An improved procedure for 15N determination by emission spectrometry

An improved method for emission spectrometric determination of ¹⁵N content with a small amount of nitrogen (2 μg, minimum) is described. Ammonium nitrogen and organic nitrogen are converted to N₂ gas by the method of Rittenberg and by the method of Dumas, respectively. The N₂ gas is purified, introduced into a MacLeod vacuum gauge for measuring the total quantity, and then an appropriate amount of the N₂ gas is collected in a discharge tube containing a molecular sieve 5A so as to give a gas pressure of about 5 Torr. Emission is stable and reproducible, and ¹⁵N abundance can be determined with an error less than 0.01 and 0.10 atom% at a natural abundance level of 0.366 and at 9 atom%, respectively. Predetermination of N content of samples is not required.     

AUTORADIOGRAPHIC LOCALIZATION OF 13N AFTER FIXATION OF 13N-LABELED NITROGEN GAS BY A HETEROCYST-FORMING BLUE-GREEN ALGA

¹³N, generated by proton bombardment of ¹³C powder, is rapidly and easily converted to ¹³N-N₂, 0.01 atm pressure, ca. 10 mCi/ml, by automated Dumas combustion. ¹³N fixed (as ¹³N-N₂) by algal filaments was localized by an autoradiographic technique which permits track autoradiography with isotopes having short half-lives. Our findings show directly that a minimum of about 25% of the N₂ fixation by intact, aerobically grown filaments of Anabaena cylindrica is carried out by the heterocysts. If all of the N₂ fixation takes place in the heterocysts, then the movement of nitrogen along the filaments can be characterized by a constant τ < ca. 5 s (cell^-2).     

New Method of Denitrification Analysis of Bradyrhizobium Field Isolates by Gas Chromatographic Determination of 15N-Labeled N2

To evaluate the denitrification abilities of many Bradyrhizobium field isolates, we developed a new ¹⁵N-labeled N₂ detection methodology, which is free from interference from atmospheric N₂ contamination. ³⁰N₂ (¹⁵N¹⁵N) and ²⁹N₂ (¹⁵N¹⁴N) were detected as an apparent peak by a gas chromatograph equipped with a thermal conductivity detector with N₂ gas having natural abundance of ¹⁵N (0.366 atom%) as a carrier gas. The detection limit was 0.04% ³⁰N₂, and the linearity extended at least to 40% ³⁰N₂. When Bradyrhizobium japonicum USDA110 was grown in cultures anaerobically with ¹⁵NO₃⁻, denitrification product (³⁰N₂) was detected stoichiometrically. A total of 65 isolates of soybean bradyrhizobia from two field sites in Japan were assayed by this method. The denitrification abilities were partly correlated with filed sites, Bradyrhizobium species, and the hup genotype.     

Natural 15N abundance of presumed N2-fixing and non-N2-fixing plants from selected ecosystems

Summary The ¹⁵N/¹⁴N ratios of plant and soil samples from Northern California ecosystems were determined by mass spectrometry. The ¹⁵N abundance of 176 plant foliar samples averaged 0.0008 atom % ¹⁵N excess relative to atmospheric N₂ and ranged from-0.0028 to 0.0064 atom % ¹⁵N excess relative to atmospheric N₂. Foliage from reported N₂-fixing species had significantly lower mean ¹⁵N abundance (relative to atmospheric N₂ and total soil N) and significantly higher N concentration (% N dry wt.) than did presumed non-N₂-fixing plants growing on the same sites. The mean difference between N₂-fixing species and other plants was 0.0007 atom % ¹⁵N. N₂-fixing species had lower ¹⁵N abundance than the other plants on most sites examined despite large differences between sites in vegetation, soil, and climate. The mean ¹⁵N abundance of N₂-fixing plants varied little between sites and was close to that of atmospheric N₂. The ¹⁵N abundance of presumed non-N₂-fixing species was highest at coastal sites and may reflect an input of marine spray N having relatively high ¹⁵N abundance. The ¹⁵N abundance of N₂-fixing species was not related to growth form but was for other plants. Annual herbaceous plants had highest ¹⁵N abundance followed in decreasing order by perennial herbs, shrubs, and trees. Several terrestrial ferns (Pteridaceae) had ¹⁵N abundances comparable to N₂-fixing legumes suggesting N₂-fixation by these ferns. On sites where the ¹⁵N abundance of soil N differs from that of the atmosphere, N₂-fixing plants can be identified by the natural ¹⁵N abundance of their foliage. This approach can be useful in detecting and perhaps measuring N₂-fixation on sites where direct recovery of nodules is not possible.     

