Multiphasic Uptake of Sulfate by Barley Roots

Uptake of sulfate by excised barley roots increases upon their washing in aerated water or dilute CaCl₂ solutions. Washing increases the values for V_max and the sulfate concentrations required for transition between the lower phases, but the K_M-values remain essentially constant. At low sulfate concentrations, phase transitions do not occur in the absence of calcium or other divalent cations. These ions are about equally effective in enhancing short-term sulfate uptake. Phase transitions were not principally altered by sulfhydryl or protein reagents. These concentration-dependent transitions appear unrelated to temperature-dependent phase transitions as evidenced by similar multiphasic patterns at low and high temperature.     

Protection of Pyruvate,Pi Dikinase from Maize against Cold Lability by Compatible Solutes

Most C₄ species are chilling sensitive and certain enzymes like pyruvate,Pi dikinase of the C₄ pathway are also cold labile. The ability of cations and compatible solutes to protect maize (Zea mays) dikinase against cold lability was examined. The enzyme in desalted extracts at pH 8 from preilluminated leaves could be protected against cold lability (at 0°C) by the divalent cations Mn²⁺, Mg²⁺, and Ca²⁺. There was substantial protection by sulfate based salts but little protection by chloride based salts of potassium or ammonium (concentration 250 millimolar). The degree of protection against cold lability under limiting MgCl₂ (5 millimolar) was pH sensitive (maximum protection at pH 8), but independent of ionic strength (up to 250 millimolar by addition of KCl). In catalysis Mg²⁺ is required and Mn²⁺ could not substitute as a cofactor. Several compatible solutes reduced or prevented the cold inactivation of dikinase (in desalted extracts and the partially purified enzyme), including glycerol, proline, glycinebetaine and trimethylamine-N-oxide (TMAO). TMAO and Mg²⁺ had an additive effect in protecting dikinase against cold inactivation. TMAO could largely substitute for the divalent cation and addition of TMAO during cold treatment prevented further inactivation. Cold inactivation was partially reversed by incubation at room temperature; with addition of TMAO reversal was complete. The temperature dependence of inactivation at pH 8 and 3 millimolar MgCl₂ was evaluated by incubation at 2 to 17°C for 45 minutes, followed by assay at room temperature. At preincubation temperatures below 11°C there was a progressive inactivation which could be prevented by TMAO (450 millimolar). The results are discussed relative to possible effects of the solutes on the quaternary structure of this enzyme, which is known to dissociate at low temperatures.     

Kinetics of sulfate uptake by yeast

Uptake of sulfate by yeast requires the presence of a metabolic substrate and is dependent on the time during which the cells have been metabolizing in the absence of sulfate. At low concentrations of sulfate, uptake can be described by simple saturation kinetics. Uptake of sulfate is accompanied by a net proton influx of 3 H⁺ and an efflux of 1 K⁺ for each sulfate ion taken up. Divalent cations stimulate sulfate uptake at low concentrations of sulfate; the maximal rate of uptake is not significantly affected but $\text{K}{}_{\mathrm{<mtext>m</mtext>}}$ is lowered. Stimulation by divalent cations shows an optimum at a cation concentration of about 4 mM. Monovalent cations are less effective, trivalent cations are more effective in stimulating sulfate uptake. The results are qualitatively in accordance with the notion, that the effect of cations is due to an effect via the surface potential.     

Counter-ion dependence in salt-free,aqueous solutions of heparin

Chiroptical properties of heparin for various degrees of neutralization of the sulfate and carboxylic groups and for different counter-ions in salt-free aqueous solutions were investigated. Variations of optical rotation and ellipticity values at given wavelengths are compared to simultaneous pH and viscosity changes observed during the neutralization of heparin by sodium and calcium hydroxide. For Na⁺, variations of ellipticity at 210 nm are related to acid—base properties of uronic carboxylic groups. C.d. characteristics found for alkaline-earth counter-ions (Mg²⁺, Ca²⁺ and Ba²⁺), as compared to Na⁺, are assigned to effects of divalent ions on the ionization behavior of carboxylic groups. Among the divalent counter-ions considered, Ca²⁺ gave the strongest interaction with the heparin polyanion, but no specific complex formation was observed. O.r.d. and c.d. data are discussed on the basis of a randomly coiled structure for macromolecules composed of rigid, heterocyclic repeating-units that are independent of each other in so far as electronic transitions of chromophore groups contributing to optical activity are concerned.     

