Preferential Assimilation of Ammonium Ions from Ammonium Nitrate Solutions by Apple Seedlings

Apple seedlings, Pyrus malus L., were grown in complete nutrient solutions containing nitrate, ammonium, or ammonium plus nitrate as the nitrogen source. Uptake of nitrogen was calculated from depletion measurements of the nutrient solutions and by using ¹⁵N labelled nitrate and ammonium salts. If the plants received nitrogen as ammonium only or as nitrate only, the amounts of nitrogen taken up were similar. However, if the seedlings were supplied with ammonium nitrate, the amount of nitrate-nitrogen assimilated was only half that of ammonium. Nevertheless, if ammonium and nitrate were supplied to a plant with a split-root system, with each root half receiving a different ion, the uptakes were similar. The possibility of independent inhibition by ammonium of both nitrate uptake and reduction in the roots is discussed.     

Conversion of Nitrite to Nitrate by Nitrite-resistant Yeasts

Candida species YK 11 and YK 92 and Geotrichum candidum YK 57, which were isolated as nitrite-resistants, converted nitrite in the culture medium to nitrate stoichiometrically during growth. The nitrite-oxidizing reaction was confirmed under aerobic conditions in the intact cell system with 15 mm nitrite, 150 mm glucose, and 100mm Tris-HCl buffer (pH 7.0). Glucose or other carbohydrate which supported the microbial growth was indispensable for the reaction. The rate of oxidation (0.9 ~ 1.3 × 10⁵ μg-N/g of YK 92 cells·day) and the maximum amounts of nitrate formed in the culture medium (200 mm, 2800 μg-N/ml) were much larger than those of other heterotrophic nitrifiers and almost the same as those of Nitrobacter.

The nitrite-oxidizing activity was demonstrated in many types of yeast species.     

Reduction of Nitrite and Nitrate to Ammonium on Pyrite

An important constraint on the formation of the building blocks of life in the Hadean is the availability of small, activated compounds such as ammonia (NH(3)) relative to its inert dinitrogen source. Iron-sulfur particles and/or mineral surfaces have been implicated to provide the catalytic active sites for the reduction of dinitrogen. Here we provide a combined kinetic, spectroscopic, and computational modeling study for an alternative source of ammonia from water soluble nitrogen oxide ions. The adsorption of aqueous nitrite (NO (2) (-) ) and nitrate (NO (3) (-) ) on pyrite (FeS(2)) and subsequent reduction chemistry to ammonia was investigated at 22°C, 70°C, and 120°C. Batch geochemical and in situ Attenuated Total Reflection - Fourier Transform Infrared (ATR-FTIR) spectroscopy experiments were used to determine the reduction kinetics to NH(3) and to elucidate the identity of the surface complexes, respectively, during the reaction chemistry of NO (2) (-) and NO (3) (-) . Density functional theory (DFT) calculations aided the interpretation of the vibrational data for a representative set of surface species. Under the experimental conditions used in this study, we detected the adsorption of nitric oxide (NO) intermediate on the pyrite surface. NH(3) production from NO (2) (-) occurred at 70 and 120°C and from NO (3) (-) occurred only at 120°C.     

Conversion of Biovolume Measurements of Soil Organisms, Grown Under Various Moisture Tensions, to Biomass and Their Nutrient Content

Direct microscopic measurements of biomass in soil require conversion factors for calculation of the mass of microorganisms from the measured volumes. These factors were determined for two bacteria, five fungi, and a yeast isolated from soil. Moisture stress conditions occurring in nature were simulated by growth in two media using shake cultures, on agar plates, and on membranes held at 34, 330, and 1,390 kPa of suction. The observed conversion factors, i.e., the ratio between dry weight and wet volume, generally increased with increasing moisture stress. The ratios for fungi ranged from 0.11 to 0.41 g/cm³ with an average of 0.33 g/cm³. Correction of earlier data assuming 80% water and a wet-weight specific gravity of 1.1 would require a conversion factor of 1.44. The dry-weight specific gravity of bacteria and yeasts ranged from 0.38 to 1.4 g/cm³ with an average of 0.8 g/cm³. These high values can only occur at 10% ash if no more than 50% of the cell is water, and a specific conversion factor to correct past data for bacterial biomass has not yet been suggested. The high conversion factors for bacteria and yeast could not be explained by shrinkage of cells due to heat fixing, but shrinkage during preparation could not be completely discounted. Moisture stress affected the C, N, and P content of the various organisms, with the ash contents increasing with increasing moisture stress. Although further work is necessary to obtain accurate conversion factors between biovolume and biomass, especially for bacteria, this study clearly indicates that existing data on the specific gravity and the water and nutrient content of microorganisms grown in shake cultures cannot be applied when quantifying the soil microbial biomass.     

