Effect of inoculation with n(2)-fixing spirilla and azotobacter on nitrogenase activity on roots of maize grown under subtropical conditions

Inoculated and non-inoculated seedlings of maize were grown in fertile clayloam soils of Egypt and Belgium under subtropical conditions provided in a greenhouse. Acetylene-reducing activity and microbial counts were determined during a period ranging from 6 to 12 weeks after sowing. Irrespective of soil origin, N(2)-fixing spirilla and Azotobacter were common under maize cultivation. Inoculation resulted in a transitional increase in their numbers at early stages of growth. Nitrogenase activity was not detected in the rhizosphere of young plants. The maximum activities measured (81 to 1,436 nmol of C(2)H(4) g h) occurred close to the 50 to 70% silking stage. Inoculation with N(2)-fixing spirilla, particularly in Nile Delta soil, doubled the amount of N(2) fixed in a late period of growth (12 weeks), whereas inoculation with Azotobacter had no noticeable effect.     

Olive mill waste as a substrate for nitrogen fixation

Olive mill wastewaters (OMWW) because of their low content in nitrogenous organic components and reachness in carbon sources offer a highly favourable environment for the growth of free-living dinitrogen fixing microorganisms. This property is manifested both in natural environments and in axenic cultures. Repetitive addition of OMWW to soil under aerobic conditions leads progressively to its enrichment with dinitrogen fixers, the activity of which is beneficial to soil fertility. The microbial consortium that develops in soil is dominated mostly by members of Azotobacter. A very efficient N₂-fixing and slime producing strain of Azotobacter vinelandii (strain A) was isolated from such an enriched soil sample. The isolate is deposited in the culture collection of our laboratory and its biochemical and molecular characteristics are investigated. The strain proved to be effective in bio-remediation processes of OMWW both in a laboratory-scale fermenter unit and a field pilot plant of ca 5 m³ capacity. The inhibitory growth-limiting components of the principal OMWW constituents and their impact on the duration of the lag period of N₂-fixing activity recovery is examined. The design of a multi-stream two stage process is described which provides a stable N₂-fixing system suitable for the bio-transformation of OMWW into an agrobiological product and/or for the production of extracellular polysaccharide ‘slime’ in high yields.     

Untraditional N2-fixing bacteria as biofertilizers for wheat and barley

The screening of 27 isolates grown on nitrogen-free medium for nitrogen-fixing ability resulted in the isolation of five organisms belonging toBacillaceae, Enterobacteriaceae andPseudomonadaceae. Estimates of N₂-fixation efficiencies of these isolates indicated that they may be responsible for low rates of N₂-fixation in soil. The possible association of these isolates as well as ofAzotobacter andAzospirillum with wheat and barley was investigated in a greenhouse experiment. The highest values of nitrogenase activity on plant root were recorded in treatments inoculated with composite inocula of the isolated N₂-fixers, particularly whenAzotobacter and/orAzospirillum were added in combination. Inoculation with single inoculum of each of the N₂-fixing isolates had no significant influence on plant growth, except withPseudomonas andBacillus for wheat and barley, respectively. Highly significant increases in growth of both plants were recorded in all cases of multistrain inoculation.     

Effect of Inoculation and Leaf Litter Amendment on Establishment of Nodule-Forming Frankia Populations in Soil