15N-determined dinitrogen fixation potential of genetically diverse bean lines (Phaseolus vulgaris L.)

Improvement of dinitrogen fixation in beans (Phaseolus vulgaris L.) will depend on the selection of superior plant genotypes and the presence of efficient rhizobial strains. This study was conducted to evaluate diverse bean lines for N₂ fixation potential using the¹⁵N-depleted dilution technique under field conditions in Wisconsin, USA. Plants of 21 bean lines and three non-nodulating isolines of soybean received appliin Wisconsin, USA. Plants of 21 bean lines and three non-nodulating isolines of soybean received applications of¹⁵N-depleted ammonium sulphate. Shoots harvested at the V₆, R₃ and R₇ stages and dry seeds were analyzed for total N using the Kjeldahl procedure, and the ratio of¹⁵N to¹⁴N was determind on a MAT 250 mass spectrometer. Nodule occupancy of the applied strain ofR. leguminosarum biovarphaseoli, CIAT 899, was determined in five of the bean lines. Total shoot N content showed a pattern of accumulation similar to shoot dry weight and fixed N₂ in the shoot. Based on shoot total N, N₂ fixed in the shoot and shoot dry weight Riz 30 and Preto Cariri were identified as being as good fixers as Puebla 152 and Cargamanto appear to begin N₂ fixation early. Furthermore, some bean lines that fixed considerable N₂ did not translocate a large amount of N to the grains. Preto Cariri accumulated 21.2 kg N ha⁻¹ in the seeds compared to Puebla 152 which accumulated 43.8 kg N ha⁻¹ of the fixed N₂ into the grains. At the early sampling, Puebla 152 and 22–27 had a considerable higher percentage of their crown nodules formed by the inoculant strain CIAT 899, than did Rio Tibagi which has been considered a poor N₂ fixer.     

Evaluation of automated analysis of 15N and total N in plant material and soil

Simultaneous determination of ¹⁵N and total N using an automated nitrogen analyser interfaced to a continuous-flow isotope ratio mass spectrometer (ANA-MS method) was evaluated. The coefficient of variation (CV) of repeated analyses of homogeneous standards and samples at natural abundance was lower than 0.1%. The CV of repeated analyses of ¹⁵N-labelled plant material and soil samples varied between 0.3% and 1.1%. The reproductibility of repeated total N analyses using the automated method was comparable to results obtained with a semi-micro Kjeldahl procedure. However, the automated method gave results which were 3% to 5% higher than those obtained with the Kjeldahl procedure. Since only small samples can be analysed, careful sample homogenization and fine grinding are very important. Evaluation of a diffusion method for preparing nitrate and ammonium in solution for automated ¹⁵N analysis showed that the recovery of inorganic N in the NH₃ trap was lower when the N was diffused from water than from 2 M KCl. The results also indicated that different proportions of the NO₃ ^- and the NH₄ ⁺ in aqueous solution were recovered in the trap after combined diffusion. The method is most suited for diffusing either NO₃ ^- or NH₄ ⁺ alone, but can be used for combined diffusion of the two ions.     

