Role of nitrate and nitrite for production and consumption of nitric oxide during denitrification in soil

Abstract Anaerobic production and consumption of NO was measured in a calcic cambisol (KBE; pH 7.3) and a forest luvisol (PBE; pH 4.4) which were incubated at 80% water-holding capacity and continuously flushed with N₂. Both NO production and NO consumption were negligibly low when nitrate and nitrite concentrations in the soil were exhausted. Addition of glucose alone had no effect, but addition of nitrate ± glucose greatly stimulated both NO production and NO consumption. NO consumption followed an apparent first-order reaction at low NO mixing ratios (1–3 ppmv), but a higher NO mixing ratios it followed Michaelis-Menten kinetics. In PBE the apparent K _m was 980 ppbv NO (1.92 nM in soil water). During reduction of nitrate, nitrite intermediately accumulated and simultaneously, production rates of NO and N₂O were at the maximum. Production rates of NO plus N₂O amounted to 20% and 34% of the nitrate reduction rate in KBE and PBE, respectively. NO production was hyperbolically related to the nitrite concentration, indicating an apparent K_m of 1.6 μg nitrite-N g⁻¹ d.w. soil (equivalent to 172 μM nitrite in soil solution) for the reduction of nitrite to NO in KBE. Under nitrate and nitrite-limiting conditions, 62–76% and 93–97% of the consumed NO-N were recovered as N₂O-N in KBE and PBE, respectively. Gassing of nitrate plus nitrite-depretsu KBE with increasing mixing ratios of NO₂ resulted in increasing rates of NO₂ uptake and presumably in the formation of low concentrations of nitrite and nitrate. This NO₂ uptake resulted in increasing rates of both NO production and NO consumption indicating that nitrite or nitrate was limiting for both reactions.     

Metabolism of nitric oxide in soil and denitrifying bacteria

Abstract Production and consumption of NO was measured under anaerobic conditions in a slightly alkaline and an acidic soil as well as in pure cultures of denitrifying Pseudomonas aeruginosa, P. stutzeri, P. fluorescens, Paracoccus denitrificans, Azospirillum brasilense , and A. lipoferum . Growing bacterial cultures reduced nitrate and intermediately accumulated nitrite, NO, N₂O, but not NO₂. Addition of formaldehyde inhibited NO production and NO consumption. In the presence of acetylene NO was reduced to N₂O. Net NO release rates in denitrifying bacterial suspensions and in soil samples decreased hyperbolically with increasing NO up to mixing ratios of about 5 ppmv NO. This behaviour could be modelled by assuming a constant rate of NO production simultaneously with a NO consumption activity that increased with NO until V _max was reached. The data allowed calculation of the gross rates ( P ) of NO production, of the rate constants ( k ), V _max and K _m of NO consumption, and of the NO compensation mixing ratio ( m _c). In soil, P was larger than V _max resulting in net NO release even at high NO mixing ratios unless P was selectively inhibited by chlorate + chlorite or by aerobic incubation conditions. In bacteria, V _max was somewhat larger than P resulting in net NO uptake at high NO mixing ratios. Both P and V _max were dependent on the supply of electron donor (e.g. glucose). Both in soil (aerobic or anaerobic) and in pure culture, the K _m values of NO consumption were in a similar low range of about 0.5–6.0 nM. Anaerobic soil and denitrifying bacteria exhibited m _c values of 1.6–2.1 ppmv NO and 0.2–4.0 ppmv NO, respectively.     

