas. In contrast, Ca²⁺ influx was not tightly coupled to respiratory energy production. The influx of K⁺ was highest between pH 6.5 and 7.5 whereas the influx of H₂PO₄⁻ and Cl⁻ was greatest between pH 4.5 and 5.5. Influx of K⁺ and Cl⁻ was maximal at 35 and 45 C, respectively, and was almost completely inhibited below 10 C. Fusicoccin (0.01 millimolar) stimulated K⁺ influx by more than 200% but had no effect on the influx of either Cl⁻ or H₂PO₄⁻. Apparent H⁺ efflux, as measured by decrease in solution pH, was enhanced by K⁺, stimulated further by 0.01 millimolar fusicoccin, and inhibited by 0.1 millimolar dinitrophenol or 5 micrograms per milliliter oligomycin. The measured ionic fluxes into protoplasts were similar to those obtained with intact cultured cells. The results indicate that enzymic removal of the cell wall produced no significant alteration in the transport properties of the protoplast, and that it is feasible to use isolated protoplasts for studies on ion transport.     

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⁺.     

Effects of Catchment and Riparian Landscape Setting on Water Chemistry and Seasonal Evolution of Water Quality in the Upper Han River Basin,China

Six-year (2005–2010) evolution of water chemistry (Cl⁻, NO₃ ⁻, SO₄ ²⁻, HCO₃ ⁻, Na⁺, K⁺, Ca²⁺ and Mg²⁺) and their interactions with morphological properties (i.e., slope and area), land cover, and hydrological seasonality were examined to identify controlling factors and processes governing patterns of stream water quality in the upper Han River, China. Correlation analysis and stepwise multiple regression models revealed significant correlations between ions (i.e., Cl⁻, SO₄ ²⁻, Na⁺ and K⁺) and land cover (i.e., vegetation and bare land) over the entire catchment in both high- and low-flow periods, and in the buffer zone the correlation was much more stronger in the low-flow period. Catchment with steeper slope (>15°) was negatively correlated with major ions, largely due to multicollinearity of basin characteristics. Land cover within the buffer zone explained slightly less of major elements than at catchment scale in the rainy season, whereas in the dry season, land cover along the river networks in particular this within 100 m riparian zone much better explained major elements rather than this over the entire catchment. Anthropogenic land uses (i.e., urban and agriculture) however could not explain water chemical variables, albeit EC, TDS, anthropogenic markers (Cl⁻, NO₃ ⁻, SO₄ ²), Na⁺, K⁺ and Ca²⁺ significantly increased during 2005–2010, which was corroborated by principal component analyses (PCA) that indicated anthropogenic inputs. Observations demonstrated much higher solute concentrations in the industrial-polluted river. Our results suggested that seasonal evolution of water quality in combined with spatial analysis at multiple scales should be a vital part of identifying the controls on spatio-temporal patterns of water quality.     

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.     

Inhibition of anion transport in corn root protoplasts

The effects of several amino-reactive disulfonic stilbene derivatives and N-(4-azido-2-nitrophenyl)-2-aminoethylsulfonate on Cl⁻, SO₄²⁻, and inorganic phosphate (Pi) uptake in protoplasts isolated from corn root tissue were studied. 4-Acetamido-4′-isothiocyano-2,2′-stilbenedisulfonic acid, 4,4′-diisothiocyano-2,2′-stilbenedisulfonic acid, 4,4′-diamino-2,2′-stilbenedisulfonic acid, and NAP-taurine inhibited Cl⁻ and SO₄²⁻ but not Pi and K⁺ uptake in corn root protoplasts; whereas mersalyl inhibited Pi but not Cl⁻ or SO₄²⁻ uptake. The rate of uptake of all anions decreased with increasing external pH. In addition, these reagents markedly inhibited plasmalemma ATPase activity isolated from corn root tissue. Excised root segments were less sensitive to Cl⁻ and SO₄²⁻ transport inhibitors.     

Properties of Single K and Cl Channels in Asclepias tuberosa Protoplasts

Potassium and chloride channels were characterized in Asclepias tuberosa suspension cell derived protoplasts by patch voltage-clamp. Whole-cell currents and single channels in excised patches had linear instantaneous current-voltage relations, reversing at the Nernst potentials for K⁺ and Cl⁻, respectively. Whole cell K⁺ currents activated exponentially during step depolarizations, while voltage-dependent Cl⁻ channels were activated by hyperpolarizations. Single K⁺ channel conductance was 40 ± 5 pS with a mean open time of 4.5 milliseconds at 100 millivolts. Potassium channels were blocked by Cs⁺ and tetraethylammonium, but were insensitive to 4-aminopyridine. Chloride channels had a single-channel conductance of 100 ± 17 picosiemens, mean open time of 8.8 milliseconds, and were blocked by Zn²⁺ and ethacrynic acid. Whole-cell Cl⁻ currents were inhibited by abscisic acid, and were unaffected by indole-3-acetic acid and 2,4-dichlorophenoxyacetic acid. Since internal and external composition can be controlled, patch-clamped protoplasts are ideal systems for studying the role of ion channels in plant physiology and development.