Distribution of fixed-N and nitrate-N in cowpea during pod development

If the quality and quantity of yields from cowpea (Vigna unguiculata [L.] Walp.) are to be maximised, a complete understanding of the N nutrition of the plant must be achieved. The N requirement for developing pods of this species may come from mobilization of N in vegetative tissue, biological N fixation and uptake of N from soil. In this study, the fate of a pulse of fixed ¹⁵N₂ or of ¹⁵NO₃-given to different cowpea plants during pod development was determined. The plants were grown in vermiculite in plastic pots that were able to be sealed with silicone adhesive and equipped with a rubber septum so that ¹⁵N₂ gas could be injected into the air space above the vermiculite, and gas losses would be eliminated. Nineteen days after injection of ¹⁵N₂ the pods, leaves, nodules and roots contained 65%, 15%, 9%, and 4%, respectively of the quantity of ¹⁵N₂ fixed. When ¹⁵NO₃-¹⁵N was taken up by other plants during this period, these plant parts contained 40%, 26%, 3% and 19%, respectively, of the total plant ¹⁵N. The percentage ¹⁵N in roots was greater, and that of ¹⁵N in nodules was lower, when ¹⁵NO₃-¹⁵N was applied than when ¹⁵N₂ was utilised by plants. These results indicate that, while a high percentage of fixed-N or NO₃-N given to cowpea plants moved to the developing pods, other sinks were competing for this newly-aquired N.     

Nitrogen gas (N2+N2O) flux from urea applied to lowland rice as affected by green manure

A field study was conducted on a clay soil (Andaqueptic Haplaquoll) in the Philippines to directly measure the evolution of (N₂+N₂O)−¹⁵N from 98 atom %¹⁵N-labeled urea broadcast at 29 kg N ha⁻¹ into 0.05-m-deep floodwater at 15 days after transplanting (DT) rice. The flux of (N₂+N₂O)−¹⁵N during the 19 days following urea application never exceeded 28 g N ha⁻¹ day⁻¹. The total recovery of (N₂+N₂O)−¹⁵N evolved from the field was only 0.51% of the applied N, whereas total gaseous¹⁵N loss estimated from unrecovered¹⁵N in the¹⁵N balance was 41% of the applied N. Floodwater (nitrate+nitrite)−N in the 5 days following urea application never exceeded 0.14 g N m⁻³ or 0.3% of the applied N. Prior cropping of cowpea [Vigna unguiculata (L.) Walp.] to flowering with subsequent incorporation of the green manure (dry matter=2.5 Mg ha⁻¹, C/N=15) at 15 days before rice transplanting had no effect on fate of urea applied to rice at 15 DT. The recovery of (N₂+N₂O)−¹⁵N and total¹⁵N loss during the 19 days following urea application were 0.46 and 40%, respectively. Direct recovery of evolved (N₂+N₂O)−¹⁵N and total¹⁵N loss from 27 kg applied nitrate-N ha⁻¹ were 20% and 53% during the same 19-day period. The failure of directly-recovered (N₂+N₂O)−¹⁵N to match total¹⁵N loss from added nitrate-¹⁵N might be due to entrapment of denitrification end products in soil or transport of gaseous end products to the atmosphere through rice plants. The rapid conversion of added nitrate-N to (N₂+N₂O)−N, the apparently sufficient water soluble soil organic C for denitrification (101 μg C g⁻¹ in the top 0.15-m soil layer), and the low floodwater nitrate following urea application suggested that denitrification loss from urea was controlled by supply of nitrate rather than by availability of organic C.     

Rapid Conversion of Added Nitrate to Nitrous Oxide and Dinitrogen in Northern Forest Soil

The aims of this study were to simulate wet deposition of atmospheric nitrate (NO₃^?) onto forest soils and trace its fate via conversion spatially and temporally into gaseous products nitrous oxide (N₂O) and dinitrogen (N₂). The most likely mechanism is microbial denitrification, but an intermediate product nitrite (NO₂^?) can fuel N₂O production via a chemical pathway involving reactions with iron and/or organic matter referred to as chemodenitrification. During summer months, we applied tracer amounts of ¹⁵N-labeled NO₃^? onto forest soils (pH ～ 4) at three sites in the White Mountain Region of New Hampshire, USA. We recovered ¹⁵N as N₂O in 210 of 504 measurements (42%) versus ¹⁵N as N₂ in 51 of 504 measurements (10%), suggesting partial microbial denitrification and/or chemodenitrification. When recovery occurred, the mean percent recovery of added ¹⁵N was just 1.1% as N₂O, although N₂ recovery was 33%. A site with old-growth trees had a larger percentage recovery as N₂ (48%), whereas a site that had burned 100 years ago had a small percentage recovery as N₂O (0.24%). The ¹⁵N composition of N₂O in ambient air, collected before addition of the label, was markedly enriched in ¹⁵N. Since flux measurements were made 2 h after the addition, the results suggest that denitrification enzymes and conditions for chemodenitrification are present throughout the summer months but account for small amounts of NO₃^? conversion into N₂O and N₂.     