Ferrous iron dependent nitric oxide production in nitrate reducing cultures of Escherichia coli

l-Lactate-driven ferric and nitrate reduction was studied in Escherichia coli E4. Ferric iron reduction activity in E. coli E4 was found to be constitutive. Contrary to nitrate, ferric iron could not be used as electron acceptor for growth. Ferric iron reductase activity of 9 nmol Fe²⁺ mg^-1 protein min^-1 could not be inhibited by inhibitors for the respiratory chain, like Rotenone, quinacrine, Actinomycin A, or potassium cyanide. Active cells and l-lactate-driven nitrate respiration in E. coli E4 leading to the production of nitrite, was reduced to about 20% of its maximum activity with 5 mM ferric iron, or to about 50% in presence of 5 mM ferrous iron. The inhibition was caused by nitric oxide formed by a purely chemical reduction of nitrite by ferrous iron. Nitric oxide was further chemically reduced by ferrous iron to nitrous oxide. With electron paramagnetic resonance spectroscopy, the presence of a free [Fe²⁺-NO] complex was shown. In presence of ferrous or ferric iron and l-lactate, nitrate was anaerobically converted to nitric oxide and nitrous oxide by the combined action of E. coli E4 and chemical reduction reactions (chemodenitrification).     

Production and consumption of nitric oxide by denitrifying bacteria under anaerobic and aerobic conditions

Abstract: Pseudomonas aeruginosa, P. stutzeri and Azospirillum brasilense showed highest NO production rates and NO consumption rate constants when anaerobically grown cells were tested under anaerobic conditions. Aerobic assay conditions resulted in 20–75-fold lower NO production rates. NO consumption rate constants, however, decreased by less than a factor of four. NO consumption activity was observed even in aerobically grown P. aeruginosa , provided the assay was done under anaerobic conditions. Obviously, NO consumption was less O₂-sensitive than NO production so that compensation between production and consumption occurred at lower NO mixing ratios under aerobic than under anaerobic conditions.     

Reduction of nitric oxide in bacterial nitric oxide reductase—a theoretical model study

The mechanism of the nitric oxide reduction in a bacterial nitric oxide reductase (NOR) has been investigated in two model systems of the heme-b₃-Fe_B active site using density functional theory (B3LYP). A model with an octahedral coordination of the non-heme Fe_B consisting of three histidines, one glutamate and one water molecule gave an energetically feasible reaction mechanism. A tetrahedral coordination of the non-heme iron, corresponding to the one of Cu_B in cytochrome oxidase, gave several very high barriers which makes this type of coordination unlikely. The first nitric oxide coordinates to heme b₃ and is partly reduced to a more nitroxyl anion character, which activates it toward an attack from the second NO. The product in this reaction step is a hyponitrite dianion coordinating in between the two irons. Cleaving an NO bond in this intermediate forms an Fe_B (IV)O and nitrous oxide, and this is the rate determining step in the reaction mechanism. In the model with an octahedral coordination of Fe_B the intrinsic barrier of this step is 16.3 kcal/mol, which is in good agreement with the experimental value of 15.9 kcal/mol. However, the total barrier is 21.3 kcal/mol, mainly due to the endergonic reduction of heme b₃ taken from experimental reduction potentials. After nitrous oxide has left the active site the ferrylic Fe_B will form a μ-oxo bridge to heme b₃ in a reaction step exergonic by 45.3 kcal/mol. The formation of a quite stable μ-oxo bridge between heme b₃ and Fe_B is in agreement with this intermediate being the experimentally observed resting state in oxidized NOR. The formation of a ferrylic non-heme Fe_B in the proposed reaction mechanism could be one reason for having an iron as the non-heme metal ion in NOR instead of a Cu as in cytochrome oxidase.     

The impact of organic matter on nitric oxide formation by Nitrosomonas europaea

Chemolithoautotrophically growing cells of Nitrosomonas europaea quantitatively oxidized ammonia to nitrite under aerobic conditions with no loss of inorganic nitrogen. Significant inorganic nitrogen losses occurred when cells were growing mixotrophically with ammonium, pyruvate, yeast extract and peptone. Under oxygen limitation the nitrogen losses were even higher. In the absence of oxygen pyruvate was metabolized slowly while nitrite was consumed concomitantly. Nitrogen losses were due to the production of nitric oxide and nitrous oxide. In mixed cultures of Nitrosomonas and Nitrobacter, strong inhibition of nitrite oxidation was reproducibly measured. NO and ammonium were not inhibitory to Nitrobacter. First evidence is given that hydroxylamine, the intermediate of the Nitrosomonas monooxygenase-reaction, is formed. 0.2 to 1.7 M NH₂OH were produced by mixotrophically growing cells of Nitrosomonas and Nitrosovibrio. Hydroxylamine was both a selective inhibitory agent to Nitrobacter cells and a strong reductant which reduced nitrite to NO and N₂O. It is discussed whether chemodenitrification or denitrification is the most abundant process for NO and N₂O production of Nitrosomonas.     