High-N₂-fixing activities of Frankia populations in root nodules on Alnus glutinosa improve growth performance of the host plant. Therefore, the establishment of active, nodule-forming populations of Frankia in soil is desirable. In this study, we inoculated Frankia strains of Alnus host infection groups I, IIIa, and IV into soil already harboring indigenous populations of infection groups (IIIa, IIIb, and IV). Then we amended parts of the inoculated soil with leaf litter of A. glutinosa and kept these parts of soil without host plants for several weeks until they were spiked with [¹⁵N]NO₃ and planted with seedlings of A. glutinosa. After 4 months of growth, we analyzed plants for growth performance, nodule formation, specific Frankia populations in root nodules, and N₂ fixation rates. The results revealed that introduced Frankia strains incubated in soil for several weeks in the absence of plants remained infective and competitive for nodulation with the indigenous Frankia populations of the soil. Inoculation into and incubation in soil without host plants generally supported subsequent plant growth performance and increased the percentage of nitrogen acquired by the host plants through N₂ fixation from 33% on noninoculated, nonamended soils to 78% on inoculated, amended soils. Introduced Frankia strains representing Alnus host infection groups IIIa and IV competed with indigenous Frankia populations, whereas frankiae of group I were not found in any nodules. When grown in noninoculated, nonamended soil, A. glutinosa plants harbored Frankia populations of only group IIIa in root nodules. This group was reduced to 32% ± 23% (standard deviation) of the Frankia nodule populations when plants were grown in inoculated, nonamended soil. Under these conditions, the introduced Frankia strain of group IV was established in 51% ± 20% of the nodules. Leaf litter amendment during the initial incubation in soil without plants promoted nodulation by frankiae of group IV in both inoculated and noninoculated treatments. Grown in inoculated, amended soils, plants had significantly lower numbers of nodules infected by group IIIa (8% ± 6%) than by group IV (81% ± 11%). On plants grown in noninoculated, amended soil, the original Frankia root nodule population represented by group IIIa of the noninoculated, nonamended soil was entirely exchanged by a Frankia population belonging to group IV. The quantification of N₂ fixation rates by ¹⁵N dilution revealed that both the indigenous and the inoculated Frankia populations of group IV had a higher specific N₂-fixing capacity than populations belonging to group IIIa under the conditions applied. These results show that through inoculation or leaf litter amendment, Frankia populations with high specific N₂-fixing capacities can be established in soils. These populations remain infective on their host plants, successfully compete for nodule formation with other indigenous or inoculated Frankia populations, and thereby increase plant growth performance.     

Effect of N Source on the Steady State Growth and N Assimilation of P-limited Anabaena flos-aquae

Phosphate-limited chemostat cultures were used to study cell growth and N assimilation in Anabaena flos-aquae under various N sources to determine the relative energetic costs associated with the assimilation of NH₃, NO₃⁻, or N₂. Expressed as a function of relative growth rate, steady state cellular P contents and PO₄ assimilation rates did not vary with N-source. However, N-source did alter the maximal PO₄-limited growth rate achieved by the cultures: the NO₃⁻ and N₂ cultures attained only 97 and 80%, respectively, of the maximal growth rate of the NH₃ grown cells. Cellular biomass and C contents did not vary with growth rate, but changed with N source. The NO₃⁻-grown cells were the smallest (627 ± 34 micromoles C · 10⁻⁹ cells), while NH₃-grown cells were largest (900 ± 44 micromoles C · 10⁻⁹ cells) and N₂-fixing cells were intermediate (726 ± 48 micromoles C · 10⁻⁹ cells) in size. In the NO₃⁻-and N₂-grown cultures, N content per cell was only 57 and 63%, respectively, of that in the NH₃-grown cells. Heterocysts were absent in NH₃-grown cultures but were present in both the N₂ and NO₃⁻ cultures. In the NO₃⁻-grown cultures C₂H₂ reduction was detected only at high growth rates, where it was estimated to account for a maximum of 6% of the N assimilated. In the N₂-fixing cultures the acetylene:N₂ ratio varied from 3.4:1 at lower growth rates to 3.0:1 at growth rates approaching maximal.

Compared with NH₃, the assimilation of NO₃⁻ and N₂ resulted either in a decrease in cellular C (NO₃⁻ and N₂ cultures) or in a lower maximal growth rate (N₂ culture only). The observed changes in cell C content were used to calculate the net cost (in electron pair equivalents) associated with growth on NO₃⁻ or N₂ compared with NH₃.

