Comparison of control of Listeria by nitric oxide redox chemistry from murine macrophages and NO donors: insights into listeriocidal activity of oxidative and nitrosative stress

The physiological function of nitric oxide (NO) in the defense against pathogens is multifaceted. The exact chemistry by which NO combats intracellular pathogens such as Listeria monocytogenes is yet unresolved. We examined the effects of NO exposure, either delivered by NO donors or generated in situ within ANA-1 murine macrophages, on L. monocytogenes growth. Production of NO by the two NONOate compounds PAPA/NO (NH2(C3H6)(N[N(O)NO]C3H7) and DEA/NO (Na(C2H5)2N[N(O)NO]) resulted in L. monocytogenes cytostasis with minimal cytotoxicity. Reactive oxygen species generated from xanthine oxidase/hypoxanthine were neither bactericidal nor cytostatic and did not alter the action of NO. L. monocytogenes growth was also suppressed upon internalization into ANA-1 murine macrophages primed with interferon-gamma (INF-gamma) + tumor necrosis factor-alpha (TNF-alpha or INF-gamma + lipid polysaccharide (LPS). Growth suppression correlated with nitrite formation and nitrosation of 2,3-diaminonaphthalene elicited by stimulated murine macrophages. This nitrosative chemistry was not dependent upon nor mediated by interaction with reactive oxygen species (ROS), but resulted solely from NO and intermediates related to nitrosative stress. The role of nitrosation in controlling L. monocytogenes was further examined by monitoring the effects of exposure to NO on an important virulence factor, Listeriolysin O, which was inhibited under nitrosative conditions. These results suggest that nitrosative stress mediated by macrophages is an important component of the immunological arsenal in controlling L. monocytogenes infections.     

Evidence for mutagenesis by nitric oxide during nitrate metabolism in Escherichia coli

In Escherichia coli, nitrosative mutagenesis may occur during nitrate or nitrite respiration. The endogenous nitrosating agent N2O3 (dinitrogen trioxide, nitrous anhydride) may be formed either by the condensation of nitrous acid or by the autooxidation of nitric oxide, both of which are metabolic by-products. The purpose of this study was to determine which of these two agents is more responsible for endogenous nitrosative mutagenesis. An nfi (endonuclease V) mutant was grown anaerobically with nitrate or nitrite, conditions under which it has a high frequency of A:T-to-G:C transition mutations because of a defect in the repair of hypoxanthine (nitrosatively deaminated adenine) in DNA. These mutations could be greatly reduced by two means: (i) introduction of an nirB mutation, which affects the inducible cytoplasmic nitrite reductase, the major source of nitric oxide during nitrate or nitrite metabolism, or (ii) flushing the anaerobic culture with argon (which should purge it of nitric oxide) before it was exposed to air. The results suggest that nitrosative mutagenesis occurs during a shift from nitrate/nitrite-dependent respiration under hypoxic conditions to aerobic respiration, when accumulated nitric oxide reacts with oxygen to form endogenous nitrosating agents such as N2O3. In contrast, mutagenesis of nongrowing cells by nitrous acid was unaffected by an nirB mutation, suggesting that this mutagenesis is mediated by N2O3 that is formed directly by the condensation of nitrous acid.     

Nitrosative capacity of macrophages is dependent on nitric-oxide synthase induction signals

Nitrosative stress can occur when reactive nitric oxide (NO) species compromise the function of biomolecules via formation of NO adducts on critical amine and thiol residues. The capacity of inducible nitric-oxide synthase (iNOS) to generate nitrosative stress was investigated in the murine macrophage line ANA-1. Sequential activation with the cytokines IFN-gamma and either tumor necrosis factor-alpha or interleukin-1beta resulted in the induction of iNOS and production of nitrite (20 nM/min) but failed to elicit nitrosation of extracellular 2,3-diaminonapthalene. Stimulation with IFN-gamma and bacterial lipopolysaccharide increased the relative level of iNOS protein and nitrite production of ANA-1 cells 2-fold; however, a substantial level of NO in the media was also observed, and nitrosation of 2,3-diaminonapthalene was increased greater than 30-fold. Selective scavenger compounds suggested that the salient nitrosating mechanism was the NO/O(2) reaction leading to N(2)O(3) formation. These data mimicked the pattern observed with a 5 microM concentration of the synthetic NO donor (Z)-1-[N-ammoniopropyl)-N-(n-propyl)amino]diazen-1-ium -1,2-diolate (PAPA/NO). The NO profiles derived from iNOS can be distinct and depend on the inductive signal cascades. The diverse consequences of NO production in macrophages may reside in the cellular mechanisms that control the ability of iNOS to form N(2)O(3) and elicit nitrosative stress.     