Nitrification and nitrous oxide production potentials in aerobic soil samples from the soil profile of a Finnish coniferous site receiving high ammonium deposition

Abstract Using aerobic soil slurry technique nitrification and nitrous oxide production were studied in samples from a pine site in Western Finland. The site received atmospheric ammonium deposition of 7–33 kg N ha⁻¹ a⁻¹ from a mink farm. The experiments with soil slurries showed that the nitrification potential in the litter layer was higher at pH 6 than at pH 4. However, the nitrification potentials in the samples from the organic and mineral horizons at pH 6 and 4 were almost equal. Also N₂O was produced at a higher rate at pH 6 than at pH 4 in slurries of the litter layer samples. The reverse was true for samples from the organic and mineral horizons. The highest N₂O production and nitrification rates were measured in the suspensions of litter layer samples. Nitrification activity in field-moist soil samples was lower than the activity in the slurries indicating that the availability of ammonium limited nitrification in these soils. Acetylene (2.5 kPa) retarded nitrification activity (70-–100%) and N₂O production (40 – 90%) in soil slurries. Acetylene inhibited the N₂O production by 40–60% during the first 3 days after its addition to field-moist samples incubated in aerobic atmosphere. After 3 days the inhibition became much lower (4–5%). The results indicate that, in soil profiles of boreal coniferous forests receiving ammonium deposition, chemolithotrophic nitrification may have importance in the N₂O production, and that changes in soil pH affect differently nitrification as well as N₂O production in litter and deeper soil layers.     

Theoretical study of the reduction of nitric oxide in an A-type flavoprotein

The mechanism for the reduction of nitric oxide to nitrous oxide and water in an A-type flavoprotein (FprA) in Moorella thermoacetica, which has been proposed to be a scavenging type of nitric oxide reductase, has been investigated using density functional theory (B3LYP). A dinitrosyl complex, [{FeNO}⁷]₂, has previously been proposed to be a key intermediate in the NO reduction catalyzed by FprA. The electrons and protons involved in the reduction were suggested to “super-reduce” the dinitrosyl intermediate to [{FeNO}⁸]₂ or the corresponding diprotonated form, [{FeNO(H)}⁸]₂. In this type of mechanism the electron and/or proton transfers will be a part of the rate-determining step. In the present study, on the other hand, a reaction mechanism is suggested in which N₂O can be formed before the protons and electrons enter the catalytic cycle. One of the irons in the diiron center is used to stabilize the formation of a hyponitrite dianion, instead of binding a second NO. Cleaving the N–O bond in the hyponitrite dianion intermediate is the rate-determining step in the proposed reaction mechanism. The barrier of 16.5 kcal mol⁻¹ is in good agreement with the barrier height of the experimental rate-determining step of 14.8 kcal mol⁻¹. The energetics of some intermediates in the “super-reduction” mechanism and the mechanism proceeding via a hyponitrite dianion are compared, favoring the latter. It is also discussed how to experimentally discriminate between the two mechanisms. Electronic supplementary material Supplementary material is available in the online version of this article at and is accessible for authorized users.     