Nitrous Oxide Reduction in Nodules: Denitrification or N2 Fixation?

Detached cowpea nodules that contained a nitrous oxide reductase-positive (Nor⁺) rhizobium strain (8A55) and a nitrous oxide reductase-negative (Nor⁻) rhizobium strain (32H1) were incubated with 1% ¹⁵N₂O (95 atom% ¹⁵N) in the following three atmospheres: (i) aerobic with C₂H₂ (10%), (ii) aerobic without C₂H₂, and (iii) anaerobic (argon atmosphere) without C₂H₂. The greatest production of ¹⁵N₂ occurred anaerobically with 8A55, yet very little was formed with 32H1. Although acetylene reduction activity was slightly higher with 32H1, about 10 times more ¹⁵N₂ was produced aerobically by 8A55 than by 32H1 in the absence of acetylene. The major reductive pathway of N₂O reduction by denitrifying rhizobium strain 8A55 is by nitrous oxide reductase rather than nitrogenase.     

Impaired Synthesis of Acetylcholine by Mild Hypoxic Hypoxia or Nitrous Oxide

The effect of mild hypoxic hypoxia on brain metabolism and acetylcholine synthesis was studied in awake, restrained rats. Since many studies of hypoxia are done with animals anesthetized with nitrous oxide (N₂O), the effects of N²O were evaluated. N²O (70%) increased the cerebral cortical blood flow by 33% and the cortical metabolic rate of oxygen by 26%. In addition, the synthesis of acetylcholine in N²O-anesthetized animals, measured with [U-¹⁴C]glucose and [1-²H₂,2-²H₂]choline, decreased by 45 and 53%, respectively. Consequently, mild hypoxia was studied in unanesthetized rats. Control rats breathing 30% O₂ (partial pressure of oxygen, Pao₂= 120 mm Hg) were compared with rats exposed to 15% O₂ (Pao₂= 57 mm Hg) or 10% O₂ (Pao₂= 42 mm Hg). The synthesis of acetylcholine, measured with [U-¹⁴C]glucose, was decreased by 35 and 54% with 15% O₂ and 10% O₂ respectively; acetylcholine synthesis, measured with [1-²H₂,2-²H₂]choline, was decreased by 50 and 68% with 15% O₂ and 10% O₂ respectively. Animals breathing either 15% or 10% O₂ had normal cerebral metabolic rates of oxygen but had increased brain lactates and increased cortical blood flows compared with animals breathing 30% O₂. These results show that even mild hypoxic hypoxia impairs acetylcholine synthesis, which in turn may account for the early symptoms of brain dysfunction associated with hypoxia.     

Denitrification of nitrate to nitrogen gas by washed cells ofRhizobium japonicum and by bacteroids fromGlycine max

Nitrate, nitrite and nitrous oxide were denitrified to N₂ gas by washed cells ofRhizobium japonicum CC706 as well as by bacteroids prepared from root nodules ofGlycine max (L.) Merr. (CV. Clark 63). Radiolabelled N₂ was produced from either K¹⁵NO₃ or Na¹⁵NO₂ by washed cells ofRh. japonicum CC705 grown with either nitrate only (5 mM) or nitrate (5 mM) plus glutamate (10 mM). Nitrogen gas was also produced from N₂O. Similar results were obtained with bacteroids ofG. max. The stoichiometry for the utilization of¹⁵NO ₃ ^- or¹⁵NO ₂ ^- and the produciton of¹⁵N₂ was 2:1 and for N₂O utilization and N₂ production it was 1:1. Some of the¹⁵N₂ gas produced by denitrification of¹⁵NO ₃ ^- in bacteroids was recycled via nitrogenase into cell nitrogen.     