Kinetics of Ca2+ and Sr2+ uptake by yeast. Effects of pH,cations and phosphate

The uptake of Ca²⁺ and Sr²⁺ by the yeast Saccharomyces cerevisiae is energy dependent, and shows a deviation from simple Michaelis-Menten kinetics. A model is discussed that takes into account the effect of the surface potential and the membrane potential on uptake kinetics.The rate of Ca²⁺ and Sr²⁺ uptake is influenced by the cell pH and by the medium pH. The inhibition of uptake at low concentrations of Ca²⁺ and Sr²⁺ at low pH may be explained by a decrease of the surface potential.The inhibition of Ca²⁺ and Sr²⁺ uptake by monovalent cations is independent of the divalent cation concentration. The inhibition shows saturation kinetics, and the concentration of monovalent cation at which half-maximal inhibition is observed, is equal to the affinity constant of this ion for the monovalent cation transport system. The inhibition of divalent cation uptake by monovalent cations appears to be related to depolarization of the cell membrane.Phosphate exerts a dual effect on uptake of divalent cations: and initial inhibition and a secondary stimulation. The inhibition shows saturation kinetics, and the inhibition constant is equal to the affinity constant of phosphate for its transport mechanism. The secondary stimulation can only partly be explained by a decrease of the cell pH, suggesting interaction of intracellular phosphate, or a phosphorylated compound, with the translocation mechanism.     

Multiphasic Uptake of Amino Acids by Barley Roots

Concentration-dependence and other characteristics of uptake of ³H-labeled l -lysine, l -methionine and l -proline by excised roots of barley (Hordeum vulgare L.) were studied. Use of relatively short uptake and wash periods and low solute concentrations ensured good estimates of influx across the plasmalemma. Uptake in the range of 10^?7M– 6.3 × 10^?3M can be precisely represented by four or five phases of single, multiphasic mechanisms. The mechanisms appear to be relatively specific as judged from the competition by unlabeled analogues. Structural requirements for interaction of a compound with the uptake site for methionine are given, as are the effects of analogues on the phase pattern for this amino acid. There is no indication of separate uptake and transition sites for methionine or lysine. i.e. phase transitions seem in this case to be caused by binding of molecule(s) to the uptake site. Uptake, but not phase patterns, was highly pH-dependent. The optima were pH 5 for lysine, pH 3–5 (a broad peak) for methionine and about pH 5.5 for proline. Uptake of the three amino acids was strongly inhibited by 2,4-dinitrophenol. sulfhydryl reagents and deoxycholate.     

Mesophyll Resistances to SO(2) Fluxes into Leaves

Uptake of label from solutions containing ³⁵SO₂, H³⁵SO₃⁻ and ³⁵SO₃²⁻ into mesophyll protoplasts, vacuoles, and chloroplasts isolated from young barley leaves was measured at different pH values. Uptake was fast at low pH, when the concentration of SO₂ was high, and low at high pH, when the concentration of SO₂ was low. When the resistance (R) of plasmalemma, tonoplast, and chloroplast envelope to the penetration of SO₂ was calculated from rates of uptake of label, comparable values were obtained for the different biomembranes at low pH values. R was close to 8000 seconds per meter and permeability coefficients were close to 1.25 × 10⁻⁴ meters per second. Under these conditions R may describe resistance to SO₂ diffusion across a lipid bilayer. At higher pH values, R decreased. As R was calculated on the assumption that SO₂ is the only penetrating molecular species, the data suggest that carrier-mediated anion transport contributes to the uptake of sulfur at physiological pH values thereby decreasing apparent R_SO2. The contribution of anion transport appeared to be smaller for transfer across the plasmalemma than for transfer across the tonoplast. It was large for transfer across the chloroplast envelope. The phosphate translocator of the chloroplast envelope catalyzed uptake of SO₃²⁻ into chloroplasts at neutral pH. Uptake was decreased in the presence of high levels of phosphate or sulfate and by pyridoxal phosphate. SO₂ transfer into cells leads to the intracellular liberation of one or two protons, depending on pH and oxidizing conditions. When the divalent sulfite anion is exchanged across the chloroplast envelope, bisulfite formation results in proton uptake in the chloroplast stroma, whereas SO₂ uptake into chloroplasts lowers the stroma pH.     