Distinction between nitrosating mechanisms within human cells and aqueous solution

The quintessential nitrosating species produced during NO autoxidation is N(2)O(3). Nitrosation of amine, thiol, and hydroxyl residues can modulate critical cell functions. The biological mechanisms that control reactivity of nitrogen oxide species formed during autoxidation of nano- to micromolar levels of NO were examined using the synthetic donor NaEt(2)NN(O)NO (DEA/NO), human tumor cells, and 4,5-diaminofluorescein (DAF). Both the disappearance of NO and formation of nitrosated product from DAF in aerobic aqueous buffer followed second order processes; however, consumption of NO and nitrosation within intact cells were exponential. An optimal ratio of DEA/NO and 2-phenyl-4,4,5,5-tetramethylimidazole-1-oxyl 3-oxide (PTIO) was used to form N(2)O(3) through the intermediacy of NO(2). This route was found to be most reflective of the nitrosative mechanism within intact cells and was distinct from the process that occurred during autoxidation of NO in aqueous media. Manipulation of the endogenous scavengers ascorbate and glutathione indicated that the location, affinity, and concentration of these substances were key determinants in dictating nitrosative susceptibility of molecular targets. Taken together, these findings suggest that the functional effects of nitrosation may be organized to occur within discrete domains or compartments. Nitrosative stress may develop when scavengers are depleted and this architecture becomes compromised. Although NO(2) was not a component of aqueous NO autoxidation, the results suggest that the intermediacy of this species may be a significant factor in the advent of either nitrosation or oxidation chemistry in biological systems.     

An apoptotic model for nitrosative stress

Nitric oxide overproduction has been implicated in the pathogenesis of many disorders, including artherosclerosis, neurodegenerative diseases, inflammatory and autoimmune diseases, and cancer. The common view holds that nitric oxide-induced cellular injury is caused by oxidative stress. This theory predicts that interactions between reactive nitrogen species and reactive oxygen species produce powerful oxidants that initiate cell death programs. Cytokine-treated murine macrophages are the prototype of this form of cellular injury. Here we report that generation of reactive nitrogen species upon lipopolysacharide/interferon-gamma stimulation of RAW 264.7 cells is largely divorced from production of reactive oxygen species, and that oxidative stress is not principally responsible for cell death (in this model). Rather, the death program is induced mainly by a nitrosative challenge, characterized by the accrual of nitrosylated proteins without a major alteration in cellular redox state. Moreover, interactions between reactive oxygen and nitrogen species may alter the balance between pathways that yield nitrite and nitrate, without impacting the level of S-nitrosylation or extent of cell death. Our results thus (1) provide new insights into NO-related metabolic pathways, (2) demonstrate that apoptotic injury can be caused by nitrosative mechanisms, and (3) establish a model for nitrosative stress in mammalian cells.     

Interplay of Cu,Zn superoxide dismutase and nitric oxide synthase in neurodegenerative processes

Reactive oxygen and nitrogen species (ROS and RNS) have been extensively recognized as important signaling molecules implicated in physiological processes such as gene expression, cell differentiation and immune activation. Nevertheless, continuous production of these species may produce oxidative and/or nitrosative stress resulting in cell damage and ultimately leading to cell death. Due to the high oxygen consumption and relative poor antioxidant defense, the central nervous system is highly susceptible to ROS- and RNS-mediated toxicity. Actually, the oxidative and nitrosative stress have been implicated in the pathogenesis of neurodegeneration of a large variety of neurological disorders. This review will cover some aspects of the involvement of ROS- and RNS-mediated apoptotic processes occurring in cellular models of familial amyotrophic lateral sclerosis (FALS), in particular the cases associated with mutations in SOD1, the gene encoding Cu,Zn superoxide dismutase (Cu,Zn SOD). A possible role for proteasome in the inhibition of neurodegenerative process by balancing ROS and RNS species is envisaged on the basis of evidence provided by results obtained from studies on this experimental model.     