Symbiotic Bradyrhizobium japonicum Reduces N2O Surrounding the Soybean Root System via Nitrous Oxide Reductase

N₂O reductase activity in soybean nodules formed with Bradyrhizobium japonicum was evaluated from N₂O uptake and conversion of ¹⁵N-N₂O into ¹⁵N-N₂. Free-living cells of USDA110 showed N₂O reductase activity, whereas a nosZ mutant did not. Complementation of the nosZ mutant with two cosmids containing the nosRZDFYLX genes of B. japonicum USDA110 restored the N₂O reductase activity. When detached soybean nodules formed with USDA110 were fed with ¹⁵N-N₂O, they rapidly emitted ¹⁵N-N₂ outside the nodules at a ratio of 98.5% of ¹⁵N-N₂O uptake, but nodules inoculated with the nosZ mutant did not. Surprisingly, N₂O uptake by soybean roots nodulated with USDA110 was observed even in ambient air containing a low concentration of N₂O (0.34 ppm). These results indicate that the conversion of N₂O to N₂ depends exclusively on the respiratory N₂O reductase and that soybean roots nodulated with B. japonicum carrying the nos genes are able to remove very low concentrations of N₂O.     

Elevated CO2 stimulates associative N2 fixation in a C3 plant of the Chesapeake Bay wetland

In this study, the response of N₂ fixation to elevated CO₂ was measured in Scirpus olneyi, a C₃ sedge, and Spartina patens, a C₄ grass, using acetylene reduction assay and ¹⁵N₂ gas feeding. Field plants grown in PVC tubes (25 cm long, 10 cm internal diameter) were used. Exposure to elevated CO₂ significantly (P < 0·05) caused a 35% increase in nitrogenase activity and 73% increase in ¹⁵N incorporated by Scirpus olneyi. In Spartina patens, elevated CO₂ (660 ± 1 μ mol mol ^{− 1}) increased nitrogenase activity and ¹⁵N incorporation by 13 and 23%, respectively. Estimates showed that the rate of N₂ fixation in Scirpus olneyi under elevated CO₂ was 611 ± 75 ng ¹⁵N fixed plant ^{− 1} h ^{− 1} compared with 367 ± 46 ng ¹⁵N fixed plant ^{− 1} h ^{− 1} in ambient CO₂ plants. In Spartina patens, however, the rate of N₂ fixation was 12·5 ± 1·1 versus 9·8 ± 1·3 ng ¹⁵N fixed plant ^{− 1} h ^{− 1} for elevated and ambient CO₂, respectively. Heterotrophic non-symbiotic N₂ fixation in plant-free marsh sediment also increased significantly (P < 0·05) with elevated CO₂. The proportional increase in ¹⁵N₂ fixation correlated with the relative stimulation of photosynthesis, in that N₂ fixation was high in the C₃ plant in which photosynthesis was also high, and lower in the C₄ plant in which photosynthesis was relatively less stimulated by growth in elevated CO₂. These results are consistent with the hypothesis that carbon fixation in C₃ species, stimulated by rising CO₂, is likely to provide additional carbon to endophytic and below-ground microbial processes.     