Feedback Regulation of Nitrate Influx in Barley Roots by Nitrate,Nitrite, and Ammonium

The short-lived radiotracer 13N was used to study feedback regulation of nitrate influx through the inducible high-affinity transport system of barley (Hordeum vulgare L. cv Steptoe) roots. Both wild-type plants and the mutant line Az12:Az70 (genotype nar1a;nar7w), which is deficient in the NADH-specific and NAD(P)H-bispecific nitrate reductases (R.L. Warner, R.C. Huffaker [1989] Plant Physiol 91: 947-953) showed strong feedback inhibition of nitrate influx within approximately 5 d of exposure to 100 fmu]M nitrate. The result with the mutant, in which the flux of nitrogen into reduced products is greatly reduced, indicated that nitrate itself was capable of exercising feedback regulation upon its own influx. This conclusion was supported by the observation that feedback in wild-type plants occurred in both the presence and absence of L-methionine sulfoximine, an inhibitor of ammonium assimilation. Nitrite and ammonium were also found to be capable of exerting feedback inhibition upon nitrate influx, although it was not determined whether these ions themselves or subsequent metabolites were responsible for the effect. It is suggested that feed-back regulation of nitrate influx is potentially mediated through several nitrogen pools, including that of nitrate itself.     

The Assimilation of Nitrogen from Ammonium Salts and Nitrate by Fungi

1. The assimilation of inorganic nitrogen by Scopulariopsis brevicaulisand some physiologically similar species has been studied. Theirfailure to assimilate completely from ammonium sulphate hasbeen shown to be due to the fall in pH of the medium inducedby the initial uptake of ammonia.
2. Complete assimilation ofammonia takes place in the presenceof the neutral salts ofeach of thirteen organic acids investigated.The organic acidsact primarily through their buffering effectwhich preventsor slows down the fall in pH. They are not specificallyrequiredfor ammonia assimilation by these fungi and can beeffectivelyreplaced by certain inorganic buffers.
3. The influence of severalexternal factors on the rate of assimilationof ammonia, nitrate,and nitrite has been studied in S. brevicaulis.In correspondingconditions the mycelium assimilates ammoniamore rapidly thannitrate over a wide range of conditions.
4. Ammonia, even invery low concentration, completely suppressesnitrate assimilationwhen both sources of nitrogen are presenttogether. Nitrite,however, is assimilated simultaneously withammonia. It is thereforeconcluded that ammonia blocks the reductionof nitrate to nitriteby the fungus.
5. The suppression of nitrate assimilation inthe presence of ammoniais common to many mould fungi besidesS. brevicaulis, and isbelieved to have adaptive significancein natural habitats.
6. The nitrate-reducing and assimilatingsystem is formed, evenwhen S. brevicaulis is grown in completeabsence of nitrate(ammonia medium with organic acid). It comesinto action rapidlywhen the inhibiting effect of ammonia isremoved. Similarly,nitrate-grown mycelium is capable of assimilatingammonia atmaximal rate without any adaptive lag.

     

Stimulation of Nitrate Reductase by Light and Ammonium in Spirodela oligorrhiza

Light-enhanced nitrate reductase (NR) activity was 8 times greaterthan the dark control. Exogenous application of sucrose, glucoseand fructose increased the induction of NR in the light as wellas in the dark, whereas glycolate had no effect. DCMU [3-(3,4-dichlorophenyl)-1, 1-dimethyl urea] completely inhibited thedevelopment of NR in light. Sucrose, when added with DCMU, reversedthis inhibitory effect NR in vivo was more stable in light thanin darkness, the half-lives being 9.6 h and 6.4 h, respectively.The addition of sucrose did not change the half-life of NR ineither light or darkness. Ammonium, the end product of the inorganicnitrogen assimilatory pathway, stimulated the NR activity whereasamino acids decreased it. Key words: Spirodela oligorrhiza, nitrate reductase, ammonium, light     

Effects of Grazing by Flagellates on Competition for Ammonium between Nitrifying and Heterotrophic Bacteria in Chemostats