Mycobacterium tuberculosis hemoglobin N displays a protein tunnel suited for O2 diffusion to the heme

Macrophage-generated oxygen- and nitrogen-reactive species control the development of Mycobacterium tuberculosis infection in the host. Mycobacterium tuberculosis 'truncated hemoglobin' N (trHbN) has been related to nitric oxide (NO) detoxification, in response to macrophage nitrosative stress, during the bacterium latent infection stage. The three-dimensional structure of oxygenated trHbN, solved at 1.9 A resolution, displays the two-over-two alpha-helical sandwich fold recently characterized in two homologous truncated hemoglobins, featuring an extra N-terminal alpha-helix and homodimeric assembly. In the absence of a polar distal E7 residue, the O2 heme ligand is stabilized by two hydrogen bonds to TyrB10(33). Strikingly, ligand diffusion to the heme in trHbN may occur via an apolar tunnel/cavity system extending for approximately 28 A through the protein matrix, connecting the heme distal cavity to two distinct protein surface sites. This unique structural feature appears to be conserved in several homologous truncated hemoglobins. It is proposed that in trHbN, heme Fe/O2 stereochemistry and the protein matrix tunnel may promote O2/NO chemistry in vivo, as a M.tuberculosis defense mechanism against macrophage nitrosative stress.     

Production and consumption of nitric oxide by three methanotrophic bacteria

We studied nitrogen oxide production and consumption by methanotrophs Methylobacter luteus (group I), Methylosinus trichosporium OB3b (group II), and an isolate from a hardwood swamp soil, here identified by 16S ribosomal DNA sequencing as Methylobacter sp. strain T20 (group I). All could consume nitric oxide (nitrogen monoxide, NO), and produce small amounts of nitrous oxide (N(2)O). Only Methylobacter strain T20 produced large amounts of NO (>250 parts per million by volume [ppmv] in the headspace) at specific activities of up to 2.0 x 10(-17) mol of NO cell(-1) day(-1), mostly after a culture became O(2) limited. Production of NO by strain T20 occurred mostly in nitrate-containing medium under anaerobic or nearly anaerobic conditions, was inhibited by chlorate, tungstate, and O(2), and required CH(4). Denitrification (methanol-supported N(2)O production from nitrate in the presence of acetylene) could not be detected and thus did not appear to be involved in the production of NO. Furthermore, cd(1) and Cu nitrite reductases, NO reductase, and N(2)O reductase could not be detected by PCR amplification of the nirS, nirK, norB, and nosZ genes, respectively. M. luteus and M. trichosporium produced some NO in ammonium-containing medium under aerobic conditions, likely as a result of methanotrophic nitrification and chemical decomposition of nitrite. For Methylobacter strain T20, arginine did not stimulate NO production under aerobiosis, suggesting that NO synthase was not involved. We conclude that strain T20 causes assimilatory reduction of nitrate to nitrite, which then decomposes chemically to NO. The production of NO by methanotrophs such as Methylobacter strain T20 could be of ecological significance in habitats near aerobic-anaerobic interfaces where fluctuating O(2) and nitrate availability occur.     

Inhibitory effects of nitric oxide and nitrosative stress on dopamine-beta-hydroxylase

Dopamine-beta-hydroxylase (DbetaH) is a copper-containing enzyme that uses molecular oxygen and ascorbate to catalyze the addition of a hydroxyl group on the beta-carbon of dopamine to form norepinephrine. While norepinephrine causes vasoconstriction following reflex sympathetic stimulation, nitric oxide (NO) formation results in vasodilatation via a guanylyl cyclase-dependent mechanism. In this report, we investigated the relationship between NO and DbetaH enzymatic activity. In the initial in vitro experiments, the activity of purified DbetaH was inhibited by the NO donor, diethylamine/NO (DEA/NO), with an IC(50) of 1 mm. The inclusion of either azide or GSH partially restored DbetaH activity, suggesting the involvement of the reactive nitrogen oxide species, N(2)O(3). Treatment of human neuroblastoma cells (SK-N-MC) with diethylamine/NO decreased cellular DbetaH activity without affecting their growth rate and was augmented by the depletion of intracellular GSH. Co-culture of the SK-N-MC cells with interferon-gamma and lipopolysaccharide-activated macrophages, which release NO, also reduced the DbetaH activity in the neuroblastoma cells. Our results are consistent with the hypothesis that nitrosative stress, mediated by N(2)O(3), can result in the inhibition of norepinephrine biosynthesis and may contribute to the regulation of neurotransmission and vasodilatation.     