pH modulation of the kinetics of rabbit jejunal,brush-border folate transport

Summary In jejunal brush-border membrane vesicles, an outwardly directed OH^– gradient (in>out) stimulates DIDS-sensitive, saturable folate (F) uptake (Schron, C.M. 1985.J. Clin. Invest. 76:2030–2033), suggesting carrier-mediated folate: OH^– exchange (or phenomenologically indistinguishable H⁺: folate cotransport). In the present study, the precise role of pH in the transport process was elucidated by examining F uptake at varying pH. For pH gradients of identical magnitude, F uptake (0.1 M) was greater at lower (pH_int/pH_ext: 5.5/4.5) compared with higher (6.5/5.5) pH ranges. In the absence of a pH gradient, internal Ftrans stimulated DIDS-sensitive³H-folate uptake only at pH6.0. Since stepwise increments ininternal pH (4.57.5; pH_ext=4.5) stimulated F uptake, an inhibitory effect of higherinternal pH was excluded. In contrast, with increasing external pH (4.356.5; pH_int=7.8), a 50-fold decrement in F uptake was observed (H⁺ K _m =12.8±1.2 M). Hill plots of these data suggest involvement of at least one H⁺ (OH^–) at low pH (monovalent F^– predominates) and at least 2 H⁺ (OH^–) at high pH (divalent F^–2 predominates). Since an inside-negative electrical potential did not affect F uptake at either pH_ext 4.55 or 5.8, transport of F^– and F^–2 is electroneutral. Kinetic parameters for F^– and F^–2 were calculated from uptake data at pH_ext 4.55 and 5.0. Comparison of predictedvs. experimentally determined kinetic parameters at pH_ext5.8 (K _m =1.33vs. 1.70 M;V _max=123.8vs. 58.0 pmol/mg prot min) suggest that increasing external pH lowers theV _max, but does not affect theK _m for carrier-mediated F transport. These data are consistent with similarK _i ^' s for sulfasalazine (competitive inhibitor) at pH_ext 5.35 and 5.8 (64.7 and 58.5 M, respectively). In summary, the jejunal F carrier mediates electroneutral transport of mono- and divalent F and is sensitive to external pH with a H⁺ K _m (or OH^– lC₅₀) corresponding to pH 4.89. External pH effects theV _max, but not theK _m for carriermediated F uptake suggesting a reaction mechanism involving a ternary complex between the outward-facing conformation of the carrier and the transported ions (F and either OH^– or H⁺),rather than competitive binding that is mutually exclusive.     

The stabilizing influence of divalent ions and Na+ on the di-decameric structure of Yoldia limatula hemocyanin

The stabilizing influence of Ca²⁺, Mg²⁺, Ba²⁺ and Na⁺ on the di-decameric structure of the hemocyanin of the bivalve, Yoldia limatula has been investigated by light-scattering molecular weight measurements and by analytical ultracentrifugation. The molecular weight (M_w) data, examined as a function of decreasing divalent ion and sodium ion concentrations at pH 8.0 and at a constant hemocyanin concentration of 0.10 g·l⁻¹, show biphasic transition profiles, with a sharp initial decline in M_w as the concentration of the stabilizing cations is reduced. The analysis of the molecular weight data is best described in terms of the four-species, di-decamer-decamer-dimer-monomer scheme of association-dissociation equilibria. About 25 to 35 bound divalent ions and about 10 bound Na⁺ ions per half-molecule or decamer are required in order to account for the initial step of the observed transitions. The subsequent transitions representing the decamer to dimer and the dimer to nonomer steps of the reaction account for the additional binding of three to four and two to four cations per dimer and per monomer, respectively. The relatively large number of divalent ions per decamer suggests strong ionic stabilization of the decamer to decamer contacts within the parent di-decameric assembly of Yoldia hemocyanin. This is consistent with earlier observations showing relatively few hydrophobic groups at the decamer to decamer contact areas.     