     

Enumeration and Relative Importance of Acetylene-Reducing (Nitrogen-Fixing) Bacteria in a Delaware Salt Marsh

Three groups of N₂-fixing bacteria were enumerated from the top 1 cm of the surface in four vegetational areas in a Delaware salt marsh. The results over the 9-month sampling period showed that there were no discernible seasonal patterns for any of the groups enumerated (Azotobacter sp., Clostridium sp., and Desulfovibrio sp.). Azotobacter sp. was present in numbers of 10⁷ per g of dry mud, whereas the two anaerobic fixers were present in much lower numbers (10³ to 10⁴ per g of dry mud). There were no differences in the numbers of each group among the different vegetational areas, indicating that there was a heterogeneous population of N₂ fixers present. Additional studies indicate that the activity of sulfate reducers (Desulfovibrio sp.) may account for as much as 50% of the total observed acetylene reduction activity. Oxygen was found to exert little effect on the observed acetylene reduction activity, indicating that stable aerobic and anaerobic microenvironments exist in the surface layer of marsh sediments.     

Plant growth stimulation of wheat (Triticum aestivum L.) by inoculation of salinity tolerant Azotobacter strains

Five salinity tolerant Azotobacter strains i.e., ST3, ST6, ST9, ST17 and ST24 were obtained from saline soils. These Azotobacter strains were used as inoculant for wheat variety WH157 in earthen pots containing saline soil under pot house conditions, using three fertilizer treatment doses i.e., control (no fertilizer, no inoculation), 90 Kg N ha⁻¹ and 120 Kg N ha⁻¹. Inoculation with salinity tolerant Azotobacter strains caused significant increase in total nitrogen, biomass and grain yield of wheat. Maximum increase in plant growth parameters were obtained after inoculation with Azotobacter strain ST24 at fertilization dose of 120 kg N ha⁻¹ and its inoculation resulted in attaining 89.9 cms plant height, 6.1 g seed yield, 12.0 g shoot dry weight and 0.7 % total nitrogen. The survival of Azotobacter strain ST24 in the soil was also highest in all the treatments at 30, 60 and 90 days after sowing (DAS). However, the population of Azotobacter decreased on 90 DAS as compared to counts observed at 60 DAS at all the fertilization treatments.     

Light-Limited Growth Rate Modulates Nitrate Inhibition of Dinitrogen Fixation in the Marine Unicellular Cyanobacterium Crocosphaera watsonii

Biological N₂ fixation is the dominant supply of new nitrogen (N) to the oceans, but is often inhibited in the presence of fixed N sources such as nitrate (NO₃ ⁻). Anthropogenic fixed N inputs to the ocean are increasing, but their effect on marine N₂ fixation is uncertain. Thus, global estimates of new oceanic N depend on a fundamental understanding of factors that modulate N source preferences by N₂-fixing cyanobacteria. We examined the unicellular diazotroph Crocosphaera watsonii (strain WH0003) to determine how the light-limited growth rate influences the inhibitory effects of fixed N on N₂ fixation. When growth (µ) was limited by low light (µ = 0.23 d⁻¹), short-term experiments indicated that 0.4 µM NH₄ ⁺ reduced N₂-fixation by ∼90% relative to controls without added NH₄ ⁺. In fast-growing, high-light-acclimated cultures (µ = 0.68 d⁻¹), 2.0 µM NH₄ ⁺ was needed to achieve the same effect. In long-term exposures to NO₃ ⁻, inhibition of N₂ fixation also varied with growth rate. In high-light-acclimated, fast-growing cultures, NO₃ ⁻ did not inhibit N₂-fixation rates in comparison with cultures growing on N₂ alone. Instead NO₃ ⁻ supported even faster growth, indicating that the cellular assimilation rate of N₂ alone (i.e. dinitrogen reduction) could not support the light-specific maximum growth rate of Crocosphaera. When growth was severely light-limited, NO₃ ⁻ did not support faster growth rates but instead inhibited N₂-fixation rates by 55% relative to controls. These data rest on the basic tenet that light energy is the driver of photoautotrophic growth while various nutrient substrates serve as supports. Our findings provide a novel conceptual framework to examine interactions between N source preferences and predict degrees of inhibition of N₂ fixation by fixed N sources based on the growth rate as controlled by light.     