Rapid Growth and Apparent Total Nitrogen Increases in Rice and Corn Plants following Applications of Triacontanol

Triacontanol (TRIA) increased fresh and dry weight and total reducible nitrogen (total N) of rice (Oryza sativa L.) seedlings within 40 minutes. Increases in total N in the supernatants from homogenates of corn (Zea mays L.) and rice leaves treated with TRIA for one minute before grinding occurred within 30 and 80 minutes, respectively. The source for the increase was investigated utilizing atmospheric substitution and enrichment and depletion studies with ¹⁵N. The increase in total N in seedlings was shown to be independent of method of N analysis and the presence of nitrate in the plants. Automated Kjeldahl determinations showing apparent increases in N composition due to TRIA were shown to be correlated with hand Kjeldahl, elemental analysis, and chemiluminescent analysis in three independent laboratories. TRIA did not alter the nitrate uptake or endogenous levels of nitrate in corn and rice seedlings. Enrichment experiments revealed that the total N increases in rice seedlings, in vivo, and in supernatants of corn leaf homogenates, in vitro, are not due to atmospheric N₂. TRIA increased the soluble N pools of the plants, specifically the free amino acid and soluble protein fractions. No differences in depletion or enrichment of ¹⁵N incorporated into soluble and insoluble N fractions of rice seedlings could be detected on an atom per cent ¹⁵N basis. The apparent short-term total N increases cannot be explained by current knowledge of major N assimilation pathways. TRIA may stimulate a change in the chemical composition of the seedlings, resulting in interference with standard methods of N analysis.     

An in-depth look into a tropical lowland forest soil: nitrogen-addition effects on the contents of N2O, CO2 and CH4 and N2O isotopic signatures down to 2-m depth

Atmospheric nitrogen (N) deposition is rapidly increasing in tropical regions. We investigated how a decade of experimental N addition (125 kg N ha^?1 year^?1) to a seasonal lowland forest affected depth distribution and contents of soil nitrous oxide (N₂O), carbon dioxide (CO₂) and methane (CH₄), as well as natural abundance isotopic signatures of N₂O, nitrate (NO₃ ^?) and ammonium (NH₄ ⁺). In the control plots during dry season, we deduced limited N₂O production by denitrification in the topsoil (0.05–0.40 m) as indicated by: ambient N₂O concentrations and ambient ¹⁵N-N₂O signatures, low water-filled pore space (35–60%), and similar ¹⁵N signatures of N₂O and NO₃ ^?. In the subsoil (0.40–2.00 m), we detected evidence of N₂O reduction to N₂ during upward diffusion, indicating denitrification activity. During wet season, we found that N₂O at 0.05–2.00 m was mainly produced by denitrification with substantial further reduction to N₂, as indicated by: lighter ¹⁵N-N₂O than ¹⁵N-NO₃ ^? throughout the profile, and increasing N₂O concentrations with simultaneously decreasing ¹⁵N-N₂O enrichment with depth. These interpretations were supported by an isotopomer map and by a positive correlation between ¹⁸O-N₂O and ¹⁵N-N₂O site preferences. Long-term N addition did not affect dry-season soil N₂O-N contents, doubled wet-season soil N₂O-N contents, did not affect ¹⁵N signatures of NO₃ ^?, and reduced wet-season ¹⁵N signatures of N₂O compared to the control plots. These suggest that the increased NO₃ ^? concentrations have stimulated N₂O production and decreased N₂O-to-N₂ reduction. Soil CO₂-C contents did not differ between treatments, implying that N addition essentially did not influence soil C cycling. The pronounced seasonality in soil respiration was largely attributable to enhanced topsoil respiration as indicated by a wet-season increase in the topsoil CO₂-C contents. The N-addition plots showed reduced dry-season soil CH₄-C contents and threshold CH₄ concentrations were reached at a shallower depth compared to the control plots, revealing an N-induced stimulation of methanotrophic activity. However, the net soil CH₄ uptake rates remained similar between treatments possibly because diffusive CH₄ supply from the atmosphere largely limited CH₄ oxidation.     