Evidence for proton/sulfate cotransport and its kinetics inLemna gibba G1

Sulfate uptake into duckweed (Lemna gibba G1) was studied by means of [³⁵S]sulfate influx and measurements of electrical membrane potential. Uptake was strongly regulated by the intracellular content of soluble sulfate. At the onset of sulfate uptake the membrane potential was transiently depolarized. Fusicoccin stimulated uptake up to 165% of the control even at pH 8. It is suggested that sulfate uptake is energized in the whole pH range by a 3H⁺/sulfate cotransport mechanism. Kinetics of sulfate uptake and sulfate-induced membrane depolarization in the concentration range of 5 M to 1 mM sulfate at pH 5.7 was best described by two Michaelis-Menten terms without any linear component. The second system had a lower affinity for sulfate and was fully active only at sufficiently high proton concentrations.Abbreviations c _o extracellular sulfate concentration - c _i intracellular sulfate concentration - E _m electrical membrane potential difference - E _m sulfate-induced, maximal membrane depolarization - electrochemical proton gradient - FW fresh weight     

pH Modulation of the kinetics of rabbit jejunal,brush-border folate transport

Summary In jejunal brush-border membrane vesicles, an out-wardly directed OH^– gradient (in>out) stimulates DIDS-sensitive, saturable folate (F) uptake (Schron, C.M., 1985).J. Clin. Invest. 76:2030–2033), suggesting carrier-mediated folate: OH^– exchange (or phenomenologically indistiguishable H⁺: folate cotransport). In the present study, the precise role of pH in the transport process was elucidated by examinin F uptake at varying pH. For pH gradients of identical magnitude, F uptake (0.1 M) was geater at lower (pH_int/pH_ext:5.5/4.5) compared with higher (6.5/5.5) pH ranges. In the absence of a pH gradient, internal Ftrans stimulated DIDS-sensitive³H-folate uptake only at pH6.0. Since setepwise increments ininternal pH (4.57.5; pH_ext=4.5) stimulated F uptake, an inhibitory effect of higherinternal pH was excluded. In contrast, with increasing external pH(4.356.5; pH_int=7.8), a 50-fold decrement in F uptake was observed (H⁺ K _m =12.8±1.2m). Hill plots of these data suggest involvement of at least one H⁺ (OH^–) at high pH (divalent F^–2 predominates). Since an inside-negative electrical potential did not affect F uptake at either pH_ext 4.55 or 5.8, transport of F^– and F^–2 is electroneutral. Kinetic parameters for F^– and F^–2 were calculated from uptake data at pH_ext 4.55 and 5.0. Comparision of predictedvs. experimentally determined kinetic parameters at pH_ext 5.8 (K _m =1.33vs. 1.70 m;V _max=12.8vs. 58.0 pmol/mg prot min) suggest that increasing external pH lowers theV _max, but does not affect thatK _m, for carrier-mediated F transport. These data are consistent with similarK _i's for sulfasalazine (competitive inhibitor) at pH_ext 5.35 and 5.8 (64.7 and 58.5 m, respectively). In summary, the jejunal F carrier mediates electroneutral transport of mono- and divalen F and is sensitive to extermal pH with a H⁺ K _m (or OH^– IC₅₀) corresponding to pH 4.89. External pH affects theV _max, but not theK _m for carriermediated F uptake suggesting a reaction mechanism involving a ternary complex between the outward-facing conformation of the carrier and the transported ions (F and either OH^– or H⁺) rather than competitive binding that is mutually exclusive.     

Biogeochemical changes at the sediment–water interface during redox transitions in an acidic reservoir: exchange of protons,acidity and electron donors and acceptors

Redox transitions induced by seasonal changes in water column O₂ concentration can have important effects on solutes exchange across the sediment–water interface in systems polluted with acid mine drainage (AMD), thus influencing natural attenuation and bioremediation processes. The effect of such transitions was studied in a mesocosm experiment with water and sediment cores from an acidic reservoir (El Sancho, SW Spain). Rates of aerobic organic matter mineralization and oxidation of reduced inorganic compounds increased under oxic conditions (OX). Anaerobic process, like Fe(III) and sulfate reduction, also increased due to higher O₂ availability and penetration depth in the sediment, resulting in higher regeneration rates of their corresponding anaerobic e^? acceptors. The contribution of the different processes to oxygen uptake changed considerably over time. pH decreased due to the precipitation of schwertmannite and the release of H⁺ from the sediment, favouring the dissolution of Al-hydroxides and hydroxysulfates at the sediment surface. The increase in dissolved Al was the main contributor to water column acidity during OX. Changes in organic matter degradation rates and co-precipitation and dissolution of dissolved organic carbon and nitrogen with redox-sensitive Fe(III) compounds affected considerably C and N cycling at the sediment–water interface during redox transitions. The release of NO₂^? and NO₃^? during the hypoxic period could be attributed to ammonium oxidation coupled to ferric iron reduction (Feammox). Considering the multiple effects of redox transitions at the sediment–water interface is critical for the successful outcome of natural attenuation and bioremediation of AMD impacted aquatic environments.     