Photosynthate metabolism in the source leaves of n(2)-fixing soybean plants

Soybean plants (Glycine max [L.] Merr. cv Williams), which were symbiotic with Bradyrhizobium japonicum, and which grew well upon reduced nitrogen supplied solely through N₂ fixation processes, often exhibited excess accumulation of starch and sucrose and diminished soluble protein in their source leaves. Nitrate and ammonia, when supplied to the nodulated roots of N₂-fixing plants, mediated a reduction of foliar starch accumulation and a corresponding increase in soluble protein in the source leaves. This provided an opportunity to examine the potential metabolic adjustments by which NO₃⁻ and NH₄⁺ (N) sufficiency or deficiency exerted an influence upon soybean leaf starch synthesis. When compared with soybean plants supplied with N, elevated starch accumulation was focused in leaf palisade parenchyma tissue of N₂-fixing plants. Foliar activities of starch synthesis pathway enzymes including fructose-1,6-bisphosphate phosphatase, phosphohexoisomerase, phosphoglucomutase (PGM), as well as adenosine diphosphate glucose pyrophosphorylase (in some leaves) exhibited highest activities in leaf extracts of N₂-fixing plants when expressed on a leaf protein basis. This was interpreted to mean that there was an adaptation of these enzyme activities in the leaves of N₂-fixing plants, and this contributed to an increase in starch accumulation. Another major causal factor associated with increased starch accumulation was the elevation in foliar levels of fructose-6-phosphate, glucose-6-phosphate, and glucose-1-phosphate (G1P), which had risen to chloroplast concentrations considerably in excess of the K_m values for their respective target enzymes associated with starch synthesis, e.g. elevated G1P with respect to adenosine diphosphate glucose pyrophosphorylase (ADPG-PPiase) binding sites. The cofactor glucose-1,6-bisphosphate (G1,6BP) was found to be obligate for maximal PGM activity in soybean leaf extracts of N₂-fixing as well as N-supplemented plants, and G1,6BP levels in N₂-fixing plant leaves was twice that of levels in N-supplied treatments. However the concentration of chloroplastic G1,6BP in illuminated leaves was computed to be saturating with respect to PGM in both N₂-fixing and N-supplemented plants. This suggested that the higher level of this cofactor in N₂-fixing plant leaves did not confer any higher PGM activation and was not a factor in higher starch synthesis rates. Relative to plants supplied with NO₃⁻ and NH₄⁺, the source leaf glycerate-3-phosphate (3-PGA) and orthophosphate (Pi) concentrations in leaves of N₂-fixing plants were two to four times higher. Although Pi is a physiological competitive inhibitor of leaf chloroplast ADPG-PPiase, and hence, starch synthesis, elevated chloroplast 3-PGA levels in N₂-fixing plant leaves apparently prevented interference of Pi with ADPG-PPiase catalysis and starch synthesis.     

Modeling the C Economy of Anabaena flos-aquae: Estimates of Establishment, Maintenance, and Active Costs Associated with Growth on NH(3), NO(3), and N(2)