Unique oxidative mechanisms for the reactive nitrogen oxide species, nitroxyl anion

The nitroxyl anion (NO-) is a highly reactive molecule that may be involved in pathophysiological actions associated with increased formation of reactive nitrogen oxide species. Angeli's salt (Na2N2O3; AS) is a NO- donor that has been shown to exert marked cytotoxicity. However, its decomposition intermediates have not been well characterized. In this study, the chemical reactivity of AS was examined and compared with that of peroxynitrite (ONOO-) and NO/N2O3. Under aerobic conditions, AS and ONOO- exhibited similar and considerably higher affinities for dihydrorhodamine (DHR) than NO/N2O3. Quenching of DHR oxidation by azide and nitrosation of diaminonaphthalene were exclusively observed with NO/N2O3. Additional comparison of ONOO- and AS chemistry demonstrated that ONOO- was a far more potent one-electron oxidant and nitrating agent of hydroxyphenylacetic acid than was AS. However, AS was more effective at hydroxylating benzoic acid than was ONOO-. Taken together, these data indicate that neither NO/N2O3 nor ONOO- is an intermediate of AS decomposition. Evaluation of the stoichiometry of AS decomposition and O2 consumption revealed a 1:1 molar ratio. Indeed, oxidation of DHR mediated by AS proved to be oxygen-dependent. Analysis of the end products of AS decomposition demonstrated formation of NO2- and NO3- in approximately stoichiometric ratios. Several mechanisms are proposed for O2 adduct formation followed by decomposition to NO3- or by oxidation of an HN2O3- molecule to form NO2-. Given that the cytotoxicity of AS is far greater than that of either NO/N2O3 or NO + O2, this study provides important new insights into the implications of the potential endogenous formation of NO- under inflammatory conditions in vivo.     

Nitrous oxide production by Alcaligenes faecalis under transient and dynamic aerobic and anaerobic conditions.

Nitrous oxide can be a harmful by-product in nitrogen removal from wastewater. Since wastewater treatment systems operate under different aeration regimens, the influence of different oxygen concentrations and oxygen fluctuations on denitrification was studied. Continuous cultures of Alcaligenes faecalis TUD produced N2O under anaerobic as well as aerobic conditions. Below a dissolved oxygen concentration of 5% air saturation, the relatively highest N2O production was observed. Under these conditions, significant activities of nitrite reductase could be measured. After transition from aerobic to anaerobic conditions, there was insufficient nitrite reductase present to sustain growth and the culture began to wash out. After 20 h, nitrite reductase became detectable and the culture started to recover. Nitrous oxide reductase became measurable only after 27 h, suggesting sequential induction of the denitrification reductases, causing the transient accumulation of N2O. After transition from anaerobic conditions to aerobic conditions, nitrite reduction continued (at a lower rate) for several hours. N2O reduction appeared to stop immediately after the switch, indicating inhibition of nitrous oxide reductase, resulting in high N2O emissions (maximum, 1.4 mmol liter-1 h-1). The nitrite reductase was not inactivated by oxygen, but its synthesis was repressed. A half-life of 16 to 22 h for nitrite reductase under these conditions was calculated. In a dynamic aerobic-anaerobic culture of A. faecalis, a semisteady state in which most of the N2O production took place after the transition from anaerobic to aerobic conditions was obtained. The nitrite consumption rate in this culture was equal to that in an anaerobic culture (0.95 and 0.92 mmol liter-1 h-1, respectively), but the production of N2O was higher in the dynamic culture (28 and 26% of nitrite consumption, respectively).     

Oxidative and nitrosative signaling in plants: Two branches in the same tree?