甲醛炎性痛增强大鼠海马NOS表达和NO生成

目的：观察甲醛炎性痛过程中大鼠痛行为、海马一氧化氮合酶（NOS）活性及一氧化氮（NO）含量的变化以及变化的时程及区域特征。方法：采用辐射热甩尾法测定大鼠痛阈变化;采用NADPH—d组织化学法和硝酸还原酶法分别测定大鼠海马NOS表达和No含量。结果：皮下注射甲醛溶液后,大鼠出现伤害性感受反应及痛阈降低。注射甲醛后6h,海马CA1、CA2～3区及DG区NOS阳性细胞数目、阳性细胞染色深度均显著增加。海马NO含量亦显著增加;注射甲醛后12h时这些改变最为显著,48h时恢复至对照组水平。结论：甲醛炎性痛可诱导海马NOS活性增强及NO生成增多．这种改变可发生在海马各区．并具有一定的时程特征。     

Analysis of the effects of nitric oxide and oxygen on nitric oxide production by macrophages

The interactions between NO and O(2) in activated macrophages were analysed by incorporating previous cell culture and enzyme kinetic results into a novel reaction-diffusion model for plate cultures. The kinetic factors considered were: (i) the effect of O(2) on NO production by inducible NO synthase (iNOS); (ii) the effect of NO on NO synthesis by iNOS; (iii) the effect of NO on respiratory and other O(2) consumption; and (iv) the effects of NO and O(2) on NO consumption by a possible NO dioxygenase (NOD). Published data obtained by varying the liquid depth in macrophage cultures provided a revealing test of the model, because varying the depth should perturb both the O(2) and the NO concentrations at the level of the cells. The model predicted that the rate of NO(2)(-) production should be nearly constant, and that the net rate of NO production should decline sharply with increases in liquid depth, in excellent agreement with the experimental findings. In further agreement with available results for macrophage cultures, the model predicted that net NO synthesis should be more sensitive to liquid depth than to the O(2) concentration in the headspace. The main reason for the decrease in NO production with increasing liquid depth was the modulation of NO synthesis by NO, with O(2) availability playing only a minor role. The model suggests that it is the ability of iNOS to consume NO, as well as to synthesize it, that creates very sensitive feedback control, setting an upper bound on the NO concentration of approximately 1 microM. The effect of NO consumption by other possible pathways (e.g., NOD) would be similar to that of iNOS, in that it would help limit net NO production. The O(2) utilized during enzymatic NO consumption is predicted to make the O(2) demands of activated macrophages much larger than those of unactivated ones (where iNOS is absent); this remains to be tested experimentally.     

Production of nitric oxide in Nitrosomonas europaea by reduction of nitrite

Nitrosomonas europaea and Nitrosovibrio sp. produced NO and N₂O during nitrification of ammonium. Less then 15% of the produced NO was due to chemical decomposition of nitrite. Production of NO and especially of N₂O increased when the bacteria were incubated under anaerobic conditions at decreasing flow rates of air, or at increasing cell densities. Low concentrations of chlorite (10 M) inhibited the production of NO and N₂, but not of nitrite indicating that NO and N₂O were not produced during the oxidative conversion of ammonium to nitrite. NO and N₂O were produced during reduction of nitrite with hydrazine as electron donor in almost stoichiometric quantities indicating that reduction of nitrite was the main source of NO and N₂O.     

Nitrous oxide production by cyanobacteria

Evidence is presented here that axenic cultures of Nostoc spp., Aphanocapsa (PCC 6308), and Aphanocapsa (PCC 6714) but not Anacystis nidulans R-2 (PCC 7942) produce N₂O and ammonia when grown on nitrite. The data suggest that the cyanobacteria produce N₂O by nitrite reduction to ammonia.Nonstandard abbreviations DCMU 3-(3,4-dichlorophenyl)-1,1-dimethyl urea - NIR nitrite reductase     

Phylogenetic analysis of nitric oxide reductase gene homologues from aerobic ammonia-oxidizing bacteria

Nitric oxide (NO) and nitrous oxide (N2O) are climatically important trace gases that are produced by both nitrifying and denitrifying bacteria. In the denitrification pathway, N2O is produced from nitric oxide (NO) by the enzyme nitric oxide reductase (NOR). The ammonia-oxidizing bacterium Nitrosomonas europaea also possesses a functional nitric oxide reductase, which was shown recently to serve a unique function. In this study, sequences homologous to the large subunit of nitric oxide reductase (norB) were obtained from eight additional strains of ammonia-oxidizing bacteria, including Nitrosomonas and Nitrosococcus species (i.e., both beta- and gamma-Proteobacterial ammonia oxidizers), showing widespread occurrence of a norB homologue in ammonia-oxidizing bacteria. However, despite efforts to detect norB homologues from Nitrosospira strains, sequences have not yet been obtained. Phylogenetic analysis placed nitrifier norB homologues in a subcluster, distinct from denitrifier sequences. The similarities and differences of these sequences highlight the need to understand the variety of metabolisms represented within a "functional group" defined by the presence of a single homologous gene. These results expand the database of norB homologue sequences in nitrifying bacteria.     