The enhanced mineralization of organic nitrogen by bacteriophagous protozoa is thought to favor the nitrification process in soils, in which nitrifying bacteria have to compete with heterotrophic bacteria for the available ammonium. To obtain more insight into this process, the influence of grazing by the bacteriovorous flagellate Adriamonas peritocrescens on the competition for limiting amounts of ammonium between the ammonium-oxidizing species Nitrosomonas europaea and the heterotrophic species Arthrobacter globiformis was studied in the presence of Nitrobacter winogradskyi in continuous cultures at dilution rates of 0.004 and 0.01 h^-1. The ammonium concentration in the reservoir was maintained at 2 mM, whereas the glucose concentration was increased stepwise from 0 to 7 mM. A. globiformis won the competition for limiting amounts of ammonium when the glucose concentration in the reservoirs increased, in agreement with previously described experiments in which the flagellates were not included. The numbers of nitrifying bacteria decreased as the numbers of heterotrophic bacteria rose with increasing glucose concentrations. Critical C/N ratios, i.e., ratios between glucose and ammonium in the reservoirs at which no nitrate was found in the culture vessels, of 12.5 and 10.5 were determined at dilution rates of 0.004 and 0.01 h^-1, respectively. Below these critical values, coexistence of the competing species was found. The numbers of nitrifying bacteria decreased more in the presence of flagellates than in their absence, presumably by selective predation on the nitrifying bacteria, either in the liquid culture or on the glass wall of the culture vessels. Despite this, the rate of nitrate production did not decrease more in the presence of flagellates than in their absence. This demonstrates that no correlation has to be expected between numbers of nitrifying bacteria and their activity and that a constant nitrification rate per cell cannot be assumed for nitrifying bacteria. Above the critical C/N ratios, low numbers of nitrifying bacteria were still found in the culture vessels, probably because of attachment of the nitrifying bacteria to the glass wall of the culture vessels. Like the numbers of heterotrophic bacteria, the numbers of flagellates increased when the glucose concentrations in the reservoirs increased. Numbers of 2 × 10⁵ and 12 × 10⁵ flagellates ml^-1 were found at 7 mM glucose at dilution rates of 0.004 and 0.01 h^-1, respectively. It was concluded that the critical C/N ratios were practically unaffected by the presence of protozoa. Although nitrate production rates were equal in the presence and absence of flagellates, the numbers of nitrifying bacteria decreased more strongly in their presence. This indicates a higher activity per nitrifying cell in the presence of flagellates.     

铵离子对不同基因型水稻吸收硝酸根离子的影响1

NH+4可在很短时间内影响两种不同水稻亚种吸收NO-3,即可以影响NO-3的最初跨膜运输.籼型稻在NH+4存在时对NO-3吸收有促进,而粳型稻NO-3吸收则明显减少.     

Promotion of Assimilation of Ammonium Ions by Simultaneous Application of Nitrate and Ammonium Ions in Radish Plants

When radish plants were grown in nutrient solutions that containedammonium ions (NH₄⁺) as the sole source of nitrogen, they grewpoorly and accumulated high levels of NH₄⁺ in their leaves.However, radish plants cultured in 5 mM NH₄⁺ plus 1 mM NO₃^–(a ratio of 5 : 1 in forms of nitrogen; referred to as 5:lmix-N)grew well and accumulated very low levels of NH₄⁺ in their leaves.After radish plants were cultured in solutions that containedNO₃^–, or NH₄⁺, or 5: lmix-N for a week, they were thensupplied with the same nitrogen source labeled with ¹⁵N forone day. The uptake of ¹⁵N from labeled NH₄⁺ into total nitrogenwas the highest in plants supplied with 5:1mix-N. These plantsconverted far fewer labeled NH₄⁺ into free NH₄⁺ than did NH₄⁺-fedplants, but converted many more labeled NH₄⁺ into the insolublefraction than did NH₄⁺- or NO₃^–-fed plants. The presence of a small amount of nitrate was shown to stimulatethe assimilation of ammonium ions and the synthesis of proteins. (Received October 26, 1988; Accepted January 24, 1989)     

Effects of Grazing by Flagellates on Competition for Ammonium between Nitrifying and Heterotrophic Bacteria in Chemostats

[This corrects the article on p. 1964 in vol. 58.].     