Reactive oxygen species (ROS) and reactive nitrogen species (RNS) constitute key features underpinning the dynamic nature of cell signaling systems in plants. Despite their importance in many aspects of cell biology, our understanding of oxidative and especially of nitrosative signaling and their regulation remains poorly understood. Early reports have established that ROS and RNS coordinately regulate plant defense responses to biotic stress. In addition, evidence has accumulated demonstrating that there is a strong cross-talk between oxidative and nitrosative signaling upon abiotic stress conditions. The goal of this mini-review is to provide latest findings showing how both ROS and RNS comprise a coordinated oxidative and nitrosative signaling network that modulates cellular responses in response to environmental stimuli.Key words: abiotic stress, nitrosative stress, oxidative stress, reactive nitrogen species, reactive oxygen species, signaling     

Nitrosation-modulating effect of ascorbate in a model dynamic system of coexisting nitric oxide and superoxide

Abstract

The coexistence of nitric oxide and superoxide leads to complex oxidative and nitrosative chemistry, which has been implicated in many pathophysiological conditions. The present study investigated the role of ascorbate in affecting the kinetics of nitrosative chemistry in a model dynamic snystem of coexisting nitric oxide and superoxide. SIN-1 (3-morpholinosydnonimine) was used to elicit various degrees of nitroxidative stress in a reaction buffer and DAN (2,3-diaminonaphthalene) was used as a probe for N-nitrosation reaction. The nitrosation kinetics in the absence and presence of ascorbate was followed by measuring the formation of the fluorescent product over time. Computational modelling was used to provide quantitative or semi-quantitative insights into the studied system. The results show that ascorbate effectively quenches N-nitrosation reaction, which could be partially attributed to the free radical scavenging and repairing effect of ascorbate. Computational modelling reveals an interesting temporal distribution of superoxide, nitric oxide and peroxynitrite. The model predicts that peroxynitrite is the most predominant species in the SIN-1 system. Furthermore, ascorbate might alter the system dynamics by removing superoxide and, thereby, increasing the availability of nitric oxide.     

Flavohemoglobin: structure and reactivity

Flavohemoglobins (flavoHbs) are made of a globin domain fused with a ferredoxin reductaselike FAD- and NAD-binding modules. These proteins are widely represented among bacteria and yeasts and represent a most challenging research subject in view of their high reactivity both as reductases and as oxidases. The functional annotations of flavoHbs are still controversial, and different physiological roles that are linked to cell responses to oxidative and/or nitrosative stress have been proposed. The flavoHb from Escherichia coli (HMP) has been the object of a large number of investigations to unveil its physiological role in the framework of bacterial resistance to nitrosative stress. HMP expression has been demonstrated to respond to the presence of NO in the culture medium, and an explicit mechanism has been proposed that involves NO scavenging and its reduction to N(2)O under anaerobic conditions. In contrast to (or together with) the anaerobic NO-reductase activity, HMP has also been shown to be able to catalyze the oxidation of NO to NO(3) (-) (NO-dioxygenase activity) both in vivo and in vitro in the presence of O(2) and NADH. HMP has also been shown to be capable of catalyzing the reduction of several alkylhydroperoxide substrates into their corresponding alcohols using NADH as an electron donor. The alkylhydroperoxide reductase activity taken together with the unique lipid-binding properties of HMP suggests that this flavoHb may be involved in the repair of the lipid membrane oxidative damage generated during oxidative/nitrosative stress.     

Nitric oxide-induced S-glutathionylation and inactivation of glyceraldehyde-3-phosphate dehydrogenase

S-Nitrosylation of protein thiol groups by nitric oxide (NO) is a widely recognized protein modification. In this study we show that nitrosonium tetrafluoroborate (BF4NO), a NO+ donor, modified the thiol groups of glyceraldehyde-3-phosphate dehydrogenase (GAPDH) by S-nitrosylation and caused enzyme inhibition. The resultant protein-S-nitrosothiol was found to be unstable and to decompose spontaneously, thereby restoring enzyme activity. In contrast, the NO-releasing compound S-nitrosoglutathione (GSNO) promoted S-glutathionylation of a thiol group of GAPDH both in vitro and under cellular conditions. The GSH-mixed protein disulfide formed led to a permanent enzyme inhibition, but upon dithiothreitol addition a functional active GAPDH was recovered. This S-glutathionylation is specific for GSNO because GSH itself was unable to produce protein-mixed disulfides. During cellular nitrosative stress, the production of intracellular GSNO might channel signaling responses to form protein-mixed disulfide that can regulate intracellular function.     