Formation of unidentified nitrogen in plants: an implication for a novel nitrogen metabolism

Plants take up inorganic nitrogen and store it unchanged or convert it to organic forms. The nitrogen in such organic compounds is stoichiometrically recoverable by the Kjeldahl method. The sum of inorganic nitrogen and Kjeldahl nitrogen has long been known to equal the total nitrogen in plants. However, in our attempt to study the mechanism of nitrogen dioxide (NO₂) metabolism, we unexpectedly discovered that about one-third of the total nitrogen derived from ¹⁵N-labeled NO₂ taken up by Arabidopsis thaliana (L.) Heynh. plants was converted to neither inorganic nor Kjeldahl nitrogen, but instead to an as yet unknown nitrogen compound(s). We here refer to this nitrogen as unidentified nitrogen (UN). The generality of the formation of UN across species, nitrogen sources and cultivation environments for plants has been shown as follows. Firstly, all of the other 11 plant species studied were found to form the UN in response to fumigation with ¹⁵NO₂. Secondly, tobacco (Nicotiana tabacum L.) plants fed with ¹⁵N-nitrate appeared to form the UN. And lastly, the leaves of naturally fed vegetables, grass and roadside trees were found to possess the UN. In addition, the UN appeared to comprise a substantial proportion of total nitrogen in these plant species. Collectively, all of our present findings imply that there is a novel nitrogen mechanism for the formation of UN in plants. Based on the analyses of the exhaust gas and residue fractions of the Kjeldahl digestion of a plant sample containing the UN, probable candidates for compounds that bear the UN were deduced to be those containing the heat-labile nitrogen–oxygen functions and those recalcitrant to Kjeldahl digestion, including organic nitro and nitroso compounds. We propose UN-bearing compounds may provide a chemical basis for the mechanism of the reactive nitrogen species (RNS), and thus that cross-talk may occur between UN and RNS metabolisms in plants. A mechanism for the formation of UN-bearing compounds, in which RNS are involved as intermediates, is proposed. The important broad impact of this novel nitrogen metabolism, not only on the general physiology of plants, but also on plant substances as human and animal food, and on plants as an integral part of the global environment, is discussed.Abbreviations NO Nitric oxide - NO₂ Nitrogen dioxide - RNS Reactive nitrogen species - UN Unidentified nitrogen - TNNAT, RNNAT, INNAT and UNNAT Total, Kjeldahl, inorganic and unidentified nitrogen in naturally fed plants, respectively - TNNIT, RNNIT, INNIT and UNNIT Total, Kjeldahl, inorganic and unidentified nitrogen derived from nitrate, respectively - TNNO2, RNNO2, INNO2 and UNNO2 Total, Kjeldahl, inorganic and unidentified nitrogen derived from NO₂, respectively     

The acetylene-ethylene assay for n(2) fixation: laboratory and field evaluation

The methodology, characteristics and application of the sensitive C₂H₂-C₂H₄ assay for N₂ fixation by nitrogenase preparations and bacterial cultures in the laboratory and by legumes and free-living bacteria in situ is presented in this comprehensive report. This assay is based on the N₂ase-catalyzed reduction of C₂H₂ to C₂H₄, gas chromatographic isolation of C₂H₂ and C₂H₄, and quantitative measurement with a H₂-flame analyzer. As little as 1 μμmole C₂H₄ can be detected, providing a sensitivity 10³-fold greater than is possible with ¹⁵N analysis.

A simple, rapid and effective procedure utilizing syringe-type assay chambers is described for the analysis of C₂H₂-reducing activity in the field. Applications to field samples included an evaluation of N₂ fixation by commercially grown soybeans based on over 2000 analyses made during the course of the growing season. Assay values reflected the degree of nodulation of soybean plants and indicated a calculated seasonal N₂ fixation rate of 30 to 33 kg N₂ fixed per acre, in good agreement with literature estimates based on Kjeldahl analyses. The assay was successfully applied to measurements of N₂ fixation by other symbionts and by free living soil microorganisms, and was also used to assess the effects of light and temperature on the N₂ fixing activity of soybeans. The validity of measuring N₂ fixation in terms of C₂H₂ reduction was established through extensive comparisons of these activities using defined systems, including purified N₂ase preparations and pure cultures of N₂-fixing bacteria.

With this assay it now becomes possible and practicable to conduct comprehensive surveys of N₂ fixation, to make detailed comparisons among different N₂-fixing symbionts, and to rapidly evaluate the effects of cultural practices and environmental factors on N₂ fixation. The knowledge obtained through extensive application of this assay should provide the basis for efforts leading to the maximum agricultural exploitation of the N₂ fixation reaction.