Steady state cultures of Anabaena flos-aquae were established over a wide range of phosphate-limited growth rates while N was supplied as either NH₃, NO₃⁻, or N₂ gas. At growth rates greater than 0.03 per hour, rates of gross and net carbon fixation were similar on all N sources. However, at lower growth rates (<0.03 per hour) in the NO₃⁻ and N₂ cultures, gross photosynthesis greatly exceeded net photosynthesis. The increase in photosynthetic O₂ evolution with growth rate was greatest when N requirements were met by NO₃⁻ and least when met by NH₃. These results were combined with previously reported measurements of cellular chemical composition, N assimilation, and acetylene reduction (Layzell, Turpin, Elrifi 1985 Plant Physiol 78: 739-745) to construct empirical models of carbon and energy flow for cultures grown at 30, 60, and 100% of their maximal growth rate on all N sources. The models suggested that over this growth range, 89 to 100% of photodriven electrons were allocated to biomass production in the NH₃ cells, whereas only 49 to 74% and 54 to 90% were partitioned to biomass in the NO₃⁻-and N₂-grown cells, respectively. The models were used to estimate the relative contribution of active, maintenance, and establishment costs associated with NO₃⁻ and N₂ assimilation over the entire range of growth rates. The models showed that the relative contribution of the component costs of N assimilation were growth rate dependent. At higher growth rates, the major costs for NO₃⁻ assimilation were the active costs, while in N₂-fixing cultures the major energetic requirements were those associated with heterocyst establishment and maintenance. It was concluded that compared with NO₃⁻ assimilation, N₂ fixation was energetically unfavorable due to the costs of heterocyst establishment and maintenance, rather than the active costs of N₂ assimilation.     

Dryland Soil Hydrological Processes and Their Impacts on the Nitrogen Balance in a Soil-Maize System of a Freeze-Thawing Agricultural Area

Understanding the fates of soil hydrological processes and nitrogen (N) is essential for optimizing the water and N in a dryland crop system with the goal of obtaining a maximum yield. Few investigations have addressed the dynamics of dryland N and its association with the soil hydrological process in a freeze-thawing agricultural area. With the daily monitoring of soil water content and acquisition rates at 15, 30, 60 and 90 cm depths, the soil hydrological process with the influence of rainfall was identified. The temporal-vertical soil water storage analysis indicated the local albic soil texture provided a stable soil water condition for maize growth with the rainfall as the only water source. Soil storage water averages at 0–20, 20–40 and 40–60 cm were observed to be 490.2, 593.8, and 358 m³ ha⁻¹, respectively, during the growing season. The evapo-transpiration (ET), rainfall, and water loss analysis demonstrated that these factors increased in same temporal pattern and provided necessary water conditions for maize growth in a short period. The dry weight and N concentration of maize organs (root, leaf, stem, tassel, and grain) demonstrated the N accumulation increased to a peak in the maturity period and that grain had the most N. The maximum N accumulative rate reached about 500 mg m⁻²d⁻¹ in leaves and grain. Over the entire growing season, the soil nitrate N decreased by amounts ranging from 48.9 kg N ha⁻¹ to 65.3 kg N ha⁻¹ over the 90 cm profile and the loss of ammonia-N ranged from 9.79 to 12.69 kg N ha⁻¹. With soil water loss and N balance calculation, the N usage efficiency (NUE) over the 0–90 cm soil profile was 43%. The soil hydrological process due to special soil texture and the temporal features of rainfall determined the maize growth in the freeze-thawing agricultural area.     

Burkholderia, a Genus Rich in Plant-Associated Nitrogen Fixers with Wide Environmental and Geographic Distribution

The genus Burkholderia comprises 19 species, including Burkholderia vietnamiensis which is the only known N₂-fixing species of this bacterial genus. The first isolates of B. vietnamiensis were recovered from the rhizosphere of rice plants grown in a phytotron, but its existence in natural environments and its geographic distribution were not reported. In the present study, most N₂-fixing isolates recovered from the environment of field-grown maize and coffee plants cultivated in widely separated regions of Mexico were phenotypically identified as B. cepacia using the API 20NE system. Nevertheless, a number of these isolates recovered from inside of maize roots, as well as from the rhizosphere and rhizoplane of maize and coffee plants, showed similar or identical features to those of B. vietnamiensis TVV75^T. These features include nitrogenase activity with 10 different carbon sources, identical or very similar nifHDK hybridization patterns, very similar protein electrophoregrams, identical amplified 16S rDNA restriction (ARDRA) profiles, and levels of DNA-DNA reassociation higher than 70% with total DNA from strain TVV75^T. Although the ability to fix N₂ is not reported to be a common feature among the known species of the genus Burkholderia, the results obtained show that many diazotrophic Burkholderia isolates analyzed showed phenotypic and genotypic features different from those of the known N₂-fixing species B. vietnamiensis as well as from those of B. kururiensis, a bacterium identified in the present study as a diazotrophic species. DNA-DNA reassociation assays confirmed the existence of N₂-fixing Burkholderia species different from B. vietnamiensis. In addition, this study shows the wide geographic distribution and substantial capability of N₂-fixing Burkholderia spp. for colonizing diverse host plants in distantly separated environments.     