Effect of copper dosing on sulfide inhibited reduction of nitric and nitrous oxide

The stimulating effect of copper addition on the reduction rate of nitrous oxide (N(2)O) to dinitrogen (N(2)) in the presence of sulfide was investigated in batch experiments (pH 7.0; 55 degrees C). N(2)O was dosed either directly as a gas to the headspace of the bottles or formed as intermediate during the denitrification of nitrite in Fe(II)EDTA(2-)-containing medium and nitrate in Fe(II)EDTA(2-)-free medium. Sulfide was either dosed externally or generated from endogenous sulfur sources during anaerobic incubation of the sludge. In the presence of sulfide (from 15 microM to 1mM), heterotrophic denitrification using ethanol as electron donor was incomplete, i.e., N(2)O accumulated instead of N(2) or was transiently formed. Copper addition (60 microM) rapidly stimulated the reduction of N(2)O to N(2). Zinc addition (60 microM) did not have a similar strong stimulating effect as observed for copper and the N(2)O reduction rate was not stimulated at all upon supply of FeCl(3) (2 mM). Thus, a copper deficiency for N(2)O reduction is most likely developed in the presence of sulfide. It is suggested that sulfide induces this deficiency as it readily precipitates as copper sulfide and thus scavenges copper in the medium or that sulfide inactivates the N(2)OR reductase as it sequesters the copper of this metalloenzyme.     

Aged garlic extract enhances production of nitric oxide

Nitric oxide (NO) controls several physiological functions of the cardiovascular system. Three kinds of NO synthases (NOSs), neuronal constitutive NOS (ncNOS), inducible NOS (iNOS) and endothelial constitutive NOS (ecNOS), were responsible for NO biosynthesis. This study investigated the effect of aged garlic extract (AGE) on NO production by measuring the NO metabolites nitrite and nitrate in the plasma of mice. AGE (2.86 g/kg, p.o.) temporarily increased NO production by 30-40% from 15 to 60 min after administration. The time course of the fluctuation in NO levels in the AGE-treated group was clearly different to that in a group of mice treated with lipopolysaccharides, a typical iNOS inducer. Arginine (63 mg/kg, p.o.) at the equivalent dose of AGE did not increase NO production. However diphenyleneiodonium chloride (1 mg/kg, i.p.), a selective cNOS inhibitor, administered prior to AGE, overcame the effect of AGE. These results indicate that AGE increased NO production by activating cNOS, but not iNOS. The arginine contained in AGE was not responsible for the effect. AGE may be a useful tool for the prevention of cardiovascular disease.     

Processes regulating nitric oxide emissions from soils

Nitric oxide (NO) is a reactive gas that plays an important role in atmospheric chemistry by influencing the production and destruction of ozone and thereby the oxidizing capacity of the atmosphere. NO also contributes by its oxidation products to the formation of acid rain. The major sources of NO in the atmosphere are anthropogenic emissions (from combustion of fossil fuels) and biogenic emission from soils. NO is both produced and consumed in soils as a result of biotic and abiotic processes. The main processes involved are microbial nitrification and denitrification, and chemodenitrification. Thus, the net result is complex and dependent on several factors such as nitrogen availability, organic matter content, oxygen status, soil moisture, pH and temperature. This paper reviews recent knowledge on processes forming NO in soils and the factors controlling its emission to the atmosphere. Schemes for simulating these processes are described, and the results are discussed with the purpose of scaling up to global emission.