     

The Contamination of Commercial 15N2 Gas Stocks with 15N–Labeled Nitrate and Ammonium and Consequences for Nitrogen Fixation Measurements

We report on the contamination of commercial 15-nitrogen (¹⁵N) N₂ gas stocks with ¹⁵N-enriched ammonium, nitrate and/or nitrite, and nitrous oxide. ¹⁵N₂ gas is used to estimate N₂ fixation rates from incubations of environmental samples by monitoring the incorporation of isotopically labeled ¹⁵N₂ into organic matter. However, the microbial assimilation of bioavailable ¹⁵N-labeled N₂ gas contaminants, nitrate, nitrite, and ammonium, is liable to lead to the inflation or false detection of N₂ fixation rates. ¹⁵N₂ gas procured from three major suppliers was analyzed for the presence of these ¹⁵N-contaminants. Substantial concentrations of ¹⁵N-contaminants were detected in four Sigma-Aldrich ¹⁵N₂ lecture bottles from two discrete batch syntheses. Per mole of ¹⁵N₂ gas, 34 to 1900 µmoles of ¹⁵N-ammonium, 1.8 to 420 µmoles of ¹⁵N-nitrate/nitrite, and ≥21 µmoles of ¹⁵N-nitrous oxide were detected. One ¹⁵N₂ lecture bottle from Campro Scientific contained ≥11 µmoles of ¹⁵N-nitrous oxide per mole of ¹⁵N₂ gas, and no detected ¹⁵N-nitrate/nitrite at the given experimental ¹⁵N₂ tracer dilutions. Two Cambridge Isotopes lecture bottles from discrete batch syntheses contained ≥0.81 µmoles ¹⁵N-nitrous oxide per mole ¹⁵N₂, and trace concentrations of ¹⁵N-ammonium and ¹⁵N-nitrate/nitrite. ¹⁵N₂ gas equilibrated cultures of the green algae Dunaliella tertiolecta confirmed that the ¹⁵N-contaminants are assimilable. A finite-differencing model parameterized using oceanic field conditions typical of N₂ fixation assays suggests that the degree of detected ¹⁵N-ammonium contamination could yield inferred N₂ fixation rates ranging from undetectable, <0.01 nmoles N L⁻¹ d⁻¹, to 530 nmoles N L⁻¹ d⁻¹, contingent on experimental conditions. These rates are comparable to, or greater than, N₂ fixation rates commonly detected in field assays. These results indicate that past reports of N₂ fixation should be interpreted with caution, and demonstrate that the purity of commercial ¹⁵N₂ gas must be ensured prior to use in future N₂ fixation rate determinations.     

Heterotrophic n(2) fixation and distribution of newly fixed nitrogen in a rice-flooded soil system

Rice (Oryza sativa L.) plants growing in pots of flooded soil were exposed to a ¹⁵N₂-enriched atmosphere for 3 to 13 days in a gas-tight chamber. The floodwater and soil surface were shaded with a black cloth to reduce the activity of phototrophic N₂-fixing micro-organisms. The highest ¹⁵N enrichments were consistently observed in the roots, although the total quantity of ¹⁵N incorporated into the soil was much greater. The rate of ¹⁵N incorporation into roots was much higher at the heading than at the tillering stage of growth. Definite enrichments were also found in the basal node and in the lower outer leaf sheath fractions after 3 days of exposure at the heading stage. Thirteen days was the shortest time period in which definite ¹⁵N enrichment was observed in the leaves and panicle. When plants were exposed to ¹⁵N₂ for 13 days just before heading and then allowed to mature in a normal atmosphere, 11.3% of the total ¹⁵N in the system was found in the panicles, 2.3% in the roots, and 80.7% in the subsurface soil. These results provide direct evidence of heterotrophic N₂ fixation associated with rice roots and the flooded soil and demonstrate that part of the newly fixed N is available to the plant.