Aerobic nitrous oxide production through N-nitrosating hybrid formation in ammonia-oxidizing archaea

Soil emissions are largely responsible for the increase of the potent greenhouse gas nitrous oxide (N₂O) in the atmosphere and are generally attributed to the activity of nitrifying and denitrifying bacteria. However, the contribution of the recently discovered ammonia-oxidizing archaea (AOA) to N₂O production from soil is unclear as is the mechanism by which they produce it. Here we investigate the potential of Nitrososphaera viennensis, the first pure culture of AOA from soil, to produce N₂O and compare its activity with that of a marine AOA and an ammonia-oxidizing bacterium (AOB) from soil. N. viennensis produced N₂O at a maximum yield of 0.09% N₂O per molecule of nitrite under oxic growth conditions. N₂O production rates of 4.6±0.6 amol N₂O cell⁻¹ h⁻¹ and nitrification rates of 2.6±0.5 fmol NO₂⁻ cell⁻¹ h⁻¹ were in the same range as those of the AOB Nitrosospira multiformis and the marine AOA Nitrosopumilus maritimus grown under comparable conditions. In contrast to AOB, however, N₂O production of the two archaeal strains did not increase when the oxygen concentration was reduced, suggesting that they are not capable of denitrification. In ¹⁵N-labeling experiments we provide evidence that both ammonium and nitrite contribute equally via hybrid N₂O formation to the N₂O produced by N. viennensis under all conditions tested. Our results suggest that archaea may contribute to N₂O production in terrestrial ecosystems, however, they are not capable of nitrifier-denitrification and thus do not produce increasing amounts of the greenhouse gas when oxygen becomes limiting.     

Epsilonproteobacteria Represent the Major Portion of Chemoautotrophic Bacteria in Sulfidic Waters of Pelagic Redoxclines of the Baltic and Black Seas

Recent studies have indicated that chemoautotrophic Epsilonproteobacteria might play an important role, especially as anaerobic or microaerophilic dark CO₂-fixing organisms, in marine pelagic redoxclines. However, knowledge of their distribution and abundance as actively CO₂-fixing microorganisms in pelagic redoxclines is still deficient. We determined the contribution of Epsilonproteobacteria to dark CO₂ fixation in the sulfidic areas of central Baltic Sea and Black Sea redoxclines by combining catalyzed reporter deposition-fluorescence in situ hybridization with microautoradiography using [¹⁴C]bicarbonate and compared it to the total prokaryotic chemoautotrophic activity. In absolute numbers, up to 3 × 10^{5 14}CO₂-fixing prokaryotic cells ml⁻¹ were enumerated in the redoxcline of the central Baltic Sea and up to 9 × 10^{4 14}CO₂-fixing cells ml⁻¹ were enumerated in the Black Sea redoxcline, corresponding to 29% and 12%, respectively, of total cell abundance. ¹⁴CO₂-incorporating cells belonged exclusively to the domain Bacteria. Among these, members of the Epsilonproteobacteria were approximately 70% of the cells in the central Baltic Sea and up to 100% in the Black Sea. For the Baltic Sea, the Sulfurimonas subgroup GD17, previously assumed to be involved in autotrophic denitrification, was the most dominant CO₂-fixing group. In conclusion, Epsilonproteobacteria were found to be mainly responsible for chemoautotrophic activity in the dark CO₂ fixation maxima of the Black Sea and central Baltic Sea redoxclines. These Epsilonproteobacteria might be relevant in similar habitats of the world's oceans, where high dark CO₂ fixation rates have been measured.     