Aluminium,boron and molybdenum availability and uptake by rice in acid sulfate soils

Although Al toxicity is believed to be a problem in acid sulfate soils cropped to rice (Oryza, sativa L.), little is known about the behavior of other trace metals such as B and Mo in these soils. The objectives of this study were to measure the availability of Al, B, and Mo in these soils, to determine what governs the availability of these metals and to investigate the relationships between metal availability and uptake by rice. Metal availability and uptake by rice were evaluated in 134 flooded acid sulfate soils in the Central Plains region of Thailand and in a growth chamber study using 50 of the same soils. Soil and plant metal analyses were conducted at the panicle differentiation stage of growth in both studies and in the soil prior to transplanting in the growth chamber study. Metal activities were determined with GEOCHEM. The mineral phases believed to be governing Al³⁺ activities were jurbanite under low pH conditions and amorphous Al(OH)₃ at high pH. The Al chemistry is believed to be intimately linked to the redox-pH cycle, which is driven by the monsoonal climate. Mortality of rice associated with Al toxicity was observed under field and growth chamber conditions. Interference in P uptake and/or assimilation was believed to be the mechanism of Al toxicity. Activities of B(OH) ₄ ^– and B(OH) ₃ ⁰ were found to be highly correlated to pH and ionic strength, respectively, with the latter being the dominant B ion found in these soils. Activities of MoO ₄ ^2– were positively correlated to pH and appeared to be controlled by wulfenite. Leaf Mo contents were found to be positively correlated with MoO ₄ ^2– activity.     

Uptake of sulfate,sulfite and thiosulfate by proton-anion symport in Desulfovibrio desulfuricans

pH changes and sulfide production upon addition of sulfate, sulfite or thiosulfate to non-buffered H₂-saturated cell suspensions of Desulfovibrio desulfuricans were studied by means of electrodes. The addition of these electron acceptors resulted in a rapid alkalinization of the suspension which was accompanied by sulfide production. At-2° C, alkalinization without immediate sulfide production could be obtained. After addition of ³⁵S-labelled sulfate at-2° C, the label was found to be concentrated 7,500-fold in the cells, while 2 protons per sulfate molecule had disappeared from the outer bulk phase. Alkalinization and sulfide production from micromolar electron acceptor additions depended on the transmembraneous proton gradient ( pH), and were reversibly inhibited in alkaline solution (pH>8.0) or by the protonophore carbonylcyanide m-chlorophenylhydrazone (CCCP). Protonophore-inhibited sulfide production from sulfite or thiosulfate could be restored if the cell membranes were permeabilized by the detergent cetyltrimethylammonium bromide (CTAB), or if downhill transport was made possible by the addition of electron acceptors at millimolar concentrations. Sulfate was not reduced under these conditions, presumably because the cells did not contain ATP for its activation. K⁺-and Na⁺-ionophores such as nigericin, valinomycin or monensin appeared to be of limited efficiency in D. desulfuricans. In most experiments, sulfate reduction was inhibited by the K⁺–H⁺ antiporter nigericin in the presence of K⁺, but not by the thiocyanate anion or the K⁺-transporter valinomycin. The results indicate that sulfate, sulfite and thiosulfate are taken up by proton-anion symport, presumably as undissociated acids with an electroneutral mechanism, driven by the transmembraneous pH gradient ( pH) or by a solute gradient. Kinetics of alkalinization and sulfide production in cells grown with different electron acceptors revealed that D. desulfuricans has different specific uptake systems for sulfate and thiosulfate, and obviously also for sulfite. It is proposed that the electron acceptor transport finally will not consume net energy during growth in buffered medium: The protons taken up during active electron acceptor transport leave the cell with the reduced end-product by simple passive diffusion of H₂S.Abbreviations CCCP carbonyl cyanide m-chlorophenylhydrazone - FCCP carbonyl cyanide p-trifluoromethoxy phenylhydrazone - CTAB cethyltrimethylammonium bromide     