Regulation of Nitrate Uptake in Penicillium chrysogenum by Ammonium Ion

A nitrate uptake system is induced (along with nitrate reductase) when NH₄⁺-grown Penicillium chrysogenum is incubated with inorganic nitrate in synthetic medium in the absence of NH₄⁺. Nitrate uptake and nitrate reduction are probably in steady state in fully induced mycelium, but the ratios of the two activities are not constant during the induction period. Substrate concentrations of ammonium cause a rapid decay of nitrate uptake and nitrate reductase activity. The two activities are differentially inactivated (the uptake activity being more sensitive). Glutamine and asparagine are as effective as NH₄⁺ in suppressing nitrate uptake activity. Glutamate and alanine were about half as effective as NH₄⁺. Cycloheximide interferes with the NH₄⁺-induced decay of nitrate uptake activity. The ammonium transport system is almost maximally deinhibited (or derepressed) in nitrate-grown mycelium.     

Effects of Nitrogen Deficiency on the Absorption of Nitrate and Ammonium by Barley Plants

When young barley plants which had been supplied with nitratewere deprived of this source of N, an enhanced capacity forabsorption of either nitrate or ammonium ions developed, reachinga maximum in about 3 d under the particular experimental conditionsused. The net uptake rate of either nutrient was then approximatelythree times that in plants which had received nitrate throughout.Likewise, withholding external N from plants previously growingwith ammonium caused a 2.4-fold increase in their subsequentcapacity to absorb that ion, compared with control plants grownwith an uninterrupted ammonium supply. Accelerated nitrate uptakein N-starved plants was not accompanied by additional phosphateor sulphate absorption, but the plants had the capacity to absorbmore potassium, whether or not ammonium was also present inthe solution. Indirect evidence from analyses of root tissuesuggests that these responses to mild N-stress may depend onsome property of an N fraction which does not include nitrateor ammonium. Hordeum vulgare, barley, nitrogen, ammonium, nitrate, N-deficiency, absorption     

Growth and Preferences for Ammonium or Nitrate Uptake by Barley in Relation to Root Termperature

Barley plants (Hordewn vulgare L. cv. Atem) were grown fromseed for 28 d in flowing solution culture, during which timeroot temperature was lowered decrementally to 5?C. Plants werethen subjected to root temperatures of 3, 5, 7, 9, 11, 13, 17or 25 ?C, with common air temperature of 25/15 ?C (day/night).Changes in growth, plant total N, and NO₃^– levels, andnet uptake of NH₄⁺ and NO₃^– from a maintained concentrationof 10 mmol m^–3 NH₄NO₃ were measured over 14 d. Dry matterproduction increased 6-fold with increasing root temperaturebetween 3–25 ?C. The growth response was biphasic followingan increase in root temperature. Phase I, lasting about 5 d,was characterized by high root specific growth rates relativeto those of the shoot, particularly on a fresh weight basis.During Phase I the shoot dry weight specific growth rates wereinversely related to root temperature between 3–13 ?C.Phase 2, from 5–14 d, was characterized by the approachtowards, and/or attainment of, balanced exponential growth betweenshoots and roots. Concentrations of total N in plant dry matterincreased with root temperature between 3–25 ?C, moreso in the shoots than roots and most acutely in the youngestfully expanded leaf (2?l–6?9% N). When N contents wereexpressed on a tissue fresh weight basis the variation withtemperature lessened and the highest concentration in the shootwas at 11 ?C. Uptake of N increased with root temperature, andat all temperatures uptake of NH₄⁺, exceeded that of NO₃^–,irrespective of time. The proportions of total N uptake over14 d absorbed in the form of NH₄⁺ were (%): 86, 91, 75, 77,76, 73, 77, and 80, respectively, at 3, 5, 7, 9, Il, 13, 17,and 25 ?C. At all temperatures the preference for NH₄⁺ overNO₃^– uptake increased with time. An inverse relationshipbetween root temperature (3–11 ?C) and the uptake of NH₄⁺as a proportion of total N uptake was apparent during PhaseI. The possible mechanisms by which root temperature limitsgrowth and influences N uptake are discussed. Key words: Hordeum vulgare, root temperature, ammonium, nitrate, ion uptake, growth rate     

Effects of Exposure to Ammonium and Transplant Shock upon the Induction of Nitrate Absorption