Maize Yield Response to Water Supply and Fertilizer Input in a Semi-Arid Environment of Northeast China

Maize grain yield varies highly with water availability as well as with fertilization and relevant agricultural management practices. With a 311-A optimized saturation design, field experiments were conducted between 2006 and 2009 to examine the yield response of spring maize (Zhengdan 958, Zea mays L) to irrigation (I), nitrogen fertilization (total nitrogen, urea-46% nitrogen,) and phosphorus fertilization (P₂O₅, calcium superphosphate-13% P₂O₅) in a semi-arid area environment of Northeast China. According to our estimated yield function, the results showed that N is the dominant factor in determining maize grain yield followed by I, while P plays a relatively minor role. The strength of interaction effects among I, N and P on maize grain yield follows the sequence N+I >P+I>N+P. Individually, the interaction effects of N+I and N+P on maize grain yield are positive, whereas that of P+I is negative. To achieve maximum grain yield (10506.0 kg·ha⁻¹) for spring maize in the study area, the optimum application rates of I, N and P are 930.4 m³·ha⁻¹, 304.9 kg·ha⁻¹ and 133.2 kg·ha⁻¹ respectively that leads to a possible economic profit (EP) of 10548.4 CNY·ha⁻¹ (CNY, Chinese Yuan). Alternately, to obtain the best EP (10827.3 CNY·ha⁻¹), the optimum application rates of I, N and P are 682.4 m³·ha⁻¹, 241.0 kg·ha⁻¹ and 111.7 kg·ha⁻¹ respectively that produces a potential grain yield of 10289.5 kg·ha⁻¹.     

Response of the Endophytic Diazotroph Gluconacetobacter diazotrophicus on Solid Media to Changes in Atmospheric Partial O2 Pressure

Gluconacetobacter diazotrophicus is an N₂-fixing endophyte isolated from sugarcane. G. diazotrophicus was grown on solid medium at atmospheric partial O₂ pressures (pO₂) of 10, 20, and 30 kPa for 5 to 6 days. Using a flowthrough gas exchange system, nitrogenase activity and respiration rate were then measured at a range of atmospheric pO₂ (5 to 60 kPa). Nitrogenase activity was measured by H₂ evolution in N₂-O₂ and in Ar-O₂, and respiration rate was measured by CO₂ evolution in N₂-O₂. To validate the use of H₂ production as an assay for nitrogenase activity, a non-N₂-fixing (Nif⁻) mutant of G. diazotrophicus was tested and found to have a low rate of uptake hydrogenase (Hup⁺) activity (0.016± 0.009 μmol of H₂ 10¹⁰ cells⁻¹ h⁻¹) when incubated in an atmosphere enriched in H₂. However, Hup⁺ activity was not detectable under the normal assay conditions used in our experiments. G. diazotrophicus fixed nitrogen at all atmospheric pO₂ tested. However, when the assay atmospheric pO₂ was below the level at which the colonies had been grown, nitrogenase activity was decreased. Optimal atmospheric pO₂ for nitrogenase activity was 0 to 20 kPa above the pO₂ at which the bacteria had been grown. As atmospheric pO₂ was increased in 10-kPa steps to the highest levels (40 to 60 kPa), nitrogenase activity decreased in a stepwise manner. Despite the decrease in nitrogenase activity as atmospheric pO₂ was increased, respiration rate increased marginally. A large single-step increase in atmospheric pO₂ from 20 to 60 kPa caused a rapid 84% decrease in nitrogenase activity. However, upon returning to 20 kPa of O₂, 80% of nitrogenase activity was recovered within 10 min, indicating a “switch-off/switch-on” O₂ protection mechanism of nitrogenase activity. Our study demonstrates that colonies of G. diazotrophicus can fix N₂ at a wide range of atmospheric pO₂ and can adapt to maintain nitrogenase activity in response to both long-term and short-term changes in atmospheric pO₂.     