Nitric oxide metabolism in Neisseria meningitidis

Neisseria meningitidis, the causative agent of meningococcal disease in humans, is likely to be exposed to nitrosative stress during natural colonization and disease. The genome of N. meningitidis includes the genes aniA and norB, predicted to encode nitrite reductase and nitric oxide (NO) reductase, respectively. These gene products should allow the bacterium to denitrify nitrite to nitrous oxide. We show that N. meningitidis can support growth microaerobically by the denitrification of nitrite via NO and that norB is required for anaerobic growth with nitrite. NorB and, to a lesser extent, the cycP gene product cytochrome c' are able to counteract toxicity due to exogenously added NO. Expression of these genes by N. meningitidis during colonization and disease may confer protection against exogenous or endogenous nitrosative stress.     

Soil microorganisms as controllers of atmospheric trace gases (H2, CO, CH4, OCS, N2O, and NO).

Production and consumption processes in soils contribute to the global cycles of many trace gases (CH4, CO, OCS, H2, N2O, and NO) that are relevant for atmospheric chemistry and climate. Soil microbial processes contribute substantially to the budgets of atmospheric trace gases. The flux of trace gases between soil and atmosphere is usually the result of simultaneously operating production and consumption processes in soil: The relevant processes are not yet proven with absolute certainty, but the following are likely for trace gas consumption: H2 oxidation by abiontic soil enzymes; CO cooxidation by the ammonium monooxygenase of nitrifying bacteria; CH4 oxidation by unknown methanotrophic bacteria that utilize CH4 for growth; OCS hydrolysis by bacteria containing carbonic anhydrase; N2O reduction to N2 by denitrifying bacteria; NO consumption by either reduction to N2O in denitrifiers or oxidation to nitrate in heterotrophic bacteria. Wetland soils, in contrast to upland soils are generally anoxic and thus support the production of trace gases (H2, CO, CH4, N2O, and NO) by anaerobic bacteria such as fermenters, methanogens, acetogens, sulfate reducers, and denitrifiers. Methane is the dominant gaseous product of anaerobic degradation of organic matter and is released into the atmosphere, whereas the other trace gases are only intermediates, which are mostly cycled within the anoxic habitat. A significant percentage of the produced methane is oxidized by methanotrophic bacteria at anoxic-oxic interfaces such as the soil surface and the root surface of aquatic plants that serve as conduits for O2 transport into and CH4 transport out of the wetland soils. The dominant production processes in upland soils are different from those in wetland soils and include H2 production by biological N2 fixation, CO production by chemical decomposition of soil organic matter, and NO and N2O production by nitrification and denitrification. The processes responsible for CH4 production in upland soils are completely unclear, as are the OCS production processes in general. A problem for future research is the attribution of trace gas metabolic processes not only to functional groups of microorganisms but also to particular taxa. Thus, it is completely unclear how important microbial diversity is for the control of trace gas flux at the ecosystem level. However, different microbial communities may be part of the reason for differences in trace gas metabolism, e.g., effects of nitrogen fertilizers on CH4 uptake by soil; decrease of CH4 production with decreasing temperature; or different rates and modes of NO and N2O production in different soils and under different conditions.     

Production of nitrous oxide in artificially flooded and drained soils

Production of nitrous oxide (N₂O) was studied in one peaty and one sandy soil undergoing wetting and drying cycles. The background concentration of N₂O in the soil was compared with the N₂O produced during 4 hours of incubation with and without addition of acetylene. The concentration of N₂O in the soil under flooded conditions was relatively stable, and net consumption of N₂O was observed as often as net production. The reference area and drained soils showed somewhat different patterns compared to the flooded soils, which was probably an effect of intermediate soil water conditions. During flooding, the nitrous oxide made up less than 1% of total denitrification on 50% and 54% of the sampling occasions for the peaty and the sandy soil, respectively, and N₂O/(N₂O+N₂)-ratios exceeded 0.2 on only 6% and 3% of the sampling occasions. Under drained conditions and in the reference areas, the ratios showed a more even frequency distribution. Grouping the nitrous oxide production data for different seasons and field conditions, we found few seasonal trends. At the sandy site, mean production of N₂O was larger during the winter months. There were weak correlations between N₂O production and floodwater nitrate concentration, and between N₂O production and soil temperature. N₂O production in the reference area varied between consumption and 4.6 kg N ha^–1 month^–1 and in flooded and drained soil between consumption and 2.6 kg N ha^–1 month^–1.