In barley (Hordeum vulgare L. cv Steptoe) seedlings, the time course for induction of root nitrate absorption varied significantly with pretreatment. Net nitrate uptake of nitrogen-deprived plants more than doubled during the 12 hours after first exposure to nitrate. For these plants, gentle physical disturbance of the roots inhibited net nitrate absorption for more than 6 hours and potassium absorption for 2 hours. Pretreatment with ammonium appeared sufficient to induce nitrate absorption; plants either grown for 2 weeks on or exposed for only 10 hours to a medium containing ammonium as a sole nitrogen source showed high rates of net nitrate uptake when first shifted to a medium containing nitrate. Gentle physical manipulation of these plants inhibited nitrate absorption for 2 hours and potassium absorption for more than 12 hours. These results indicate (a) that experimental protocols should avoid physical manipulation of the roots when-ever possible and (b) that ammonium or a product of ammonium assimilation can induce nitrate absorption.     

Effects of Grazing by Flagellates on Competition for Ammonium between Nitrifying and Heterotrophic Bacteria in Soil Columns

The enhanced mineralization of immobilized nitrogen by bacteriophagous protozoa has been thought to favor the nitrification process in soils in which nitrifying bacteria must compete with heterotrophic bacteria for the available ammonium. To obtain more insight into this process, the influence of grazing by the flagellate Adriamonas peritocrescens on the competition for ammonium between the chemolithotrophic species Nitrosomonas europaea and the heterotrophic species Arthrobacter globiformis in the presence of Nitrobacter winogradskyi was studied in soil columns, which were continuously percolated with media containing 5 mM ammonium and different amounts of glucose at a dilution rate of 0.007 h^-1 (liquid volumes). A. globiformis won the competition for ammonium. The grazing activities of the flagellates had two prominent effects on the competition between N. europaea and A. globiformis. First, the distribution of ammonium over the profile of the soil columns was more uniform in the presence of flagellates than in their absence. In the absence of flagellates, relatively high amounts of ammonium accumulated in the upper layer (0 to 3 cm), whereas in the underlying layers the ammonium concentrations were low. In the presence of flagellates, however, considerable amounts of ammonium were found in the lower layers, whereas less ammonium accumulated in the upper layer. Second, the potential ammonium-oxidizing activity of N. europaea was stimulated in the presence of flagellates. The numbers of N. europaea at different glucose concentrations in the presence of flagellates were comparable to those in the absence of protozoa. However, in the presence of flagellates, the potential ammonium-oxidizing activities were four to five times greater than those in the absence of protozoa.     

Rapid, Reversible Inhibition of Nitrate Influx in Barley by Ammonium

The rate of influx of nitrate into the roots of intact barleyplants was measured over a period of 3–5 min from externalnitrate concentrations of 1–150 mmol m^–3, using¹³N-labelled nitrate as tracer. Ammonium at external concentrationsof 0.005–50 mol m^–3 inhibited nitrate influx ina manner which did not conform to a simple kinetic model butincreased approximately as the logarithm of the ammonium concentration.At any particular ammonium concentration, inhibition of nitrateinflux reached its full extent within 3 min of the ammoniumbeing supplied and was not made more severe by up to 17 minpre-treatment with ammonium. On removing the external ammonium,nitrate influx returned to its original rate within about 3min. Potassium at 0.005–50 mol m^–3 did not reproducethe rapid effect of ammonium on nitrate influx. Net uptake of nitrate also decreased when ammonium was supplied,over a similar timescale and to a similar extent as nitrateinflux. The decrease in nitrate influx caused by ammonium wassufficient to account for the observed reduction in net uptake,without necessitating any acceleration of nitrate efflux. Key words: Hordeum vulgare, roots, ion transport, short-lived isotopes, ¹³N     

Root Development and Absorption of Ammonium and Nitrate from the Rhizosphere

Plant roots operate in an environment that is extremely heterogeneous, both spatially and temporally. Nonetheless, under conditions of limited diffusion and against intense competition from soil microorganisms, plant roots locate and acquire vital nitrogen resources. Several factors influence the mechanisms by which roots respond to ammonium and nitrate. Nitrogen that is required for cell division and expansion derives primarily from the apex itself absorbing rhizosphere ammonium and nitrate. Root density and extension are greater in nutrient solutions containing ammonium than in those containing nitrate as the sole nitrogen source. Root nitrogen acquisition alters rhizosphere pH and redox potential, which in turn regulate root cell proliferation and mechanical properties. The net result is that roots proliferate in soil zones rich in nitrogen. Moreover, plants develop thinner and longer roots when ammonium is the primary nitrogen source, an appropriate strategy for a relatively immobile nitrogen form.