Hymenolepis diminuta: Partial characterization of membrane-bound nucleotidase activities (ATPase and 5′-nucleotidase) in the isolated brush border membrane

Adenosine triphosphatase (ATPase; EC 3.6.1.3) and 5′-nucleotidase (5′-NTase; EC 3.1.3.5) activities of the isolated brush border membrane of Hymenolepis diminuta have been studied. The pH optimum for ATPase activity is 7.4, and divalent cations are necessary for maximum activity; no Na⁺-K⁺ activated ATPase is present in the isolated brush border membrane. ATPase activity is inhibited by molybdate and phosphorylated monosaccharides, but not by N-ethylmaleimide (NEM), p-chloromercuribenzoate (pCMB), or fluoride. The pH optimum for 5′-NTase activity is 9.6–10.2, and divalent cations are necessary for maximum activity. 5′-NTase activity is inhibited by molybdate at pH 9.6 and 7.4, and activated by NEM and pCMB and pH 9.6 and 7.4, respectively; fluoride has no effect on 5′-NTase activity. Solubilization of the brush border membrane fraction in 1% sodium dodecyl sulfate has no inhibitory action on either enzyme activity.     

Human kidney alpha-L-iduronidase: purification and characterization.

α-l-Iduronidase has been purified 25,000-fold from the soluble proteins of human kidney by chromatography on heparin-Sepharose, hydroxylapatite, and Bio-Gel P-100. The α-l-iduronidase activity is associated with 80% of the protein in the most purified preparation. It has a molecular weight of 60,000 ± 6500, determined by sedimentation equilibrium, and can be dissociated by reduction into subunits of molecular weight 31,000 ± 6500 determined by polyacrylamide gel electrophoresis in sodium dodecyl sulfate in the presence of dithiothreitol. It contains glucosamine and binds to concanavalin A. The pH optimum, K_m and V_max for two substrates, phenyl iduronide and [³H]anhydromannitol iduronide, were found to be 4.0, 1.05 mm, 16 μmol/mg protein/min, and 4·5, 9 mm and 270 μmol/mg protein/min, respectively. The enzyme is of the low uptake, noncorrective form with respect to fibroblasts cultured from the skin of patients with Hurler syndrome. It is inhibited by 10⁶ m p-chloromercuribenzoate and 10^?3 m Cu²⁺, but is not significantly affected by other divalent cations, EDTA, or sulfhydryl compounds. Antibodies to α-l-iduronidase have been raised in goats.     

Effect of pH on the transport of Krebs cycle intermediates in renal brush border membranes

Lowering extravesicular pH stimulated Na⁺-dependent citrate transport in renal brush border membrane vesicles: e.g., at pH_out = 5.5, the initial rate of citrate uptake was increased 10-fold compared to parallel control experiments at pH 7.5. The same experimental conditions had little effect on succinate uptake. The influence of pH on citrate transport is a product of the extravesicular H⁺ concentration; pH gradients did not potentiate the effects nor were proton gradients capable of driving transport in the absence of Na⁺. The effect of pH is adequately explained if only the mono- and divalent species of citrate (Cit^1?, Cit^2?) are considered acceptable substrates for transport. The stimulatory influence of pH on transport correlated quite well with pH-related increases in the concentrations of Cit^1? and Cit^2?, and over the same pH range [Cit^3?] was inversely related to citrate uptake. A model of the Na⁺-dependent dicarboxylate transport system is discussed in which three sodium ions are translocated per molecule of dicarboxylic acid.     