Coliform Bacteria and Nitrogen Fixation in Pulp and Paper Mill Effluent Treatment Systems

The majority of pulp and paper mills now biotreat their combined effluents using activated sludge. On the assumption that their wood-based effluents have negligible fixed N, and that activated-sludge microorganisms will not fix significant N, these mills routinely spend large amounts adding ammonia or urea to their aeration tanks (bioreactors) to permit normal biomass growth. N₂ fixation in seven Eastern Canadian pulp and paper mill effluent treatment systems was analyzed using acetylene reduction assays, quantitative nitrogenase (nifH) gene probing, and bacterial isolations. In situ N₂ fixation was undetectable in all seven bioreactors but was present in six associated primary clarifiers. One primary clarifier was studied in greater detail. Approximately 50% of all culturable cells in the clarifier contained nifH, of which >90% were Klebsiella strains. All primary-clarifier coliform bacteria growing on MacConkey agar were identified as klebsiellas, and all those probed contained nifH. In contrast, analysis of 48 random coliform isolates from other mill water system locations showed that only 24 (50%) possessed the nifH gene, and only 13 (27%) showed inducible N₂-fixing activity. Thus, all the pulp and paper mill primary clarifiers tested appeared to be sites of active N₂ fixation (0.87 to 4.90 mg of N liter⁻¹ day⁻¹) and a microbial community strongly biased toward this activity. This may also explain why coliform bacteria, especially klebsiellas, are indigenous in pulp and paper mill water systems.     

Root Nodule Enzymes of Ammonia Assimilation in Alfalfa (Medicago sativa L.) : DEVELOPMENTAL PATTERNS AND RESPONSE TO APPLIED NITROGEN

Nitrogenase-dependent acetylene reduction activity of glasshouse-grown alfalfa (Medicago sativa L.) decreased rapidly in response both to harvesting (80% shoot removal) and applied NO₃⁻ at 40 and 80 kilograms N per hectare. Acetylene reduction activity of harvested plants grown on 0 kilogram N per hectare began to recover by day 15 as shoot regrowth became significant. In contrast, acetylene reduction activity of all plants treated with 80 kilograms NO₃⁻-N per hectare and harvested plants treated with 40 kilograms NO₃⁻-N per hectare remained low for the duration of the experiment. Acetylene reduction of unharvested alfalfa treated with 40 kilograms N per hectare declined to an intermediate level and appeared to recover slightly by day 15. Changes in N₂-fixing capacity were accompanied by similar changes in levels of nodule soluble protein.     

Alder and lupine enhance nitrogen cycling in a degraded forest soil in Northern Sweden

Positive effects of legumes and actinorhizal plants on N-poor soils have been observed in many studies but few have been done at high latitudes, which was the location of our study. We measured N₂ fixation and several indices of soil N at a site near the Arctic Circle in northern Sweden. More than 20 years ago lupine (Lupinus nootkatensis Donn) and gray alder (Alnus incana L. Moench) were planted on this degraded forest site. We measured total soil N, net N mineralization and nitrification with a buried bag technique, and fluxes of NH⁺ ₄ and NO^– ₃ as collected on ion exchange membranes. We also estimated N₂ fixation activity of the N₂-fixing plants by the natural abundance of ¹⁵N of leaves with Betula pendula Roth. as reference species. Foliar nitrogen in the N₂-fixing plants was almost totally derived from N₂ fixation. Plots containing N₂-fixing species generally had significantly higher soil N and N availability than a control plot without N₂-fixing plants. Taken together, all measurements indicated that N₂-fixing plants can be used to effectively improve soil fertility at high latitudes in northern Sweden.