Die pH-Abhängigkeit der Aufnahme von H2PO 4 - , SO 4 = , Na+ und K+ und ihre gegenseitige Beeinflussung bei Ankistrodesmus braunii

Summary Ion uptake was studied using ³²P, ³⁵S, ²²Na and ⁴²K as tracers in synchronized cells of Ankistrodesmus, which were slightly starved with respect to the ions to be investigated. In the light and in the dark, phosphate uptake is maximal between pH 5.5 and 6.5. Whereas Na⁺ in comparison to K⁺ enhances phosphate uptake in the light (8 to 9-fold) and in the dark, Ca⁺⁺ exerts only a slightly stimulatory effect. The stimulation of phosphate binding by Na⁺ occurs rapidly, even after less than 5 sec of incubation, and also in the presence of an equimolar concentration of K⁺.The pH-dependence of Na⁺-uptake in the light and in the dark is comparable to a dissociation curve: Na⁺-uptake increases with decreasing extracellular H⁺-concentration and is inversely proportional to phosphate uptake in the absence of Na⁺. The light:dark ratio of Na⁺-uptake at pH 8 amounts to 7:1. Mere adsorption of Na⁺ is similarly dependent on the pH. K⁺ strongly competes with Na⁺-uptake, even at pH 8. K⁺-uptake proceeds in a quite different manner from Na⁺-uptake and has an optimum at pH 7.Sulfate is taken up linearly in a biphasic process as a function of time; the pH-optimum lies between pH 7.5 and 8. K⁺ but not Na⁺ slightly enhances sulfate uptake.The Na⁺-enhancement of phosphate uptake can be related neither to a sodium-potassium exchange pump nor to a photosynthesis-dependent ion-exchange reaction.The results suggest that the uptake of phosphate, Na⁺ and K⁺, and the influence of alkali cations on phosphate uptake, but not sulfate uptake, are strongly dependent on fixed charges of the plasmalemma or even of the cell wall. These fixed charges may even prevent an active ion uptake.     

Influence of culture density,pH, organic acids and divalent cations on the removal of nutrients and metals by immobilized Anabaena doliolum and Chlorella vulgaris

The potential of alginate-immobilized Anabaena doliolum and Chlorella vulgaris was assessed for removal of nutrients (NO _inf3 ^sup- and NH _inf4 ^sup+ ) and metals (Cr₂O _inf7 ^sup2- and Ni²⁺) at different biomass concentrations (0.05, 0.1, 0.25, 0.49 and 1.22 g dry wt l^-1) and pH values (4 to 10). Though uptake of all these substances was higher in concentrated algal beads (0.25, 0.49 and 1.22 g dry wt l^-1), their rate of uptake was significantly (P<0.001) lower than that of low (0.05 g dry wt l^-1) cell density beads. For A. doliolum, there was no significant difference in uptake rates for beads having densities of 0.05 and 0.1 g dry wt l^-1. Chlorella vulgaris, however, showed maximum efficiency at 0.1 g dry wt l^-1. Uptake of both the nutrients and the metals was maximal at pH 7 followed by pH 8, 6, 9, 10, 5 and 4. Of the different substances (organic acids and divalent cations) used, humic acid was most efficient in decreasing metal uptake. Mg²⁺ was, however, more efficient than Ca²⁺ in decreasing Ni²⁺ uptake. Immobilized algae with a cell density of 0.1 g dry wt l^-1 were the most efficient for nutrient and metal removal at pH 6 to 8.     

Multiphasic uptake of potassium by barley roots of low and high potassium content: Separate sites for uptake and transitions

In the range 10^?6M - 5 × 10^?2M uptake of K⁺ in excised roots of barley (Hordeum vulgare L. cv. Herta) with low and high K content could in both cases be represented by an isotherm with four phases. Uptake, especially in the range of the lower phases, was reduced in high K roots through decreases in V_max and increases in K_m. Similar data for other plants are also shown to be consistent with multiphasic kinetics. The concentrations at which transitions occurred were not affected by the K status, indicating the existence of separate uptake and transition sites. Uptake was markedly reduced in the presence of 10^?5M 2,4-dinitrophenol, especially at low K⁺ concentrations, but the isotherms remained multiphasic. This contraindicates major contributions from a non-carrier-mediated, passive flux. A tentative hypothesis for multiphasic ion uptake envisions a structure which changes conformation as a result of all-or-none changes in a separate transition site. The structure is “tight” at low external ion concentrations (low V_max. low K_m. active uptake, allosteric regulation) and “loose” at high concentrations (high V_max- high K_m- facilitated diffusion, no regulation).